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/erddap/griddap/V2023_chemistry_a442_9ee7_21e4 /erddap/griddap/V2023_chemistry_a442_9ee7_21e4.graph /erddap/wms/V2023_chemistry_a442_9ee7_21e4/request Mediterranean Sea, Po River, DIVAnd 4D seasonal analysis of Water body chlorophyll-a 1960/2020 v2023 [time][depth][lat][lon], 0.009°, 1990 Mediterranean Sea - Po River - DIVAnd 4D seasonal analysis of Water body chlorophyll-a 1960/2020 v2023. Water body chlorophyll-a - Seasonal Climatology for Po River for the period 1960-2020 on the domain: Lon E12.0-14.0deg., Lat N44.0-46.0deg.\nData Sources: observational data from SeaDataNet/EMODNet Chemistry Data Network.\nDescription of DIVA analysis: The computation was done with the DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.9, using GEBCO 30sec topography for the spatial connectivity of water masses.\nThe horizontal resolution of the produced DIVAnd maps grids is dx=dy=0.009 degrees (around 975m and 708m accordingly).\nThe vertical resolution is 14 depth levels: [0., 2., 4., 6., 8., 10., 15., 20., 25., 30., 40., 50., 60., 70.].\nA relative correlation length used based on topography gradients and the horizontal correlation length varies from 25 km to 12.5 km. The vertical correlation length (in meters) is:  [4.,4.,4.,4.,4.,10.,10.,10.,10.,20.,20.,20.,20.,20.]. \nDuplicates check was performed using the following criteria for space and time: dlon=0.01deg., dlat=0.01deg., ddepth=0.01m, dtime=1min, dvalue=0.01.\nThe error variance (epsilon2) was set equal to 1. Data weight was reduced at shallow waters. Data weighting was applied with the following threshold values: lon=0.03, lat=0.03, depth=2.\nAn anamorphosis transformation was applied to the data (function DIVAnd.Anam.loglin) to avoid unrealistic negative values: threshold value=200.\nThe mean value was used as background analysis field.\nQuality control of the observations was applied using the interpolated field (QCMETHOD=3). Residuals (differences between the observations and the analysis (interpolated linearly to the location of the observations) were calculated. Observations with residuals outside the minimum and maximum values of the 99% quantile were discarded from the analysis. \nSeasons definition: Winter=Jan-Mar, Spring=Apr-Jun, Summer=Jul-Sep, Autumn=Oct-Dec.\nOriginators of Italian data sets-List of contributors:\n- Brunetti Fabio (OGS)\n- Cardin Vanessa, Bensi Manuel doi:10.6092/36728450-4296-4e6a-967d-d5b6da55f306\n- Cardin Vanessa, Bensi Manuel, Ursella Laura, Siena Giuseppe doi:10.6092/f8e6d18e-f877-4aa5-a983-a03b06ccb987\n- Cataletto Bruno (OGS)\n- Cinzia Comici Cinzia (OGS)\n- Civitarese Giuseppe (OGS)\n- DeVittor Cinzia (OGS)\n- Giani Michele (OGS)\n- Kovacevic Vedrana (OGS)\n- Mosetti Renzo (OGS)\n- Solidoro C.,Beran A.,Cataletto B.,Celussi M.,Cibic T.,Comici C.,Del Negro P.,De Vittor C.,Minocci M.,Monti M.,Fabbro C.,Falconi C.,Franzo A.,Libralato S.,Lipizer M.,Negussanti J.S.,Russel H.,Valli G., doi:10.6092/e5518899-b914-43b0-8139-023718aa63f5\n- Celio Massimo (ARPA FVG)\n- Malaguti Antonella (ENEA)\n- Fonda Umani Serena (UNITS)\n- Bignami Francesco (ISAC/National Research Council (CNR))\n- Boldrini Alfredo (ISMAR/CNR)\n- Marini Mauro (ISMAR/CNR)\n- Miserocchi Stefano (ISMAR/CNR)\n- Zaccone Renata (IAMC/CNR)\n- Lavezza, R., Dubroca, L. F. C., Ludicone, D., Kress, N., Herut, B., Civitarese, G., Cruzado, A., Lefevre, D.,Souvermezoglou, E., Yilmaz, A., Tugrul, S., and Ribera d'Alcala, M.: Compilation of quality controlled nutrient profiles from the Mediterranean Sea, doi:10.1594/PANGAEA.771907, 2011.