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griddap | Subset | tabledap | Make A Graph | wms | files | Accessible | Title | Summary | FGDC | ISO 19115 | Info | Background Info | RSS | Institution | Dataset ID | |
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https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2014.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2014 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2014.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2014/ | public | EMSO Western Ligurian : Albatross mooring, AQUADOPP sensor (CSV 2014-2015) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node.\n\ncdm_data_type = Other\nVARIABLES:\ntime (seconds since 1970-01-01T00:00:00Z)\nDEPH\nX_East\nY_North\nZ_Up\nAmplitude_X\nAmplitude_Y\nAmplitude_Z\nBattery\nSVEL\n... (7 more variables)\n | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2014/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2014.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2014&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2014 | ||||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2015.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2015 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2015.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2015/ | public | EMSO Western Ligurian : Albatross mooring, AQUADOPP sensor (CSV 2015-2016) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node.\n\ncdm_data_type = Other\nVARIABLES:\ntime (seconds since 1970-01-01T00:00:00Z)\nID\nDEPH\nPRES (Pressure)\nTEMP (Temperature)\nX_East\nY_North\nZ_Up\nSVEL\nHeading\n... (4 more variables)\n | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2015/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2015.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2015&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2015 | ||||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2016.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2016 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2016.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2016/ | public | EMSO Western Ligurian : Albatross mooring, AQUADOPP sensor (CSV 2016-2017) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node.\n\ncdm_data_type = Other\nVARIABLES:\nId\ntime (seconds since 1970-01-01T00:00:00Z)\nDepth\nX_East\nY_North\nZ_Up\nAmplitude_X\nAmplitude_Y\nAmplitude_Z\nBatterie\n... (8 more variables)\n | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2016/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2016.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2016&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2016 | ||||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2018.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2018 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2018.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2018/ | public | EMSO Western Ligurian : Albatross mooring, AQUADOPP sensor (CSV 2018-2019) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node.\n\ncdm_data_type = Other\nVARIABLES:\nId\ntime (seconds since 1970-01-01T00:00:00Z)\nDepth\nX_East\nY_North\nZ_Up\nAmplitude_X\nAmplitude_Y\nAmplitude_Z\nBatterie\n... (8 more variables)\n | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2018/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2018.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2018&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2018 | ||||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2021.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2021 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2021.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2021/ | public | EMSO Western Ligurian : Albatross mooring, AQUADOPP sensor (CSV files 2021-07 to 2023-05) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node.\n\ncdm_data_type = Point\nVARIABLES:\nId\ntime (seconds since 1970-01-01T00:00:00Z)\nProfondeur\nlatitude (degrees_north)\nlongitude (degrees_east)\nX_East\nY_North\nZ_Up\nAmplitude_X\nAmplitude_Y\n... (10 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2021_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2021_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2021/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2021.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2021&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2021 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2024.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2024 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2024.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2024/ | public | EMSO Western Ligurian : Albatross mooring, AQUADOPP sensor (CSV files from 2024-03) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node.\n\ncdm_data_type = Point\nVARIABLES:\nId\ntime (seconds since 1970-01-01T00:00:00Z)\nProfondeur\nlatitude (degrees_north)\nlongitude (degrees_east)\nX_East\nY_North\nZ_Up\nAmplitude_X\nAmplitude_Y\n... (10 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2024_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2024_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2024/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2024.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2024&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Albatross_Aquadopp_CSV_2024 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2014.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2014 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2014.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2014/ | public | EMSO Western Ligurian : Albatross mooring, AQUADOPP sensor (NetCDF 2014-2015) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node.\n\ncdm_data_type = TimeSeries\nVARIABLES:\nstationname (station name)\nlatitude (Latitude of measurements, degrees_north)\nlongitude (Longitude of measurements, degrees_east)\ntime (time of measurements, seconds since 1970-01-01T00:00:00Z)\nTIME_QC (Time quality flag)\nDEPH (depth of measurements, Metres)\nTEMP (temperature, degree_C)\nTEMP_QC (Temperature quality flag)\nPRES (pressure, Decibars)\nPRES_QC (Pressure quality flag)\n... (22 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2014_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2014_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2014/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2014.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2014&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2014 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2015.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2015 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2015.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2015/ | public | EMSO Western Ligurian : Albatross mooring, AQUADOPP sensor (NetCDF 2015-2016) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node.\n\ncdm_data_type = TimeSeries\nVARIABLES:\nstationname (station name)\nlatitude (Latitude of measurements, degrees_north)\nlongitude (Longitude of measurements, degrees_east)\ntime (time of measurements, seconds since 1970-01-01T00:00:00Z)\nTIME_QC (Time quality flag)\nDEPH (depth of measurements, Metres)\nTEMP (temperature, degree_C)\nTEMP_QC (Temperature quality flag)\nPRES (pressure, Decibars)\nPRES_QC (Pressure quality flag)\n... (16 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2015_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2015_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2015/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2015.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2015&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2015 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2016.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2016 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2016.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2016/ | public | EMSO Western Ligurian : Albatross mooring, AQUADOPP sensor (NetCDF 2016-2017) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node.\n\ncdm_data_type = TimeSeries\nVARIABLES:\nstationname (station name)\nlatitude (Latitude of measurements, degrees_north)\nlongitude (Longitude of measurements, degrees_east)\nDEPH (depth of measurements, Metres)\ntime (time of measurements, seconds since 1970-01-01T00:00:00Z)\nTIME_QC (Time quality flag)\nRFVL_X (Metres per second)\nRFVL_Y (Y_North, Metres per second)\nLRZA (Metres per second)\nXYZ_QC\n... (22 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2016_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2016_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2016/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2016.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2016&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2016 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2018.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2018 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2018.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2018/ | public | EMSO Western Ligurian : Albatross mooring, AQUADOPP sensor (NetCDF 2018-2019) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node.\n\ncdm_data_type = TimeSeries\nVARIABLES:\nstationname (station name)\nlatitude (Latitude of measurements, degrees_north)\nlongitude (Longitude of measurements, degrees_east)\nDEPH (depth of measurements, Metres)\ntime (time of measurements, seconds since 1970-01-01T00:00:00Z)\nTIME_QC (Time quality flag)\nRFVL_X (Metres per second)\nRFVL_Y (Y_North, Metres per second)\nLRZA (Metres per second)\nXYZ_QC\n... (22 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2018_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2018_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2018/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2018.