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Erddap est un produit développé par : NOAA ERD |
| griddap | Subset | tabledap | Make A Graph | wms | files | Accessible | Title | Summary | FGDC | ISO 19115 | Info | Background Info | RSS | Institution | Dataset ID | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 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 from 2021-07) | 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_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 from 2021-07) | 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_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_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 | ||
| https://erddap.osupytheas.fr/erddap/griddap/DINEOF_59f6_b797_92a2 | https://erddap.osupytheas.fr/erddap/griddap/DINEOF_59f6_b797_92a2.graph | https://erddap.osupytheas.fr/erddap/wms/DINEOF_59f6_b797_92a2/request | https://erddap.osupytheas.fr/erddap/files/DINEOF_59f6_b797_92a2/ | public | HF radar daily averaged sea surface current filterd by dineof | Daily High Frequency Radar (HFR) surface current data (radial velocity files and total velocity file) from 2 different stations located on the French Mediterranean coast (Toulon), spanning from January 2012 to December 2019. The radial datasets have been processed to remove outliers. Then the gaps in the data have been filled using the DINEOF algorithm. The total velocity is then reconstructed from the filled radial velocity files, and projected onto a cartesian grid of 1kmx1km.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\nEWCT (West-east current component, m s-1)\nNSCT (South-north current component, m s-1)\nQCflag (Overall Quality Flags, 1)\nGDOP (Geometrical Dilution Of Precision, 1)\nPOSITION_QC (Position Quality Flag, 1)\nGDOP_QC (GDOP Threshold Quality Flags, 1)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/DINEOF_59f6_b797_92a2_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/DINEOF_59f6_b797_92a2_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/DINEOF_59f6_b797_92a2/index.htmlTable | http://hfradar.univ-tln.fr/HFRADAR/squel.php?content=accueil
| http://erddap.osupytheas.fr/erddap/rss/DINEOF_59f6_b797_92a2.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=DINEOF_59f6_b797_92a2&showErrors=false&email= | Mediterranean Institute of Oceanography | DINEOF_59f6_b797_92a2 | ||
| https://erddap.osupytheas.fr/erddap/griddap/cmems_nc_cf0e_c84a_8ead | https://erddap.osupytheas.fr/erddap/griddap/cmems_nc_cf0e_c84a_8ead.graph | https://erddap.osupytheas.fr/erddap/wms/cmems_nc_cf0e_c84a_8ead/request | https://erddap.osupytheas.fr/erddap/files/cmems_nc_cf0e_c84a_8ead/ | public | HF radar data hourly processed in real-time of the Surface Ocean Velocity in MedSea | Sea surface currents recorded by High Frequency (HF) radar in the north-western Mediterranean Sea. The network has been in situ on the French Riviera since 2012 and is operated by MIO - the Mediterranean Institute of Oceanography (UMR Aix Marseille Universite, CNRS, IRD, Universite de Toulon).\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\nEWCT (West-east current component, m s-1)\nNSCT (South-north current component, m s-1)\nEWCS (Standard Deviation of Surface Eastward Sea Water Velocity, m s-1)\nNSCS (Standard Deviation of Surface Northward Sea Water Velocity, m s-1)\nGDOP (Geometrical Dilution Of Precision, 1)\nPOSITION_QC (1)\nQCflag (1)\nVART_QC (1)\nGDOP_QC (1)\nDDNS_QC (1)\nCSPD_QC (1)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/cmems_nc_cf0e_c84a_8ead_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/cmems_nc_cf0e_c84a_8ead_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/cmems_nc_cf0e_c84a_8ead/index.htmlTable | https://erddap.osupytheas.fr | http://erddap.osupytheas.fr/erddap/rss/cmems_nc_cf0e_c84a_8ead.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=cmems_nc_cf0e_c84a_8ead&showErrors=false&email= | MIO UMR7294 CNRS / OSU Pytheas | cmems_nc_cf0e_c84a_8ead | ||
| 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/griddap/laser-med_climato | https://erddap.osupytheas.fr/erddap/griddap/laser-med_climato.graph | https://erddap.osupytheas.fr/erddap/wms/laser-med_climato/request | https://erddap.osupytheas.fr/erddap/files/laser-med_climato/ | public | LaSer-MED Regional Climate Projection (1985-2100) | Climate Projection (1985-2100) of the mediterranean biogeochemistry provided by the CNRM-RCSM4/Eco3M-MED model under a regional RCP8.5 scenario (LaSeR-Med project)\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\nAMON (Ammonium (NH4-N) content, umol/l)\nNTRA (Nitrate (NO3-N) content, umol/l)\nPHOS (Phosphate (PO4-P) content, umol/l)\nCHLT (Chlorophyll total, mg/m3)\nPAR (Photosynthetically Available Radiation, W/m^2)\nHBAC (Mole concentration of heterotrophic bacteria expressed as carbon in sea water, mol/m^3)\nHBAN (Mole concentration of heterotrophic bacteria expressed as nitrogen in sea water, mol/m^3)\nHBAP (Mole concentration of heterotrophic bacteria expressed as phosphorus in sea water, mol/m^3)\nHBAW (Nb Of Heterotrophic Bacteria, nb/ml)\nCIMC (Mole concentration of microzooplankton expressed as carbon in sea water, mol/m^3)\nCICW (Number of seawater ciliates, nb/l)\nCIMN (Mole concentration of microzooplankton expressed as nitrogen in sea water, mol/m^3)\nCIMP (Mole concentration of microzooplankton expressed as phophorus in sea water, mol/m^3)\nTotMeszMassC (Biomass as carbon of mesozooplankton, mg/m^3)\nCOPP (Number of copepods, nb/m^3)\nNFHC (Mole concentration of heterotrophic nanoflagellates expressed as carbon in sea water, mol/m^3)\nNFHW (Number of heterotrophic nanoflagellates, nb/l)\nNFHN (Mole concentration of heterotrophic nanoflagellates expressed as nitrogen in sea water, mol/m^3)\nNFHP (Mole concentration of heterotrophic nanoflagellatesexpressed as phosphorus in sea water, mol/m^3)\nLPHC (Mole concentration of large phytoplankton expressed as carbon in sea water, mol/m^3)\nLPHCW (Large phytoplankton abundance, nb/l)\nLPHCHL (Mole concentration of large phytoplankton expressed as chlorophyl in sea water, mol/m^3)\nLPHN (Mole concentration of large phytoplankton expressed as nitrogen in sea water, mol/m^3)\nLPHP (Mole concentration of large phytoplankton expressed as phosphorus in sea water, mol/m^3)\nSPHC (Mole concentration of small phytoplankton expressed as carbon in sea water, mol/m^3)\nSPHCW (Small phytoplankton abundance, nb/ml)\n... (7 more variables)\n | https://erddap.osupytheas.fr/erddap/metadata/fgdc/xml/laser-med_climato_fgdc.xml | https://erddap.osupytheas.fr/erddap/metadata/iso19115/xml/laser-med_climato_iso19115.xml | https://erddap.osupytheas.fr/erddap/info/laser-med_climato/index.htmlTable | ??? | http://erddap.osupytheas.fr/erddap/rss/laser-med_climato.rss | https://erddap.osupytheas.fr/erddap/subscriptions/add.html?datasetID=laser-med_climato&showErrors=false&email= | MIO UMR7294 CNRS, Marseille | laser-med_climato | ||
| 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_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 |