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\nWater_body_chlorophyll_a_L1 (Water body chlorophyll-a masked using relative error threshold 0.3, mg/m3)\nWater_body_chlorophyll_a_L2 (Water body chlorophyll-a masked using relative error threshold 0.5, mg/m3)\nWater_body_chlorophyll_a_relerr (Relative error of Water body chlorophyll-a, 1)\n /erddap/metadata/fgdc/xml/V2023_chemistry_a442_9ee7_21e4_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_a442_9ee7_21e4_iso19115.xml /erddap/info/V2023_chemistry_a442_9ee7_21e4/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Mediterranean_Sea_-_Po_River/Water_body_chlorophyll-a.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_a442_9ee7_21e4.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_a442_9ee7_21e4&showErrors=false&email= Hellenic Centre for Marine Research, Hellenic National Oceanographic Data Centre V2023_chemistry_a442_9ee7_21e4
/erddap/griddap/V2023_chemistry_fbc1_7667_5d8f /erddap/griddap/V2023_chemistry_fbc1_7667_5d8f.graph /erddap/wms/V2023_chemistry_fbc1_7667_5d8f/request Mediterranean Sea, Po River, DIVAnd 4D seasonal analysis of Water body chlorophyll-a 1960/2020 v2023 [time][lat][lon], 0.009°, 1990 Mediterranean Sea - Po River - DIVAnd 4D seasonal analysis of Water body chlorophyll-a 1960/2020 v2023. Water body chlorophyll-a - Seasonal Climatology for Po River for the period 1960-2020 on the domain: Lon E12.0-14.0deg., Lat N44.0-46.0deg.\nData Sources: observational data from SeaDataNet/EMODNet Chemistry Data Network.\nDescription of DIVA analysis: The computation was done with the DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.9, using GEBCO 30sec topography for the spatial connectivity of water masses.\nThe horizontal resolution of the produced DIVAnd maps grids is dx=dy=0.009 degrees (around 975m and 708m accordingly).\nThe vertical resolution is 14 depth levels: [0., 2., 4., 6., 8., 10., 15., 20., 25., 30., 40., 50., 60., 70.].\nA relative correlation length used based on topography gradients and the horizontal correlation length varies from 25 km to 12.5 km. The vertical correlation length (in meters) is:  [4.,4.,4.,4.,4.,10.,10.,10.,10.,20.,20.,20.,20.,20.]. \nDuplicates check was performed using the following criteria for space and time: dlon=0.01deg., dlat=0.01deg., ddepth=0.01m, dtime=1min, dvalue=0.01.\nThe error variance (epsilon2) was set equal to 1. Data weight was reduced at shallow waters. Data weighting was applied with the following threshold values: lon=0.03, lat=0.03, depth=2.\nAn anamorphosis transformation was applied to the data (function DIVAnd.Anam.loglin) to avoid unrealistic negative values: threshold value=200.\nThe mean value was used as background analysis field.\nQuality control of the observations was applied using the interpolated field (QCMETHOD=3). Residuals (differences between the observations and the analysis (interpolated linearly to the location of the observations) were calculated. Observations with residuals outside the minimum and maximum values of the 99% quantile were discarded from the analysis. \nSeasons definition: Winter=Jan-Mar, Spring=Apr-Jun, Summer=Jul-Sep, Autumn=Oct-Dec.\nOriginators of Italian data sets-List of contributors:\n- Brunetti Fabio (OGS)\n- Cardin Vanessa, Bensi Manuel doi:10.6092/36728450-4296-4e6a-967d-d5b6da55f306\n- Cardin Vanessa, Bensi Manuel, Ursella Laura, Siena Giuseppe doi:10.6092/f8e6d18e-f877-4aa5-a983-a03b06ccb987\n- Cataletto Bruno (OGS)\n- Cinzia Comici Cinzia (OGS)\n- Civitarese Giuseppe (OGS)\n- DeVittor Cinzia (OGS)\n- Giani Michele (OGS)\n- Kovacevic Vedrana (OGS)\n- Mosetti Renzo (OGS)\n- Solidoro C.,Beran A.,Cataletto B.,Celussi M.,Cibic T.,Comici C.,Del Negro P.,De Vittor C.,Minocci M.,Monti M.,Fabbro C.,Falconi C.,Franzo A.,Libralato S.,Lipizer M.,Negussanti J.S.,Russel H.,Valli G., doi:10.6092/e5518899-b914-43b0-8139-023718aa63f5\n- Celio Massimo (ARPA FVG)\n- Malaguti Antonella (ENEA)\n- Fonda Umani Serena (UNITS)\n- Bignami Francesco (ISAC/National Research Council (CNR))\n- Boldrini Alfredo (ISMAR/CNR)\n- Marini Mauro (ISMAR/CNR)\n- Miserocchi Stefano (ISMAR/CNR)\n- Zaccone Renata (IAMC/CNR)\n- Lavezza, R., Dubroca, L. F. C., Ludicone, D., Kress, N., Herut, B., Civitarese, G., Cruzado, A., Lefevre, D.,Souvermezoglou, E., Yilmaz, A., Tugrul, S., and Ribera d'Alcala, M.: Compilation of quality controlled nutrient profiles from the Mediterranean Sea, doi:10.1594/PANGAEA.771907, 2011.