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2018&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2018 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2021.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2021 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2021.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2021/ | public | EMSO Western Ligurian : Albatross mooring, AQUADOPP sensor (NetCDF files 2021-07 to 2023-05) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node.\n\ncdm_data_type = TimeSeries\nVARIABLES:\nstationname (station name)\nlatitude (Latitude of measurements, degrees_north)\nlongitude (Longitude of measurements, degrees_east)\nDEPH (depth of measurements, Metres)\ntime (time of measurements, seconds since 1970-01-01T00:00:00Z)\nTIME_QC (Time quality flag)\nRFVL_X (Metres per second)\nRFVL_Y (Y_North, Metres per second)\nLRZA (Metres per second)\nXYZ_QC\n... (22 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2021_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2021_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2021/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2021.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2021&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2021 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2024.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2024 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2024.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2024/ | public | EMSO Western Ligurian : Albatross mooring, AQUADOPP sensor (NetCDF files from 2024-03) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node\n\ncdm_data_type = TimeSeries\nVARIABLES:\nstationname (station name, N/A)\nlatitude (Latitude of measurements, degrees_north)\nlongitude (Longitude of measurements, degrees_east)\nDEPH (depth of measurements, Metres)\ntime (time of measurements, seconds since 1970-01-01T00:00:00Z)\nTIME_QC (Time quality flag)\nEWCT (X_East, Metres per second)\nNSCT (Y_North, Metres per second)\nVCSP (Metres per second)\nXYX_QC (Current Velocity Quality Code)\n... (22 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2024_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2024_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2024/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2024.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2024&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Albatross_Aquadopp_NetCDF_2024 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2014.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2014 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2014.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2014/ | public | EMSO Western Ligurian : Albatross mooring, MICROCAT sensor (NetCDF 2014-2015) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node.\n\ncdm_data_type = TimeSeries\nVARIABLES:\nstationname (station name)\nlatitude (Latitude of measurements, degrees_north)\nlongitude (Longitude of measurements, degrees_east)\ntime (time of measurements, seconds since 1970-01-01T00:00:00Z)\nTIME_QC (Time quality flag)\nDEPH (depth of measurements, Metres)\nTEMP (temperature, degree_C)\nTEMP_QC (Temperature quality flag)\nDOX2 (Dissolved oxygen, Micromoles per kilogram)\nDOX_QC (Oxygen quality flag)\n... (8 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2014_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2014_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2014/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2014.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2014&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2014 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2015.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2015 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2015.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2015/ | public | EMSO Western Ligurian : Albatross mooring, MICROCAT sensor (NetCDF 2015-2016) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node.\n\ncdm_data_type = TimeSeries\nVARIABLES:\nstationname (station name)\nlatitude (Latitude of measurements, degrees_north)\nlongitude (Longitude of measurements, degrees_east)\ntime (time of measurements, seconds since 1970-01-01T00:00:00Z)\nTIME_QC (Time quality flag)\nDEPH (depth of measurements, Metres)\nTEMP (temperature, degree_C)\nTEMP_QC (Temperature quality flag)\nDOX2 (Dissolved oxygen, Micromoles per kilogram)\nDOX_QC (Oxygen quality flag)\n... (8 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2015_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2015_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2015/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2015.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2015&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2015 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2016.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2016 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2016.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2016/ | public | EMSO Western Ligurian : Albatross mooring, MICROCAT sensor (NetCDF 2016-2017) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node.\n\ncdm_data_type = TimeSeries\nVARIABLES:\nPRES (pressure, Decibars)\nTPOT (temperature potentielle, degree_C)\nCNDC (conductivity, Siemens per metre)\nPSAL (Practical salinity)\nDEPH (depth of measurements, Metres)\nTEMP (temperature, degree_C)\ntime (time of measurements, seconds since 1970-01-01T00:00:00Z)\nOSAT (Oxygen saturation, Percent)\nDOX2 (Dissolved oxygen, Micromoles per kilogram)\nDOX1 (Dissolved oxygen, Micromoles per litre)\n... (10 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2016_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2016_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2016/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2016.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2016&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2016 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2018.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2018 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2018.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2018/ | public | EMSO Western Ligurian : Albatross mooring, MICROCAT sensor (NetCDF 2018-2019) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node\n\ncdm_data_type = TimeSeries\nVARIABLES:\ntime (time of measurements, seconds since 1970-01-01T00:00:00Z)\nPRES (pressure, Decibars)\nDEPH (depth of measurements, Metres)\nTEMP (temperature, degree_C)\nTPOT (temperature potentielle, degree_C)\nCNDC (conductivity, Siemens per metre)\nPSAL (Practical salinity)\nDOX1 (Dissolved oxygen, Micromoles per litre)\nDOX2 (Dissolved oxygen, Micromoles per kilogram)\nOSAT (Oxygen saturation, Micromoles per kilogram)\n... (12 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2018_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2018_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2018/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2018.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2018&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2018 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2021.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2021 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2021.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2021/ | public | EMSO Western Ligurian : Albatross mooring, MICROCAT sensor (NetCDF files 2021-07 to 2023-05) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node\n\ncdm_data_type = TimeSeries\nVARIABLES:\nstationname (station name)\nlatitude (Latitude of measurements, degrees_north)\nlongitude (Longitude of measurements, degrees_east)\ntime (time of measurements, seconds since 1970-01-01T00:00:00Z)\nTIME_QC (Time quality flag)\nTPOT (temperature potentielle, degree_C)\nTEMP (temperature, degree_C)\nTEMP_QC (Temperature quality flag)\nCNDC (conductivity, Siemens per metre)\nCNDC_QC (Conductivity quality flag)\n... (12 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2021_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2021_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2021/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2021.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2021&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2021 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2024.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2024 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2024.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2024/ | public | EMSO Western Ligurian : Albatross mooring, MICROCAT sensor (NetCDF files from 2024-03) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node\n\ncdm_data_type = TimeSeries\nVARIABLES:\nstationname (station name, not applicable)\nlatitude (Latitude of measurements, degrees_north)\nlongitude (Longitude of measurements, degrees_east)\ntime (time of measurements, seconds since 1970-01-01T00:00:00Z)\nTIME_QC (Time quality flag)\nPOTT (temperature potentielle, degree_C)\nTEMP (temperature, degree_C)\nTEMP_QC (Temperature quality flag)\nCNDC (conductivity, Siemens per metre)\nCNDC_QC (Conductivity quality flag)\n... (13 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2024_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2024_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2024/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2024.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2024&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Albatross_Microcat_NetCDF_2024 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_MII_Aquadopp_CSV_2017.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_MII_Aquadopp_CSV_2017 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_MII_Aquadopp_CSV_2017.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_MII_Aquadopp_CSV_2017/ | public | EMSO Western Ligurian : MII, AQUADOPP sensor (CSV files from 2017-09) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node.\n\ncdm_data_type = Point\nVARIABLES:\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\nX_East\nY_North\nZ_Up\nAmplitude_X\nAmplitude_Y\nAmplitude_Z\nBatterie\n... (8 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_MII_Aquadopp_CSV_2017_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_MII_Aquadopp_CSV_2017_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_MII_Aquadopp_CSV_2017/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_MII_Aquadopp_CSV_2017.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_MII_Aquadopp_CSV_2017&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_MII_Aquadopp_CSV_2017 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_MII_Aquadopp_NetCDF_2017.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_MII_Aquadopp_NetCDF_2017 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_MII_Aquadopp_NetCDF_2017.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_MII_Aquadopp_NetCDF_2017/ | public | EMSO Western Ligurian : MII, AQUADOPP sensor (NetCDF files from 2017-09) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node.\n\ncdm_data_type = TimeSeries\nVARIABLES:\nstationname (station name)\nlatitude (Latitude of measurements, degrees_north)\nlongitude (Longitude of measurements, degrees_east)\ntime (time of measurements, seconds since 1970-01-01T00:00:00Z)\nTIME_QC (Time quality flag)\nDEPH (depth of measurements, Metres)\nRFVL_X (Metres per second)\nRFVL_Y (Y_North, Metres per second)\nLRZA (Metres per second)\nXYZ_QC\n... (22 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_MII_Aquadopp_NetCDF_2017_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_MII_Aquadopp_NetCDF_2017_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_MII_Aquadopp_NetCDF_2017/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_MII_Aquadopp_NetCDF_2017.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_MII_Aquadopp_NetCDF_2017&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_MII_Aquadopp_NetCDF_2017 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_MII_Cstar_NetCDF_2017.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_MII_Cstar_NetCDF_2017 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_MII_Cstar_NetCDF_2017.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_MII_Cstar_NetCDF_2017/ | public | EMSO Western Ligurian : MII, CSTAR sensor (NetCDF files from 2017-09) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node.\n\ncdm_data_type = TimeSeries\nVARIABLES:\nstationname (station name)\nlatitude (Latitude of measurements, degrees_north)\nlongitude (Longitude of measurements, degrees_east)\ntime (time of measurements, seconds since 1970-01-01T00:00:00Z)\nTIME_QC (Time quality flag)\nDEPH (depth of measurements, Metres)\nrefCount (ref Count, 1)\nrefCount_QC (refCount quality flag)\nsignalCount (signal Count, 1)\nsignalCount_QC (signalCount quality flag)\n... (6 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_MII_Cstar_NetCDF_2017_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_MII_Cstar_NetCDF_2017_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_MII_Cstar_NetCDF_2017/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_MII_Cstar_NetCDF_2017.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_MII_Cstar_NetCDF_2017&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_MII_Cstar_NetCDF_2017 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_MII_Microcat_NetCDF_2017.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_MII_Microcat_NetCDF_2017 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_MII_Microcat_NetCDF_2017.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_MII_Microcat_NetCDF_2017/ | public | EMSO Western Ligurian : MII, MICROCAT sensor (NetCDF files from 2017-09) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node.\n\ncdm_data_type = TimeSeries\nVARIABLES:\nstationname (station name)\nlatitude (Latitude of measurements, degrees_north)\nlongitude (Longitude of measurements, degrees_east)\ntime (time of measurements, seconds since 1970-01-01T00:00:00Z)\nTIME_QC (Time quality flag)\nTEMP (temperature, degree_C)\nTEMP_QC (Temperature quality flag)\nCNDC (conductivity, Siemens per metre)\nCNDC_QC (Conductivity quality flag)\nPRES (pressure, Decibars)\nPRES_QC (Pressure quality flag)\nDEPH (depth of measurements, Metres)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_MII_Microcat_NetCDF_2017_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_MII_Microcat_NetCDF_2017_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_MII_Microcat_NetCDF_2017/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_MII_Microcat_NetCDF_2017.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_MII_Microcat_NetCDF_2017&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_MII_Microcat_NetCDF_2017 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_MII_Oxygen_NetCDF_2017.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_MII_Oxygen_NetCDF_2017 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_MII_Oxygen_NetCDF_2017.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_MII_Oxygen_NetCDF_2017/ | public | EMSO Western Ligurian : MII, OXYGEN sensor (NetCDF files from 2017-09) | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is also part of KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation connected to KM3NeT is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS). The ALBATROSS line is an inductive line (2000 m) composed of an acoustic communication system, two inductive cables equipped with Conductivity, Temperature, Depth (CTD)-O2 sensors, current meters and two instrumented buoys. This line is deployed at a distance of 2-3 kilometers from the MII, and communication on land is done by an acoustic link with the MII, and electro-optical cable via the KM3NeT node.\n\ncdm_data_type = TimeSeries\nVARIABLES:\nstationname (station name)\nlatitude (Latitude of measurements, degrees_north)\nlongitude (Longitude of measurements, degrees_east)\ntime (time of measurements, seconds since 1970-01-01T00:00:00Z)\nTIME_QC (Time quality flag)\nDOX1 (Dissolved oxygen, Micromoles per litre)\nDOX_QC (Oxygen quality flag)\nOSAT (Oxygen saturation, Percent)\nOSAT_QC (Oxygen Saturation quality flag)\nTEMP (temperature, degree_C)\n... (5 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_MII_Oxygen_NetCDF_2017_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_MII_Oxygen_NetCDF_2017_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_MII_Oxygen_NetCDF_2017/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_MII_Oxygen_NetCDF_2017.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_MII_Oxygen_NetCDF_2017&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_MII_Oxygen_NetCDF_2017 | ||
https://erddap.osupytheas.fr/erddap/tabledap/EMSO_LO_BJS_ADCP_NCF_2023.subset | https://erddap.osupytheas.fr/erddap/tabledap/EMSO_LO_BJS_ADCP_NCF_2023 | https://erddap.osupytheas.fr/erddap/tabledap/EMSO_LO_BJS_ADCP_NCF_2023.graph | https://erddap.osupytheas.fr/erddap/files/EMSO_LO_BJS_ADCP_NCF_2023/ | public | EMSO-LO Western Ligurian : BJS_Bathydock, ADCP sensor (NetCDF files from 2023-09-20 | The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian (EMSO-WL) is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is located close by KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation at the EMSO-WL station is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS) as well as a junction box (BJS). The BathyFamily is a package of innovative multi-instrumented platforms to observe the deep sea. BathyBot is an Internet Operated Vehicle (IOV) deployed from a landing station (BathyDock), and close to BathyReef a 3D-printed biomimetic colonizer.\n\ncdm_data_type = TimeSeries\nVARIABLES:\nlatitude (degrees_north)\nlongitude (degrees_east)\nPOSITION_QC (quality flag for position)\ndepth (depth of measurements, m)\nDEPH_QC (Profondeur quality flag)\ntime (time of measurements, seconds since 1970-01-01T00:00:00Z)\nTIME_QC (Time quality flag)\nHEAD (Heading, degrees)\nHead_QC (Heading quality code)\nPITCH (degrees)\nPitch_QC (Pitch quality code)\n... (26 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/EMSO_LO_BJS_ADCP_NCF_2023_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/EMSO_LO_BJS_ADCP_NCF_2023_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/EMSO_LO_BJS_ADCP_NCF_2023/index.htmlTable | https://www.seadatanet.org/ | http://erddap.osupytheas.fr/erddap/rss/EMSO_LO_BJS_ADCP_NCF_2023.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=EMSO_LO_BJS_ADCP_NCF_2023&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | EMSO_LO_BJS_ADCP_NCF_2023 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Bathybot_Aquadopp_CSV_2023.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Bathybot_Aquadopp_CSV_2023 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Bathybot_Aquadopp_CSV_2023.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Bathybot_Aquadopp_CSV_2023/ | public | EMSO-LO Western Ligurian : BJS_Bathydock_Bathybot Aquadopp sensor (CSV files from 2023-09-20) | EMSO-LO Western Ligurian : BathyBot, Aquadopp sensor (Network Common Data Format (NetCDF) files from 2023-04-28). The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian (EMSO-WL) is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is located close by KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation at the EMSO-WL station is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS) as well as a junction box (BJS). The BathyFamily is a package of innovative multi-instrumented platforms to observe the deep sea. BathyBot is an Internet Operated Vehicle (IOV) deployed from a landing station (BathyDock), and close to BathyReef a 3D-printed biomimetic colonizer\n\ncdm_data_type = Point\nVARIABLES:\ntime (Datetime, seconds since 1970-01-01T00:00:00Z)\nProfondeur\nlatitude (degrees_north)\nlongitude (degrees_east)\nX_East (m.s-1)\nY_North (m.s-1)\nZ_up (m.s-1)\nAmplitude_X (1)\nAmplitude_Y (1)\nAmplitude_Z (1)\n... (10 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_Bathybot_Aquadopp_CSV_2023_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_Bathybot_Aquadopp_CSV_2023_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Bathybot_Aquadopp_CSV_2023/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Bathybot_Aquadopp_CSV_2023.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Bathybot_Aquadopp_CSV_2023&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Bathybot_Aquadopp_CSV_2023 | ||