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][latitude][longitude]):\nWater_body_chlorophyll_a_deepest (Deepest values of Water body chlorophyll-a, mg/m3)\n /erddap/metadata/fgdc/xml/V2023_chemistry_fbc1_7667_5d8f_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_fbc1_7667_5d8f_iso19115.xml /erddap/info/V2023_chemistry_fbc1_7667_5d8f/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Mediterranean_Sea_-_Po_River/Water_body_chlorophyll-a.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_fbc1_7667_5d8f.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_fbc1_7667_5d8f&showErrors=false&email= Hellenic Centre for Marine Research, Hellenic National Oceanographic Data Centre V2023_chemistry_fbc1_7667_5d8f
/erddap/griddap/V2023_chemistry_997b_834f_60e1 /erddap/griddap/V2023_chemistry_997b_834f_60e1.graph /erddap/wms/V2023_chemistry_997b_834f_60e1/request Mediterranean Sea, Po River, DIVAnd 4D seasonal analysis of Water body dissolved inorganic nitrogen (DIN) 1980/2020 v2023 [time][depth][lat][lon], 0.009°, 2000 Mediterranean Sea - Po River - DIVAnd 4D seasonal analysis of Water body dissolved inorganic nitrogen (DIN) 1980/2020 v2023. Water body chlorophyll-a - Seasonal Climatology for Po River for the period 1960-2020 on the domain: Lon E12.0-14.0deg., Lat N44.0-46.0deg.\nData Sources: observational data from SeaDataNet/EMODNet Chemistry Data Network.\nDescription of DIVA analysis: The computation was done with the DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.9, using GEBCO 30sec topography for the spatial connectivity of water masses.\nThe horizontal resolution of the produced DIVAnd maps grids is dx=dy=0.009 degrees (around 975m and 708m accordingly).\nThe vertical resolution is 14 depth levels: [0., 2., 4., 6., 8., 10., 15., 20., 25., 30., 40., 50., 60., 70.].\nA relative correlation length used based on topography gradients and the horizontal correlation length varies from 25 km to 12.5 km. The vertical correlation length (in meters) is:  [4.,4.,4.,4.,4.,10.,10.,10.,10.,20.,20.,20.,20.,20.]. \nDuplicates check was performed using the following criteria for space and time: dlon=0.01deg., dlat=0.01deg., ddepth=0.01m, dtime=1min, dvalue=0.01.\nThe error variance (epsilon2) was set equal to 1. Data weight was reduced at shallow waters. Data weighting was applied with the following threshold values: lon=0.03, lat=0.03, depth=2.\nAn anamorphosis transformation was applied to the data (function DIVAnd.Anam.loglin) to avoid unrealistic negative values: threshold value=200.\nThe mean value was used as background analysis field.\nQuality control of the observations was applied using the interpolated field (QCMETHOD=3). Residuals (differences between the observations and the analysis (interpolated linearly to the location of the observations) were calculated. Observations with residuals outside the minimum and maximum values of the 99% quantile were discarded from the analysis. \nSeasons definition: Winter=Jan-Mar, Spring=Apr-Jun, Summer=Jul-Sep, Autumn=Oct-Dec.