https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Bathybot_Aquadopp_NetCDF_2023.subset | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Bathybot_Aquadopp_NetCDF_2023 | https://erddap.osupytheas.fr/erddap/tabledap/Emso_Western_Ligurian_Bathybot_Aquadopp_NetCDF_2023.graph | https://erddap.osupytheas.fr/erddap/files/Emso_Western_Ligurian_Bathybot_Aquadopp_NetCDF_2023/ | public | EMSO-LO Western Ligurian : BJS_Bathydock_Bathybot Aquadopp sensor (NetCDF files from 2023-09-20) | EMSO-LO Western Ligurian : BathyBot, Aquadopp sensor (Network Common Data Format (NetCDF) files from 2023-04-28). The European Multidisciplinary Seafloor and water column Observatory (EMSO) is a research infrastructure distributed throughout Europe for seabed and water column observatories. It aims to further explore the oceans, better understand the phenomena that occur on the seabed, and elucidate the critical role that these phenomena play in global Earth systems. This observatory is based on observation sites (or nodes) that have been deployed in strategic locations in European seas, from the Arctic to the Atlantic, from the Mediterranean to the Black Sea. There are currently eleven deep water nodes plus four shallow water test nodes. EMSO Western Ligurian (EMSO-WL) is one of these permanent underwater observatories located in the Ligurian Sea and is deployed off Toulon, France. This region was chosen for its particular scientific interests such as: seismicity, topography, turbidity, biodiversity, water mass dynamics and organic matter flow. This underwater observation network is located close by KM3NeT (https://www.km3net.org/) which has a modular topology designed to connect up to 120 neutrino detection units. Earth and Sea Science (ESS) instrumentation at the EMSO-WL station is based on two complementary components: an instrumented interface module (MII) and an autonomous instrumented line (ALBATROSS) as well as a junction box (BJS). The BathyFamily is a package of innovative multi-instrumented platforms to observe the deep sea. BathyBot is an Internet Operated Vehicle (IOV) deployed from a landing station (BathyDock), and close to BathyReef a 3D-printed biomimetic colonizer\n\ncdm_data_type = TimeSeries\nVARIABLES:\nstation_id (station name, Not applicable)\nlatitude (Latitude of measurements, degrees_north)\nlongitude (Longitude of measurements, degrees_east)\nPosition_QC (quality flag for position)\nDEPH (depth of measurements, Metres)\nDeph_QC (Profondeur quality flag)\ntime (time of measurements, seconds since 1970-01-01T00:00:00Z)\nTime_QC (Time quality flag)\nEWCT (X_East eastward_sea_water_velocity, Metres per second)\nNSCT (Y_North northward_sea_water_velocity, Metres per second)\n... (26 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/Emso_Western_Ligurian_Bathybot_Aquadopp_NetCDF_2023_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/Emso_Western_Ligurian_Bathybot_Aquadopp_NetCDF_2023_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/Emso_Western_Ligurian_Bathybot_Aquadopp_NetCDF_2023/index.htmlTable | http://www.emso-fr.org/EMSO-France | http://erddap.osupytheas.fr/erddap/rss/Emso_Western_Ligurian_Bathybot_Aquadopp_NetCDF_2023.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=Emso_Western_Ligurian_Bathybot_Aquadopp_NetCDF_2023&showErrors=false&email= | MIO UMR 7294 CNRS / OSU Pytheas | Emso_Western_Ligurian_Bathybot_Aquadopp_NetCDF_2023 | ||
log in | ICOS Meteo files (CSV files) station OHP ICOS, Projet ICOS Observatoire Haute Provence. | ICOS Meteo files (CSV files) station OHP ICOS - Projet ICOS Observatoire Haute Provence. fchier MTO. Observatoire Sciences Univers\n\ncdm_data_type = Point\nVARIABLES:\nstation\nlatitude (degrees_north)\nlongitude (degrees_east)\ntime (seconds since 1970-01-01T00:00:00Z)\nair_temp10_degree_C (Air Temp10 [degree C])\nair_pressure10_hpa (Air Pressure)\nhumidity10_percent (Humidity10 [percent %])\nwind_speed10_m_s_1 (Wind Speed)\nwind_direction10_degree (Wind From Direction)\nair_temp50_degree_C (Air Temp50 [degree C])\nhumidity50_percent (Humidity50 [percent %])\nwind_speed50_m_s_1 (Wind Speed)\nwind_direction50_degree (Wind From Direction)\nair_temp100_degree_C (Air Temp100 [degree C])\nhumidity100_percent (Humidity100 [percent %])\nwind_speed100_m_s_1 (Wind Speed)\nwind_direction100_degree (Wind From Direction)\n | OSU Pytheas institut - Observatoire de Haute Provence | CSV_3d66_7f82_fe2d | ||||||||||||
log in | ICOS Meteo files (NetCDF files) station OHP ICOS, Projet ICOS Observatoire Haute Provence | ICOS Meteo files (Network Common Data Format (NetCDF) files) station OHP ICOS - Projet ICOS Observatoire Haute Provence. fchier MTO. Observatoire Sciences Univers (OSU) Pytheas institut data from a local source.\n\ncdm_data_type = TimeSeries\nVARIABLES:\nstationname (station name)\nlatitude (degrees_north)\nlongitude (degrees_east)\ntime (measurement time, seconds since 1970-01-01T00:00:00Z)\nair_pressure10 (Pression Air 10m, hpa)\nair_temp10 (air temperature 10m, degree_C)\nair_temp50 (air temperature 50m, degree_C)\nair_temp100 (air temperature 100m, degree_C)\nair_humidity10 (relative humidity 10m, percent)\nair_humidity50 (relative humidity 50m, percent)\nair_humidity100 (relative humidity 100m, percent)\nwind_speed10 (vitesse du vent 10m, m.s-1)\nwind_speed50 (vitesse du vent 50m, m.s-1)\nwind_speed100 (vitesse du vent 100m, m.s-1)\nwind_direction10 (direction du vent 10m, degree)\nwind_direction50 (direction du vent 50m, degree)\nwind_direction100 (direction du vent 100m, degree)\n | OSU Pytheas institut | mto_c5ff_5ade_e512 | ||||||||||||
https://erddap.osupytheas.fr/erddap/tabledap/JULIO_ADCP_2012.subset | https://erddap.osupytheas.fr/erddap/tabledap/JULIO_ADCP_2012 | https://erddap.osupytheas.fr/erddap/tabledap/JULIO_ADCP_2012.graph | https://erddap.osupytheas.fr/erddap/files/JULIO_ADCP_2012/ | public | Julio ADCP current measurements, 2012 | JULIO - Acoustic Doppler Current Profiler (ADCP) current measurements. JULIO - ADCP ; JULIO (Judicious Location for Intrusions Observations) mooring is located close to the 100 m-deep isobath (around 5.25 degEast and 43.13 degNorth), offshore Marseille. With its bottom-moored (300kHz) ADCP, it enables measuring horizontal currents (every 4 m and every 30 minutes) through the water column, and among others, identifying periods of exchange between the Northern Current and the continental shelf.\n\ncdm_data_type = Other\nVARIABLES:\ndepth (Depth of measurement, m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (Latitude of each location, degrees_north)\nlongitude (Longitude of each location, degrees_east)\nSTATION_ID (Station identifier)\nMPMN (Moored instrument DEPH, m)\nEWCT (Eastward Sea Water Velocity, m s-1)\nNSCT (Northward Sea Water Velocity, m s-1)\nVCSP (Bottom-top current component, m s-1)\nERVV (Error velocity, m s-1)\nCSPD (Speed mean of water current in the water body, m s-1)\nCDIR (Direction (towards) of water current in the water body, m s-1)\nECI1 (Echo intensity per beam 1, count)\nECI2 (Echo intensity per beam 2, count)\nECI3 (Echo intensity per beam 3, count)\nECI4 (Echo intensity per beam 4, count)\nPGB1 (Pings received as a percentage of pings sent per beam 1, percent)\nPGB2 (Pings received as a percentage of pings sent per beam 2, percent)\nPGB3 (Pings received as a percentage of pings sent per beam 3, percent)\nPGB4 (Pings received as a percentage of pings sent per beam 4, percent)\nQCflag (Overall quality flag, 1)\nTIME_QC (Time quality flag, 1)\n... (4 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/JULIO_ADCP_2012_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/JULIO_ADCP_2012_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/JULIO_ADCP_2012/index.htmlTable | https://www.mio.osupytheas.fr/ | http://erddap.osupytheas.fr/erddap/rss/JULIO_ADCP_2012.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=JULIO_ADCP_2012&showErrors=false&email= | MIO UMR7294 CNRS Marseille | JULIO_ADCP_2012 | ||
https://erddap.osupytheas.fr/erddap/tabledap/JULIO_ADCP_2013.subset | https://erddap.osupytheas.fr/erddap/tabledap/JULIO_ADCP_2013 | https://erddap.osupytheas.fr/erddap/tabledap/JULIO_ADCP_2013.graph | https://erddap.osupytheas.fr/erddap/files/JULIO_ADCP_2013/ | public | Julio ADCP current measurements, 2013 | JULIO - Acoustic Doppler Current Profiler (ADCP) current measurements. JULIO - ADCP ; JULIO (Judicious Location for Intrusions Observations) moori\nng is located close to the 100 m-deep isobath (around 5.25 degEast and 43.13 degNorth), offshore Marseille. With its bottom-moored (300kHz) ADCP, it enables measuring horizon\ntal currents (every 4 m and every 30 minutes) through the water column, and among others, identifying periods of exchange between the Northern Current and the continental she\nlf.\n\ncdm_data_type = Other\nVARIABLES:\ndepth (Depth of measurement, m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (Latitude of each location, degrees_north)\nlongitude (Longitude of each location, degrees_east)\nSTATION_ID (Station identifier)\nMPMN (Moored instrument DEPH, m)\nEWCT (Eastward Sea Water Velocity, m s-1)\nNSCT (Northward Sea Water Velocity, m s-1)\nVCSP (Bottom-top current component, m s-1)\nERVV (Error velocity, m s-1)\nCSPD (Speed mean of water current in the water body, m s-1)\nCDIR (Direction (towards) of water current in the water body, m s-1)\nECI1 (Echo intensity per beam 1, count)\nECI2 (Echo intensity per beam 2, count)\nECI3 (Echo intensity per beam 3, count)\nECI4 (Echo intensity per beam 4, count)\nPGB1 (Pings received as a percentage of pings sent per beam 1, percent)\nPGB2 (Pings received as a percentage of pings sent per beam 2, percent)\nPGB3 (Pings received as a percentage of pings sent per beam 3, percent)\nPGB4 (Pings received as a percentage of pings sent per beam 4, percent)\nQCflag (Overall quality flag, 1)\n... (5 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/JULIO_ADCP_2013_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/JULIO_ADCP_2013_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/JULIO_ADCP_2013/index.htmlTable | https://www.mio.osupytheas.fr/ | http://erddap.osupytheas.fr/erddap/rss/JULIO_ADCP_2013.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=JULIO_ADCP_2013&showErrors=false&email= | MIO UMR7294 CNRS Marseille | JULIO_ADCP_2013 | ||