\nOriginators of Italian data sets-List of contributors:\n- Brunetti Fabio (OGS)\n- Cardin Vanessa, Bensi Manuel doi:10.6092/36728450-4296-4e6a-967d-d5b6da55f306\n- Cardin Vanessa, Bensi Manuel, Ursella Laura, Siena Giuseppe doi:10.6092/f8e6d18e-f877-4aa5-a983-a03b06ccb987\n- Cataletto Bruno (OGS)\n- Cinzia Comici Cinzia (OGS)\n- Civitarese Giuseppe (OGS)\n- DeVittor Cinzia (OGS)\n- Giani Michele (OGS)\n- Kovacevic Vedrana (OGS)\n- Mosetti Renzo (OGS)\n- Solidoro C.,Beran A.,Cataletto B.,Celussi M.,Cibic T.,Comici C.,Del Negro P.,De Vittor C.,Minocci M.,Monti M.,Fabbro C.,Falconi C.,Franzo A.,Libralato S.,Lipizer M.,Negussanti J.S.,Russel H.,Valli G., doi:10.6092/e5518899-b914-43b0-8139-023718aa63f5\n- Celio Massimo (ARPA FVG)\n- Malaguti Antonella (ENEA)\n- Fonda Umani Serena (UNITS)\n- Bignami Francesco (ISAC/National Research Council (CNR))\n- Boldrini Alfredo (ISMAR/CNR)\n- Marini Mauro (ISMAR/CNR)\n- Miserocchi Stefano (ISMAR/CNR)\n- Zaccone Renata (IAMC/CNR)\n- Lavezza, R., Dubroca, L. F. C., Ludicone, D., Kress, N., Herut, B., Civitarese, G., Cruzado, A., Lefevre, D.,Souvermezoglou, E., Yilmaz, A., Tugrul, S., and Ribera d'Alcala, M.: Compilation of quality controlled nutrient profiles from the Mediterranean Sea, doi:10.1594/PANGAEA.771907, 2011.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\nWater_body_dissolved_inorganic_nitrogen_L1 (Water body dissolved inorganic nitrogen (DIN) masked using relative error threshold 0.3, umol/l)\nWater_body_dissolved_inorganic_nitrogen_L2 (Water body dissolved inorganic nitrogen (DIN) masked using relative error threshold 0.5, umol/l)\nWater_body_dissolved_inorganic_nitrogen_relerr (Relative error of Water body dissolved inorganic nitrogen (DIN), 1)\n /erddap/metadata/fgdc/xml/V2023_chemistry_997b_834f_60e1_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_997b_834f_60e1_iso19115.xml /erddap/info/V2023_chemistry_997b_834f_60e1/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Mediterranean_Sea_-_Po_River/Water_body_dissolved_inorganic_nitrogen.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_997b_834f_60e1.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_997b_834f_60e1&showErrors=false&email= Hellenic Centre for Marine Research, Hellenic National Oceanographic Data Centre V2023_chemistry_997b_834f_60e1
/erddap/griddap/V2023_chemistry_2a9c_5046_f2cb /erddap/griddap/V2023_chemistry_2a9c_5046_f2cb.graph Mediterranean Sea, Po River, DIVAnd 4D seasonal analysis of Water body dissolved inorganic nitrogen (DIN) 1980/2020 v2023 [time][lat][lon], 0.009°, 2000 Mediterranean Sea - Po River - DIVAnd 4D seasonal analysis of Water body dissolved inorganic nitrogen (DIN) 1980/2020 v2023. Water body chlorophyll-a - Seasonal Climatology for Po River for the period 1960-2020 on the domain: Lon E12.0-14.0deg., Lat N44.0-46.0deg.\nData Sources: observational data from SeaDataNet/EMODNet Chemistry Data Network.\nDescription of DIVA analysis: The computation was done with the DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.9, using GEBCO 30sec topography for the spatial connectivity of water masses.\nThe horizontal resolution of the produced DIVAnd maps grids is dx=dy=0.009 degrees (around 975m and 708m accordingly).\nThe vertical resolution is 14 depth levels: [0., 2., 4., 6., 8., 10., 15., 20., 25., 30., 40., 50., 60., 70.].\nA relative correlation length used based on topography gradients and the horizontal correlation length varies from 25 km to 12.5 km. The vertical correlation length (in meters) is:  [4.,4.,4.,4.,4.,10.,10.,10.,10.,20.,20.,20.,20.,20.]. \nDuplicates check was performed using the following criteria for space and time: dlon=0.01deg., dlat=0.01deg., ddepth=0.01m, dtime=1min, dvalue=0.01.\nThe error variance (epsilon2) was set equal to 1. Data weight was reduced at shallow waters. Data weighting was applied with the following threshold values: lon=0.03, lat=0.03, depth=2.\nAn anamorphosis transformation was applied to the data (function DIVAnd.Anam.loglin) to avoid unrealistic negative values: threshold value=200.\nThe mean value was used as background analysis field.\nQuality control of the observations was applied using the interpolated field (QCMETHOD=3). Residuals (differences between the observations and the analysis (interpolated linearly to the location of the observations) were calculated. Observations with residuals outside the minimum and maximum values of the 99% quantile were discarded from the analysis. \nSeasons definition: Winter=Jan-Mar, Spring=Apr-Jun, Summer=Jul-Sep, Autumn=Oct-Dec.\nOriginators of Italian data sets-List of contributors:\n- Brunetti Fabio (OGS)\n- Cardin Vanessa, Bensi Manuel doi:10.6092/36728450-4296-4e6a-967d-d5b6da55f306\n- Cardin Vanessa, Bensi Manuel, Ursella Laura, Siena Giuseppe doi:10.6092/f8e6d18e-f877-4aa5-a983-a03b06ccb987\n- Cataletto Bruno (OGS)\n- Cinzia Comici Cinzia (OGS)\n- Civitarese Giuseppe (OGS)\n- DeVittor Cinzia (OGS)\n- Giani Michele (OGS)\n- Kovacevic Vedrana (OGS)\n- Mosetti Renzo (OGS)\n- Solidoro C.,Beran A.,Cataletto B.,Celussi M.,Cibic T.,Comici C.,Del Negro P.,De Vittor C.,Minocci M.,Monti M.,Fabbro C.,Falconi C.,Franzo A.,Libralato S.,Lipizer M.,Negussanti J.S.,Russel H.,Valli G., doi:10.6092/e5518899-b914-43b0-8139-023718aa63f5\n- Celio Massimo (ARPA FVG)\n- Malaguti Antonella (ENEA)\n- Fonda Umani Serena (UNITS)\n- Bignami Francesco (ISAC/National Research Council (CNR))\n- Boldrini Alfredo (ISMAR/CNR)\n- Marini Mauro (ISMAR/CNR)\n- Miserocchi Stefano (ISMAR/CNR)\n- Zaccone Renata (IAMC/CNR)\n- Lavezza, R., Dubroca, L. F. C., Ludicone, D., Kress, N., Herut, B., Civitarese, G., Cruzado, A., Lefevre, D.,Souvermezoglou, E., Yilmaz, A., Tugrul, S., and Ribera d'Alcala, M.: Compilation of quality controlled nutrient profiles from the Mediterranean Sea, doi:10.1594/PANGAEA.771907, 2011.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][latitude][longitude]):\nWater_body_dissolved_inorganic_nitrogen_deepest (Deepest values of Water body dissolved inorganic nitrogen (DIN), umol/l)\n /erddap/metadata/fgdc/xml/V2023_chemistry_2a9c_5046_f2cb_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_2a9c_5046_f2cb_iso19115.xml /erddap/info/V2023_chemistry_2a9c_5046_f2cb/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Mediterranean_Sea_-_Po_River/Water_body_dissolved_inorganic_nitrogen.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_2a9c_5046_f2cb.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_2a9c_5046_f2cb&showErrors=false&email= Hellenic Centre for Marine Research, Hellenic National Oceanographic Data Centre V2023_chemistry_2a9c_5046_f2cb
/erddap/griddap/V2023_chemistry_5e98_b55b_17a1 /erddap/griddap/V2023_chemistry_5e98_b55b_17a1.graph /erddap/wms/V2023_chemistry_5e98_b55b_17a1/request Mediterranean Sea, Po River, DIVAnd 4D seasonal analysis of Water body dissolved oxygen concentration 1960/2020 v2023 [time][depth][lat][lon], 0.009°, 1990 Mediterranean Sea - Po River - DIVAnd 4D seasonal analysis of Water body dissolved oxygen concentration 1960/2020 v2023. Water body chlorophyll-a - Seasonal Climatology for Po River for the period 1960-2020 on the domain: Lon E12.0-14.0deg., Lat N44.0-46.0deg.\nData Sources: observational data from SeaDataNet/EMODNet Chemistry Data Network.\nDescription of DIVA analysis: The computation was done with the DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.9, using GEBCO 30sec topography for the spatial connectivity of water masses.\nThe horizontal resolution of the produced DIVAnd maps grids is dx=dy=0.009 degrees (around 975m and 708m accordingly).\nThe vertical resolution is 14 depth levels: [0., 2., 4., 6., 8., 10., 15., 20., 25., 30., 40., 50., 60., 70.].