https://erddap.osupytheas.fr/erddap/tabledap/JULIO_ADCP_2014.subset | https://erddap.osupytheas.fr/erddap/tabledap/JULIO_ADCP_2014 | https://erddap.osupytheas.fr/erddap/tabledap/JULIO_ADCP_2014.graph | https://erddap.osupytheas.fr/erddap/files/JULIO_ADCP_2014/ | public | Julio ADCP current measurements, 2014 | JULIO - Acoustic Doppler Current Profiler (ADCP) current measurements. JULIO - ADCP ; JULIO (Judicious Location for Intrusions Observations) moori\nng is located close to the 100 m-deep isobath (around 5.25 degEast and 43.13 degNorth), offshore Marseille. With its bottom-moored (300kHz) ADCP, it enables measuring horizon\ntal currents (every 4 m and every 30 minutes) through the water column, and among others, identifying periods of exchange between the Northern Current and the continental she\nlf.\n\ncdm_data_type = Other\nVARIABLES:\ndepth (Depth of measurement, m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (Latitude of each location, degrees_north)\nlongitude (Longitude of each location, degrees_east)\nSTATION_ID (Station identifier)\nMPMN (Moored instrument DEPH, m)\nEWCT (Eastward Sea Water Velocity, m s-1)\nNSCT (Northward Sea Water Velocity, m s-1)\nVCSP (Bottom-top current component, m s-1)\nERVV (Error velocity, m s-1)\nCSPD (Speed mean of water current in the water body, m s-1)\nCDIR (Direction (towards) of water current in the water body, m s-1)\nECI1 (Echo intensity per beam 1, count)\nECI2 (Echo intensity per beam 2, count)\nECI3 (Echo intensity per beam 3, count)\nECI4 (Echo intensity per beam 4, count)\nPGB1 (Pings received as a percentage of pings sent per beam 1, percent)\nPGB2 (Pings received as a percentage of pings sent per beam 2, percent)\nPGB3 (Pings received as a percentage of pings sent per beam 3, percent)\nPGB4 (Pings received as a percentage of pings sent per beam 4, percent)\nQCflag (Overall quality flag, 1)\n... (5 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/JULIO_ADCP_2014_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/JULIO_ADCP_2014_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/JULIO_ADCP_2014/index.htmlTable | https://www.mio.osupytheas.fr/ | http://erddap.osupytheas.fr/erddap/rss/JULIO_ADCP_2014.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=JULIO_ADCP_2014&showErrors=false&email= | MIO UMR7294 CNRS Marseille | JULIO_ADCP_2014 | ||
https://erddap.osupytheas.fr/erddap/tabledap/JULIO_ADCP_2020.subset | https://erddap.osupytheas.fr/erddap/tabledap/JULIO_ADCP_2020 | https://erddap.osupytheas.fr/erddap/tabledap/JULIO_ADCP_2020.graph | https://erddap.osupytheas.fr/erddap/files/JULIO_ADCP_2020/ | public | Julio ADCP current measurements, 2020 | JULIO - Acoustic Doppler Current Profiler (ADCP) current measurements. JULIO - ADCP ; JULIO (Judicious Location for Intrusions Observations) moori\nng is located close to the 100 m-deep isobath (around 5.25 degEast and 43.13 degNorth), offshore Marseille. With its bottom-moored (300kHz) ADCP, it enables measuring horizon\ntal currents (every 4 m and every 30 minutes) through the water column, and among others, identifying periods of exchange between the Northern Current and the continental she\nlf.\n\ncdm_data_type = Other\nVARIABLES:\ndepth (Depth of measurement, m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (Latitude of each location, degrees_north)\nlongitude (Longitude of each location, degrees_east)\nSTATION_ID (Station identifier)\nMPMN (Moored instrument DEPH, m)\nEWCT (Eastward Sea Water Velocity, m s-1)\nNSCT (Northward Sea Water Velocity, m s-1)\nVCSP (Bottom-top current component, m s-1)\nERVV (Error velocity, m s-1)\nCSPD (Speed mean of water current in the water body, m s-1)\nCDIR (Direction (towards) of water current in the water body, m s-1)\nECI1 (Echo intensity per beam 1, count)\nECI2 (Echo intensity per beam 2, count)\nECI3 (Echo intensity per beam 3, count)\nECI4 (Echo intensity per beam 4, count)\nPGB1 (Pings received as a percentage of pings sent per beam 1, percent)\nPGB2 (Pings received as a percentage of pings sent per beam 2, percent)\nPGB3 (Pings received as a percentage of pings sent per beam 3, percent)\nPGB4 (Pings received as a percentage of pings sent per beam 4, percent)\nQCflag (Overall quality flag, 1)\n... (5 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/JULIO_ADCP_2020_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/JULIO_ADCP_2020_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/JULIO_ADCP_2020/index.htmlTable | https://www.mio.osupytheas.fr/ | http://erddap.osupytheas.fr/erddap/rss/JULIO_ADCP_2020.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=JULIO_ADCP_2020&showErrors=false&email= | MIO UMR7294 CNRS Marseille | JULIO_ADCP_2020 | ||
https://erddap.osupytheas.fr/erddap/tabledap/JULIO_ADCP_2021.subset | https://erddap.osupytheas.fr/erddap/tabledap/JULIO_ADCP_2021 | https://erddap.osupytheas.fr/erddap/tabledap/JULIO_ADCP_2021.graph | https://erddap.osupytheas.fr/erddap/files/JULIO_ADCP_2021/ | public | Julio ADCP current measurements, 2021 | JULIO - Acoustic Doppler Current Profiler (ADCP) current measurements. JULIO - ADCP ; JULIO (Judicious Location for Intrusions Observations) moori\nng is located close to the 100 m-deep isobath (around 5.25 degEast and 43.13 degNorth), offshore Marseille. With its bottom-moored (300kHz) ADCP, it enables measuring horizon\ntal currents (every 4 m and every 30 minutes) through the water column, and among others, identifying periods of exchange between the Northern Current and the continental she\nlf.\n\ncdm_data_type = Other\nVARIABLES:\ndepth (Depth of measurement, m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (Latitude of each location, degrees_north)\nlongitude (Longitude of each location, degrees_east)\nSTATION_ID (Station identifier)\nMPMN (Moored instrument DEPH, m)\nEWCT (Eastward Sea Water Velocity, m s-1)\nNSCT (Northward Sea Water Velocity, m s-1)\nVCSP (Bottom-top current component, m s-1)\nERVV (Error velocity, m s-1)\nCSPD (Speed mean of water current in the water body, m s-1)\nCDIR (Direction (towards) of water current in the water body, m s-1)\nECI1 (Echo intensity per beam 1, count)\nECI2 (Echo intensity per beam 2, count)\nECI3 (Echo intensity per beam 3, count)\nECI4 (Echo intensity per beam 4, count)\nPGB1 (Pings received as a percentage of pings sent per beam 1, percent)\nPGB2 (Pings received as a percentage of pings sent per beam 2, percent)\nPGB3 (Pings received as a percentage of pings sent per beam 3, percent)\nPGB4 (Pings received as a percentage of pings sent per beam 4, percent)\nQCflag (Overall quality flag, 1)\n... (5 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/JULIO_ADCP_2021_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/JULIO_ADCP_2021_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/JULIO_ADCP_2021/index.htmlTable | https://www.mio.osupytheas.fr/ | http://erddap.osupytheas.fr/erddap/rss/JULIO_ADCP_2021.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=JULIO_ADCP_2021&showErrors=false&email= | MIO UMR7294 CNRS Marseille | JULIO_ADCP_2021 | ||
https://erddap.osupytheas.fr/erddap/tabledap/JULIO_ADCP_2022.subset | https://erddap.osupytheas.fr/erddap/tabledap/JULIO_ADCP_2022 | https://erddap.osupytheas.fr/erddap/tabledap/JULIO_ADCP_2022.graph | https://erddap.osupytheas.fr/erddap/files/JULIO_ADCP_2022/ | public | Julio ADCP current measurements, 2022 | JULIO (Judicious Location for Intrusions Observations) mooring is located close to the 100 m-deep isobath (around 5.25?E and 43.13?N), offshore Marseille. With its bottom-moored (300kHz) Acoustic Doppler Current Profiler (ADCP), it enables measuring horizontal currents (every 4 m and every 30 minutes) through the water column, and among others, identifying periods of exchange between the Northern Current and the continental shelf.\n\ncdm_data_type = Other\nVARIABLES:\nSTATION (Station identifier)\ndepth (DEPH of measurement, m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (Latitude of each location, degrees_north)\nlongitude (Longitude of each location, degrees_east)\nMPMN (Moored instrument DEPH, m)\nEWCT (Eastward Sea Water Velocity, m s-1)\nNSCT (Northward Sea Water Velocity, m s-1)\nVCSP (Bottom-top current component, m s-1)\nERVV (Error velocity, m s-1)\nCSPD (Speed mean of water current in the water body, m s-1)\nCDIR (Direction (towards) of water current in the water body, m s-1)\nECI1 (Echo intensity per beam 1, count)\nECI2 (Echo intensity per beam 2, count)\nECI3 (Echo intensity per beam 3, count)\nECI4 (Echo intensity per beam 4, count)\nPGB1 (Pings received as a percentage of pings sent per beam 1, percent)\nPGB2 (Pings received as a percentage of pings sent per beam 2, percent)\nPGB3 (Pings received as a percentage of pings sent per beam 3, percent)\nPGB4 (Pings received as a percentage of pings sent per beam 4, percent)\nQCflag (Overall quality flag, 1)\nTIME_QC (Time quality flag, 1)\nPOSITION_QC (Position quality flag, 1)\nEWCT_QC (Overall quality flag, 1)\nNSCT_QC (Overall quality flag, 1)\nVCSP_QC (Overall quality flag, 1)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/JULIO_ADCP_2022_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/JULIO_ADCP_2022_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/JULIO_ADCP_2022/index.htmlTable | https://dataset.osupytheas.fr/geonetwork/srv/fre/catalog.search;jsessionid=2CA212C4AE3E6178F901C9DE2EA2EC98#/metadata/ap_mio_20231114 | http://erddap.osupytheas.fr/erddap/rss/JULIO_ADCP_2022.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=JULIO_ADCP_2022&showErrors=false&email= | MIO UMR7294 CNRS / OSU Pytheas | JULIO_ADCP_2022 | ||
https://erddap.osupytheas.fr/erddap/tabledap/meteo_frioul_osu_pytheas_2007_2019.subset | https://erddap.osupytheas.fr/erddap/tabledap/meteo_frioul_osu_pytheas_2007_2019 | https://erddap.osupytheas.fr/erddap/tabledap/meteo_frioul_osu_pytheas_2007_2019.graph | https://erddap.osupytheas.fr/erddap/files/meteo_frioul_osu_pytheas_2007_2019/ | public | Meteorologie locale en baie de Marseille : Frioul (2007-2019) | Meteorological data from the Bay of Marseille based on the measurements taken on the site located on the Pomegues island\n\ncdm_data_type = Point\nVARIABLES:\ntime (Datetime, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\nDirection_Max (degree)\nRafale_m_s (Rafale(m/s), m.s-1)\nVitesse_moyenne_max (Vitesse Moyenne Max (m/s), m.s-1)\nDirection (Direction (degree), degree)\nTemperature (Temperature (degree C), degree_C)\nHumidite_relative (Humidite Relative (%), %)\nRayonnement_J_cm2 (Rayonnement(J/cm2), J.cm-2)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/meteo_frioul_osu_pytheas_2007_2019_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/meteo_frioul_osu_pytheas_2007_2019_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/meteo_frioul_osu_pytheas_2007_2019/index.htmlTable | https://dataset.osupytheas.fr/geonetwork/srv/fre/catalog.search#/metadata/5c9f6377-726b-436b-aa0f-ecc32803ef88 | http://erddap.osupytheas.fr/erddap/rss/meteo_frioul_osu_pytheas_2007_2019.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=meteo_frioul_osu_pytheas_2007_2019&showErrors=false&email= | OSU Pytheas UMS 3470 CNRS | meteo_frioul_osu_pytheas_2007_2019 | ||
https://erddap.osupytheas.fr/erddap/tabledap/meteo_frioul_osu_pytheas_2024.subset | https://erddap.osupytheas.fr/erddap/tabledap/meteo_frioul_osu_pytheas_2024 | https://erddap.osupytheas.fr/erddap/tabledap/meteo_frioul_osu_pytheas_2024.graph | https://erddap.osupytheas.fr/erddap/files/meteo_frioul_osu_pytheas_2024/ | public | Meteorologie locale en baie de Marseille : Frioul (from 2024-06) | Meteorological data from the Bay of Marseille based on the measurements taken on the site located on the Pomegues island (Lat 43.2744, Long 5.3072)\n\ncdm_data_type = Point\nVARIABLES:\ntime (Date Time, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\nBattery (Battery [volts], volts)\nInternal_Temperature (Internal Temperature [degree C], degree_C)\nAir_Temperature (Air Temperature [degree C], degree_C)\nHumidity (Humidity [%], percent %)\nDew_point (Dew Point [degree C], degree_C)\nWind_speed (m.s-1)\nWind_Direction (Wind From Direction, degree)\nSolar_Radiation (Solar Radiation [W.m-2], W.m-2)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/meteo_frioul_osu_pytheas_2024_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/meteo_frioul_osu_pytheas_2024_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/meteo_frioul_osu_pytheas_2024/index.htmlTable | https://dataset.osupytheas.fr/geonetwork/srv/fre/catalog.search#/metadata/5c9f6377-726b-436b-aa0f-ecc32803ef88 | http://erddap.osupytheas.fr/erddap/rss/meteo_frioul_osu_pytheas_2024.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=meteo_frioul_osu_pytheas_2024&showErrors=false&email= | OSU Pytheas UMS 3470 CNRS | meteo_frioul_osu_pytheas_2024 | ||
https://erddap.osupytheas.fr/erddap/tabledap/meteo_endoume_1236 | https://erddap.osupytheas.fr/erddap/tabledap/meteo_endoume_1236.graph | https://erddap.osupytheas.fr/erddap/files/meteo_endoume_1236/ | public | Meteorologie locale en baie de Marseille : site Endoume | Meteorological data from Marseille based on the measurements taken from Endoume site\n\ncdm_data_type = Point\nVARIABLES:\ntime (Datetime, seconds since 1970-01-01T00:00:00Z)\ntemperature_C (Temperature[C], degrees C)\nhumidity (Humidity[%], %)\ndew_point_C (Dew Point[C], degree C)\nsealevel_pressure_hPa (Sealevel Pressure[h Pa], hPa)\navg_wind_speed_m_s (Wind Speed, m.s-1)\ngust_speed_m_s (Wind Speed Of Gust, m.s-1)\nwinddir_degree (Wind From Direction, degree)\nrainfall00 (mm)\nlongitude (degrees_east)\nlatitude (degrees_north)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/meteo_endoume_1236_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/meteo_endoume_1236_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/meteo_endoume_1236/index.htmlTable | http://dataset.osupytheas.fr/ | http://erddap.osupytheas.fr/erddap/rss/meteo_endoume_1236.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=meteo_endoume_1236&showErrors=false&email= | OSU Pytheas UAR 3470 CNRS | meteo_endoume_1236 | |||
https://erddap.osupytheas.fr/erddap/tabledap/meteo_climed_8bcc.subset | https://erddap.osupytheas.fr/erddap/tabledap/meteo_climed_8bcc | https://erddap.osupytheas.fr/erddap/tabledap/meteo_climed_8bcc.graph | https://erddap.osupytheas.fr/erddap/files/meteo_climed_8bcc/ | public | Meteorologie locale site \"climed\" chaine de l'Etoile | Meteorological data from Marseille based on the measurements taken on \"CLIMED\" site chaine de l'Etoile\n\ncdm_data_type = Point\nVARIABLES:\ntime (Datetime, seconds since 1970-01-01T00:00:00Z)\nlongitude (degrees_east)\nlatitude (degrees_north)\nHumidity (Humidity (%), percent %)\nTemperature_Air (Temperature Air (degree C), degree C)\nSolar_radiation (Solar Radiation (W.m^-2), W.m-2)\nWind_direction (degree)\nWind_speed (m.s-1)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/meteo_climed_8bcc_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/meteo_climed_8bcc_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/meteo_climed_8bcc/index.htmlTable | http://dataset.osupytheas.fr | http://erddap.osupytheas.fr/erddap/rss/meteo_climed_8bcc.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=meteo_climed_8bcc&showErrors=false&email= | OSU Pytheas UAR 3470 CNRS | meteo_climed_8bcc | ||
https://erddap.osupytheas.fr/erddap/tabledap/meteo_toulon_2ce5.subset | https://erddap.osupytheas.fr/erddap/tabledap/meteo_toulon_2ce5 | https://erddap.osupytheas.fr/erddap/tabledap/meteo_toulon_2ce5.graph | https://erddap.osupytheas.fr/erddap/files/meteo_toulon_2ce5/ | public | Meteorologie locale site Toulon | Meteorological data from Toulon France (Var)\n\ncdm_data_type = Point\nVARIABLES:\ntime (Datetime, seconds since 1970-01-01T00:00:00Z)\nTemperature (Temperature (degree C))\nHumidity (Humidity (%))\nRainfall (Rainfall (6mn))\nSolar_radiation (Solar Radiation (W.m^-2))\nWind_Direction (Wind From Direction)\nWind_speed\nGust_Speed (Wind Speed Of Gust)\nGust_Direction (Gust Direction (degree))\nAir_pressure_at_station_level (Air Pressure)\nAir_pressure_at_sea_levele (Air Pressure)\nlatitude (degrees_north)\nlongitude (degrees_east)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/meteo_toulon_2ce5_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/meteo_toulon_2ce5_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/meteo_toulon_2ce5/index.htmlTable | https://dataset.osupytheas.fr/ | http://erddap.osupytheas.fr/erddap/rss/meteo_toulon_2ce5.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=meteo_toulon_2ce5&showErrors=false&email= | OSU Pytheas UAR 3470 CNRS | meteo_toulon_2ce5 | ||
https://erddap.osupytheas.fr/erddap/tabledap/AMOP_3b75_05e1_8951.subset | https://erddap.osupytheas.fr/erddap/tabledap/AMOP_3b75_05e1_8951 | https://erddap.osupytheas.fr/erddap/tabledap/AMOP_3b75_05e1_8951.graph | https://erddap.osupytheas.fr/erddap/files/AMOP_3b75_05e1_8951/ | public | OCARINA AMOP 2014 experiment, prototype 1, level 2 surface and air-sea turbulent fluxes | OCARINA level 2 data, calibrated. Turbulent air-sea fluxes and associated variables from the OCARINA wave-following and drifting platform (Bourras et al. 2014, DOI: 10.1175/JTECH-D-13-00055.)\n\ncdm_data_type = TimeSeries\nVARIABLES:\ntime2 (Time)\ntime (seconds since 1970-01-01T00:00:00Z)\nlongitude (degrees_east)\nlatitude (degrees_north)\npair (Air pressure, hPa)\ntair (Air Temperature, degree_C)\nhur (Relative air humidity, 1)\nsst (degree_C)\nrho (Density of air, kg m-3)\nrlds (downwelling longwave radiation flux, positive downward, W m-2)\nrlus (upwelling longwave radiation flux, positive upward, W m-2)\nrsds (downwelling shortwave radiation flux, positive downward, W m-2)\nrsus (upwelling shortwave radiation flux, positive upward, W m-2)\nwdir (Direction of the wind vector with respect to ground, measured positive clockwise from due north, degrees)\nwspd (Magnitude of wind velocity with respect to ground, m s-1)\nu10n (Equivalent neutral wind extrapolated at a 10-m height, from eddy-covariance calculation, m s-1)\nhsw (Significant wave height, calculated as four times the square root of the integration of the vertical platform velocity, m)\nhsw_day (daily estimate of the significant wave height, calculated as four times the square root of the integration of the vertical platform velocity, m)\nTsw (Inverse of the frequency at the maximum of the power spectrum of the vertical platform velocity (experimental), s)\nTsw_day (Daily estimate of the inverse of the frequency at the maximum of the power spectrum of the vertical platform velocity (experimental), s)\ntauu (Eastward component of the surface wind stress vector, from eddy-covariance calculation, Pa)\ntauv (Northward component of the surface wind stress vector, from eddy-covariance calculation, Pa)\nustar (Turbulent surface friction velocity, from eddy-covariance calculation, m s-1)\nhsv (Turbulent surface buoyancy flux, from eddy-covariance calculation, W m-2)\nzL (Monin-Obukhov ratio, which quantifies surface boundary layer stability, from eddy-covariance calculation, 1)\nustar_bulk (Turbulent surface friction velocity, COARE 3.0 (please see header) drag parameterization adjusted to OCARINA data, m s-1)\n... (12 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/AMOP_3b75_05e1_8951_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/AMOP_3b75_05e1_8951_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/AMOP_3b75_05e1_8951/index.htmlTable | http://dataset.osupytheas.fr/geonetwork/srv/fre/catalog.search#/metadata/9d2f74a1-a7af-4062-a4e9-bd63b904856a | http://erddap.osupytheas.fr/erddap/rss/AMOP_3b75_05e1_8951.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=AMOP_3b75_05e1_8951&showErrors=false&email= | MIO UMR7294 CNRS | AMOP_3b75_05e1_8951 | ||
https://erddap.osupytheas.fr/erddap/tabledap/BBWAVES_2015_proto1_02c1_999c_aa46.subset | https://erddap.osupytheas.fr/erddap/tabledap/BBWAVES_2015_proto1_02c1_999c_aa46 | https://erddap.osupytheas.fr/erddap/tabledap/BBWAVES_2015_proto1_02c1_999c_aa46.graph | https://erddap.osupytheas.fr/erddap/files/BBWAVES_2015_proto1_02c1_999c_aa46/ | public | OCARINA BBWAVES 2015 experiment, prototype 1, level 2 surface and air-sea turbulent fluxes | Turbulent air-sea fluxes and associated variables from the OCARINA wave-following and drifting platform (Bourras et al. 2014, DOI: 10.1175/JTECH-D-13-00055.)\n\ncdm_data_type = TimeSeries\nVARIABLES:\ntime2 (Time)\ntime (seconds since 1970-01-01T00:00:00Z)\nlongitude (degrees_east)\nlatitude (degrees_north)\npair (Air pressure, hPa)\ntair (Air Temperature, degree_C)\nhur (Relative air humidity, 1)\nsst (degree_C)\nrho (Density of air, kg m-3)\nrlds (downwelling longwave radiation flux, positive downward, W m-2)\nrlus (upwelling longwave radiation flux, positive upward, W m-2)\nrsds (downwelling shortwave radiation flux, positive downward, W m-2)\nrsus (upwelling shortwave radiation flux, positive upward, W m-2)\nwdir (Direction of the wind vector with respect to ground, measured positive clockwise from due north, degrees)\nwspd (Magnitude of wind velocity with respect to ground, m s-1)\nu10n (Equivalent neutral wind extrapolated at a 10-m height, from eddy-covariance calculation, m s-1)\nhsw (Significant wave height, calculated as four times the square root of the integration of the vertical platform velocity, m)\nhsw_day (daily estimate of the significant wave height, calculated as four times the square root of the integration of the vertical platform velocity, m)\nTsw (Inverse of the frequency at the maximum of the power spectrum of the vertical platform velocity (experimental), s)\nTsw_day (Daily estimate of the inverse of the frequency at the maximum of the power spectrum of the vertical platform velocity (experimental), s)\ntauu (Eastward component of the surface wind stress vector, from eddy-covariance calculation, Pa)\ntauv (Northward component of the surface wind stress vector, from eddy-covariance calculation, Pa)\nustar (Turbulent surface friction velocity, from eddy-covariance calculation, m s-1)\nhsv (Turbulent surface buoyancy flux, from eddy-covariance calculation, W m-2)\nzL (Monin-Obukhov ratio, which quantifies surface boundary layer stability, from eddy-covariance calculation, 1)\nustar_bulk (Turbulent surface friction velocity, COARE 3.0 (please see header) drag parameterization adjusted to OCARINA data, m s-1)\n... (12 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/BBWAVES_2015_proto1_02c1_999c_aa46_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/BBWAVES_2015_proto1_02c1_999c_aa46_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/BBWAVES_2015_proto1_02c1_999c_aa46/index.htmlTable | http://dataset.osupytheas.fr/geonetwork/srv/fre/catalog.search#/metadata/9d2f74a1-a7af-4062-a4e9-bd63b904856a | http://erddap.osupytheas.fr/erddap/rss/BBWAVES_2015_proto1_02c1_999c_aa46.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=BBWAVES_2015_proto1_02c1_999c_aa46&showErrors=false&email= | MIO UMR7294 CNRS | BBWAVES_2015_proto1_02c1_999c_aa46 | ||
https://erddap.osupytheas.fr/erddap/tabledap/BBWAVES_2015_proto2_0c15_7ba6_2c7c.subset | https://erddap.osupytheas.fr/erddap/tabledap/BBWAVES_2015_proto2_0c15_7ba6_2c7c | https://erddap.osupytheas.fr/erddap/tabledap/BBWAVES_2015_proto2_0c15_7ba6_2c7c.graph | https://erddap.osupytheas.fr/erddap/files/BBWAVES_2015_proto2_0c15_7ba6_2c7c/ | public | OCARINA BBWAVES 2015 experiment, prototype 2, level 2 surface and air-sea turbulent fluxes | Turbulent air-sea fluxes and associated variables from the OCARINA wave-following and drifting platform (Bourras et al. 2014, DOI: 10.1175/JTECH-D-13-00055.)\n\ncdm_data_type = TimeSeries\nVARIABLES:\ntime2 (Time)\ntime (seconds since 1970-01-01T00:00:00Z)\nlongitude (degrees_east)\nlatitude (degrees_north)\npair (Air pressure, hPa)\ntair (Air Temperature, degree_C)\nhur (Relative air humidity, 1)\nsst (degree_C)\nrho (Density of air, kg m-3)\nwdir (Direction of the wind vector with respect to ground, measured positive clockwise from due north, degrees)\nwspd (Magnitude of wind velocity with respect to ground, m s-1)\nu10n (Equivalent neutral wind extrapolated at a 10-m height, from eddy-covariance calculation, m s-1)\nhsw (Significant wave height, calculated as four times the square root of the double integration of the vertical platform acceleration, m)\nhsw_day (daily estimate of the significant wave height, calculated as four times the square root of the double integration of the vertical platform acceleration, m)\nTsw (Inverse of the frequency at the maximum of the power spectrum of the vertical platform velocity (experimental), s)\nTsw_day (Daily estimate of the inverse of the frequency at the maximum of the power spectrum of the vertical platform velocity (experimental), s)\ntauu (Eastward component of the surface wind stress vector, from eddy-covariance calculation, Pa)\ntauv (Northward component of the surface wind stress vector, from eddy-covariance calculation, Pa)\nustar (Turbulent surface friction velocity, from eddy-covariance calculation, m s-1)\nhsv (Turbulent surface buoyancy flux, from eddy-covariance calculation, W m-2)\nzL (Monin-Obukhov ratio, which quantifies surface boundary layer stability, from eddy-covariance calculation, 1)\nustar_bulk (Turbulent surface friction velocity, COARE 3.0 (please see header) drag parameterization adjusted to OCARINA data, m s-1)\nhsv_bulk (Turbulent surface buoyancy flux, positive upward, from bulk calculation, W m-2)\nhfss_bulk (Turbulent surface sensible heat flux, positive upward, from bulk calculation, W m-2)\nhfls_bulk (Turbulent surface latent heat flux, positive upward, from bulk calculation, W m-2)\nzL_bulk (Monin-Obukhov ratio, which quantifies surface boundary layer stability, from bulk calculation, 1)\n... (8 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/BBWAVES_2015_proto2_0c15_7ba6_2c7c_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/BBWAVES_2015_proto2_0c15_7ba6_2c7c_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/BBWAVES_2015_proto2_0c15_7ba6_2c7c/index.htmlTable | http://dataset.osupytheas.fr/geonetwork/srv/fre/catalog.search#/metadata/9d2f74a1-a7af-4062-a4e9-bd63b904856a | http://erddap.osupytheas.fr/erddap/rss/BBWAVES_2015_proto2_0c15_7ba6_2c7c.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=BBWAVES_2015_proto2_0c15_7ba6_2c7c&showErrors=false&email= | MIO UMR7294 CNRS | BBWAVES_2015_proto2_0c15_7ba6_2c7c | ||
https://erddap.osupytheas.fr/erddap/tabledap/BBWAVES_2016_proto1_5ecc_9507_edad.subset | https://erddap.osupytheas.fr/erddap/tabledap/BBWAVES_2016_proto1_5ecc_9507_edad | https://erddap.osupytheas.fr/erddap/tabledap/BBWAVES_2016_proto1_5ecc_9507_edad.graph | https://erddap.osupytheas.fr/erddap/files/BBWAVES_2016_proto1_5ecc_9507_edad/ | public | OCARINA BBWAVES 2016 experiment, prototype 1, level 2 surface and air-sea turbulent fluxes | Turbulent air-sea fluxes and associated variables from the OCARINA wave-following and drifting platform (Bourras et al. 2014, DOI: 10.1175/JTECH-D-13-00055.)\n\ncdm_data_type = TimeSeries\nVARIABLES:\ntime2 (Time)\ntime (seconds since 1970-01-01T00:00:00Z)\nlongitude (degrees_east)\nlatitude (degrees_north)\npair (Air pressure, hPa)\ntair (Air Temperature, degree_C)\nhur (Relative air humidity, 1)\nsst (degree_C)\nrho (Density of air, kg m-3)\nrlds (downwelling longwave radiation flux, positive downward, W m-2)\nrlus (upwelling longwave radiation flux, positive upward, W m-2)\nrsds (downwelling shortwave radiation flux, positive downward, W m-2)\nrsus (upwelling shortwave radiation flux, positive upward, W m-2)\nwdir (Direction of the wind vector with respect to ground, measured positive clockwise from due north, degrees)\nwspd (Magnitude of wind velocity with respect to ground, m s-1)\nu10n (Equivalent neutral wind extrapolated at a 10-m height, from eddy-covariance calculation, m s-1)\nhsw (Significant wave height, calculated as four times the square root of the integration of the vertical platform velocity, m)\nhsw_day (daily estimate of the significant wave height, calculated as four times the square root of the integration of the vertical platform velocity, m)\nTsw (Inverse of the frequency at the maximum of the power spectrum of the vertical platform velocity (experimental), s)\nTsw_day (Daily estimate of the inverse of the frequency at the maximum of the power spectrum of the vertical platform velocity (experimental), s)\ntauu (Eastward component of the surface wind stress vector, from eddy-covariance calculation, Pa)\ntauv (Northward component of the surface wind stress vector, from eddy-covariance calculation, Pa)\nustar (Turbulent surface friction velocity, from eddy-covariance calculation, m s-1)\nhsv (Turbulent surface buoyancy flux, from eddy-covariance calculation, W m-2)\nzL (Monin-Obukhov ratio, which quantifies surface boundary layer stability, from eddy-covariance calculation, 1)\nustar_bulk (Turbulent surface friction velocity, COARE 3.0 (please see header) drag parameterization adjusted to OCARINA data, m s-1)\n... (12 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/BBWAVES_2016_proto1_5ecc_9507_edad_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/BBWAVES_2016_proto1_5ecc_9507_edad_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/BBWAVES_2016_proto1_5ecc_9507_edad/index.htmlTable | http://dataset.osupytheas.fr/geonetwork/srv/fre/catalog.search#/metadata/9d2f74a1-a7af-4062-a4e9-bd63b904856a | http://erddap.osupytheas.fr/erddap/rss/BBWAVES_2016_proto1_5ecc_9507_edad.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=BBWAVES_2016_proto1_5ecc_9507_edad&showErrors=false&email= | MIO UMR7294 CNRS | BBWAVES_2016_proto1_5ecc_9507_edad | ||
https://erddap.osupytheas.fr/erddap/tabledap/FROMVAR_142e_219c_c4aa.subset | https://erddap.osupytheas.fr/erddap/tabledap/FROMVAR_142e_219c_c4aa | https://erddap.osupytheas.fr/erddap/tabledap/FROMVAR_142e_219c_c4aa.graph | https://erddap.osupytheas.fr/erddap/files/FROMVAR_142e_219c_c4aa/ | public | OCARINA FROMVAR 2011 experiment, prototype 1, level 2 surface and air-sea turbulent fluxes | Turbulent air-sea fluxes and associated variables from the OCARINA wave-following and drifting platform (Bourras et al. 2014, DOI: 10.1175/JTECH-D-13-00055.)\n\ncdm_data_type = TimeSeries\nVARIABLES:\ntime2 (Time)\ntime (seconds since 1970-01-01T00:00:00Z)\nlongitude (degrees_east)\nlatitude (degrees_north)\npair (Air pressure, hPa)\ntair (Air Temperature, degree_C)\nhur (Relative air humidity, 1)\nsst (degree_C)\nrho (Density of air, kg m-3)\nrlds (downwelling longwave radiation flux, positive downward, W m-2)\nrlus (upwelling longwave radiation flux, positive upward, W m-2)\nrsds (downwelling shortwave radiation flux, positive downward, W m-2)\nrsus (upwelling shortwave radiation flux, positive upward, W m-2)\nwdir (Direction of the wind vector with respect to ground, measured positive clockwise from due north, degrees)\nwspd (Magnitude of wind velocity with respect to ground, m s-1)\nu10n (Equivalent neutral wind extrapolated at a 10-m height, from eddy-covariance calculation, m s-1)\nhsw (Significant wave height, calculated as four times the square root of the integration of the vertical platform velocity, m)\nhsw_day (daily estimate of the significant wave height, calculated as four times the square root of the integration of the vertical platform velocity, m)\nTsw (Inverse of the frequency at the maximum of the power spectrum of the vertical platform velocity (experimental), s)\nTsw_day (Daily estimate of the inverse of the frequency at the maximum of the power spectrum of the vertical platform velocity (experimental), s)\ntauu (Eastward component of the surface wind stress vector, from eddy-covariance calculation, Pa)\ntauv (Northward component of the surface wind stress vector, from eddy-covariance calculation, Pa)\nustar (Turbulent surface friction velocity, from eddy-covariance calculation, m s-1)\nhsv (Turbulent surface buoyancy flux, from eddy-covariance calculation, W m-2)\nzL (Monin-Obukhov ratio, which quantifies surface boundary layer stability, from eddy-covariance calculation, 1)\nustar_bulk (Turbulent surface friction velocity, COARE 3.0 (please see header) drag parameterization adjusted to OCARINA data, m s-1)\n... (12 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/FROMVAR_142e_219c_c4aa_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/FROMVAR_142e_219c_c4aa_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/FROMVAR_142e_219c_c4aa/index.htmlTable | http://dataset.osupytheas.fr/geonetwork/srv/fre/catalog.search#/metadata/9d2f74a1-a7af-4062-a4e9-bd63b904856a | http://erddap.osupytheas.fr/erddap/rss/FROMVAR_142e_219c_c4aa.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=FROMVAR_142e_219c_c4aa&showErrors=false&email= | MIO UMR7294 CNRS | FROMVAR_142e_219c_c4aa | ||
https://erddap.osupytheas.fr/erddap/tabledap/STRASSE_89bd_108e_d909.subset | https://erddap.osupytheas.fr/erddap/tabledap/STRASSE_89bd_108e_d909 | https://erddap.osupytheas.fr/erddap/tabledap/STRASSE_89bd_108e_d909.graph | https://erddap.osupytheas.fr/erddap/files/STRASSE_89bd_108e_d909/ | public | OCARINA STRASSE 2012 experiment, prototype 1, level 2 surface and air-sea turbulent fluxes | Turbulent air-sea fluxes and associated variables from the OCARINA wave-following and drifting platform (Bourras et al. 2014, DOI: 10.1175/JTECH-D-13-00055.)\n\ncdm_data_type = TimeSeries\nVARIABLES:\ntime2 (Time)\ntime (seconds since 1970-01-01T00:00:00Z)\nlongitude (degrees_east)\nlatitude (degrees_north)\npair (Air pressure, hPa)\ntair (Air Temperature, degree_C)\nhur (Relative air humidity, 1)\nsst (degree_C)\nrho (Density of air, kg m-3)\nrlds (downwelling longwave radiation flux, positive downward, W m-2)\nrlus (upwelling longwave radiation flux, positive upward, W m-2)\nrsds (downwelling shortwave radiation flux, positive downward, W m-2)\nrsus (upwelling shortwave radiation flux, positive upward, W m-2)\nwdir (Direction of the wind vector with respect to ground, measured positive clockwise from due north, degrees)\nwspd (Magnitude of wind velocity with respect to ground, m s-1)\nu10n (Equivalent neutral wind extrapolated at a 10-m height, from eddy-covariance calculation, m s-1)\nhsw (Significant wave height, calculated as four times the square root of the integration of the vertical platform velocity, m)\nhsw_day (daily estimate of the significant wave height, calculated as four times the square root of the integration of the vertical platform velocity, m)\nTsw (Inverse of the frequency at the maximum of the power spectrum of the vertical platform velocity (experimental), s)\nTsw_day (Daily estimate of the inverse of the frequency at the maximum of the power spectrum of the vertical platform velocity (experimental), s)\ntauu (Eastward component of the surface wind stress vector, from eddy-covariance calculation, Pa)\ntauv (Northward component of the surface wind stress vector, from eddy-covariance calculation, Pa)\nustar (Turbulent surface friction velocity, from eddy-covariance calculation, m s-1)\nhsv (Turbulent surface buoyancy flux, from eddy-covariance calculation, W m-2)\nzL (Monin-Obukhov ratio, which quantifies surface boundary layer stability, from eddy-covariance calculation, 1)\nustar_bulk (Turbulent surface friction velocity, COARE 3.0 (please see header) drag parameterization adjusted to OCARINA data, m s-1)\n... (12 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/STRASSE_89bd_108e_d909_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/STRASSE_89bd_108e_d909_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/STRASSE_89bd_108e_d909/index.htmlTable | http://dataset.osupytheas.fr/geonetwork/srv/fre/catalog.search#/metadata/9d2f74a1-a7af-4062-a4e9-bd63b904856a | http://erddap.osupytheas.fr/erddap/rss/STRASSE_89bd_108e_d909.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=STRASSE_89bd_108e_d909&showErrors=false&email= | MIO UMR7294 CNRS | STRASSE_89bd_108e_d909 | ||
https://erddap.osupytheas.fr/erddap/tabledap/UPCAST_b0e2_399c_6fd2.subset | https://erddap.osupytheas.fr/erddap/tabledap/UPCAST_b0e2_399c_6fd2 | https://erddap.osupytheas.fr/erddap/tabledap/UPCAST_b0e2_399c_6fd2.graph | https://erddap.osupytheas.fr/erddap/files/UPCAST_b0e2_399c_6fd2/ | public | OCARINA UPCAST 2017 experiment, prototype 1, level 2 surface and air-sea turbulent fluxes | Turbulent air-sea fluxes and associated variables from the OCARINA wave-following and drifting platform (Bourras et al. 2014, DOI: 10.1175/JTECH-D-13-00055.)\n\ncdm_data_type = TimeSeries\nVARIABLES:\ntime2 (Time)\ntime (seconds since 1970-01-01T00:00:00Z)\nlongitude (degrees_east)\nlatitude (degrees_north)\npair (Air pressure, hPa)\ntair (Air Temperature, degree_C)\nhur (Relative air humidity, 1)\nsst (degree_C)\nrho (Density of air, kg m-3)\nrlds (downwelling longwave radiation flux, positive downward, W m-2)\nrlus (upwelling longwave radiation flux, positive upward, W m-2)\nrsds (downwelling shortwave radiation flux, positive downward, W m-2)\nrsus (upwelling shortwave radiation flux, positive upward, W m-2)\nwdir (Direction of the wind vector with respect to ground, measured positive clockwise from due north, degrees)\nwspd (Magnitude of wind velocity with respect to ground, m s-1)\nu10n (Equivalent neutral wind extrapolated at a 10-m height, from eddy-covariance calculation, m s-1)\nhsw (Significant wave height, calculated as four times the square root of the integration of the vertical platform velocity, m)\nhsw_day (daily estimate of the significant wave height, calculated as four times the square root of the integration of the vertical platform velocity, m)\nTsw (Inverse of the frequency at the maximum of the power spectrum of the vertical platform velocity (experimental), s)\nTsw_day (Daily estimate of the inverse of the frequency at the maximum of the power spectrum of the vertical platform velocity (experimental), s)\ntauu (Eastward component of the surface wind stress vector, from eddy-covariance calculation, Pa)\ntauv (Northward component of the surface wind stress vector, from eddy-covariance calculation, Pa)\nustar (Turbulent surface friction velocity, from eddy-covariance calculation, m s-1)\nhsv (Turbulent surface buoyancy flux, from eddy-covariance calculation, W m-2)\nzL (Monin-Obukhov ratio, which quantifies surface boundary layer stability, from eddy-covariance calculation, 1)\nustar_bulk (Turbulent surface friction velocity, COARE 3.0 (please see header) drag parameterization adjusted to OCARINA data, m s-1)\n... (12 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/UPCAST_b0e2_399c_6fd2_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/UPCAST_b0e2_399c_6fd2_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/UPCAST_b0e2_399c_6fd2/index.htmlTable | http://dataset.osupytheas.fr/geonetwork/srv/fre/catalog.search#/metadata/9d2f74a1-a7af-4062-a4e9-bd63b904856a | http://erddap.osupytheas.fr/erddap/rss/UPCAST_b0e2_399c_6fd2.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=UPCAST_b0e2_399c_6fd2&showErrors=false&email= | MIO UMR7294 CNRS | UPCAST_b0e2_399c_6fd2 |