\nA relative correlation length used based on topography gradients and the horizontal correlation length varies from 25 km to 12.5 km. The vertical correlation length (in meters) is:  [4.,4.,4.,4.,4.,10.,10.,10.,10.,20.,20.,20.,20.,20.]. \nDuplicates check was performed using the following criteria for space and time: dlon=0.01deg., dlat=0.01deg., ddepth=0.01m, dtime=1min, dvalue=0.01.\nThe error variance (epsilon2) was set equal to 1. Data weight was reduced at shallow waters. Data weighting was applied with the following threshold values: lon=0.03, lat=0.03, depth=2.\nAn anamorphosis transformation was applied to the data (function DIVAnd.Anam.loglin) to avoid unrealistic negative values: threshold value=200.\nThe mean value was used as background analysis field.\nQuality control of the observations was applied using the interpolated field (QCMETHOD=3). Residuals (differences between the observations and the analysis (interpolated linearly to the location of the observations) were calculated. Observations with residuals outside the minimum and maximum values of the 99% quantile were discarded from the analysis. \nSeasons definition: Winter=Jan-Mar, Spring=Apr-Jun, Summer=Jul-Sep, Autumn=Oct-Dec.\nOriginators of Italian data sets-List of contributors:\n- Brunetti Fabio (OGS)\n- Cardin Vanessa, Bensi Manuel doi:10.6092/36728450-4296-4e6a-967d-d5b6da55f306\n- Cardin Vanessa, Bensi Manuel, Ursella Laura, Siena Giuseppe doi:10.6092/f8e6d18e-f877-4aa5-a983-a03b06ccb987\n- Cataletto Bruno (OGS)\n- Cinzia Comici Cinzia (OGS)\n- Civitarese Giuseppe (OGS)\n- DeVittor Cinzia (OGS)\n- Giani Michele (OGS)\n- Kovacevic Vedrana (OGS)\n- Mosetti Renzo (OGS)\n- Solidoro C.,Beran A.,Cataletto B.,Celussi M.,Cibic T.,Comici C.,Del Negro P.,De Vittor C.,Minocci M.,Monti M.,Fabbro C.,Falconi C.,Franzo A.,Libralato S.,Lipizer M.,Negussanti J.S.,Russel H.,Valli G., doi:10.6092/e5518899-b914-43b0-8139-023718aa63f5\n- Celio Massimo (ARPA FVG)\n- Malaguti Antonella (ENEA)\n- Fonda Umani Serena (UNITS)\n- Bignami Francesco (ISAC/National Research Council (CNR))\n- Boldrini Alfredo (ISMAR/CNR)\n- Marini Mauro (ISMAR/CNR)\n- Miserocchi Stefano (ISMAR/CNR)\n- Zaccone Renata (IAMC/CNR)\n- Lavezza, R., Dubroca, L. F. C., Ludicone, D., Kress, N., Herut, B., Civitarese, G., Cruzado, A., Lefevre, D.,Souvermezoglou, E., Yilmaz, A., Tugrul, S., and Ribera d'Alcala, M.: Compilation of quality controlled nutrient profiles from the Mediterranean Sea, doi:10.1594/PANGAEA.771907, 2011.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\nWater_body_dissolved_oxygen_concentration_L1 (Water body dissolved oxygen concentration masked using relative error threshold 0.3, umol/l)\nWater_body_dissolved_oxygen_concentration_L2 (Water body dissolved oxygen concentration masked using relative error threshold 0.5, umol/l)\nWater_body_dissolved_oxygen_concentration_relerr (Relative error of Water body dissolved oxygen concentration, 1)\n /erddap/metadata/fgdc/xml/V2023_chemistry_5e98_b55b_17a1_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_5e98_b55b_17a1_iso19115.xml /erddap/info/V2023_chemistry_5e98_b55b_17a1/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Mediterranean_Sea_-_Po_River/Water_body_dissolved_oxygen_concentration.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_5e98_b55b_17a1.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_5e98_b55b_17a1&showErrors=false&email= Hellenic Centre for Marine Research, Hellenic National Oceanographic Data Centre V2023_chemistry_5e98_b55b_17a1
/erddap/griddap/V2023_chemistry_a23a_6507_7724 /erddap/griddap/V2023_chemistry_a23a_6507_7724.graph /erddap/wms/V2023_chemistry_a23a_6507_7724/request Mediterranean Sea, Po River, DIVAnd 4D seasonal analysis of Water body dissolved oxygen concentration 1960/2020 v2023 [time][lat][lon], 0.009°, 1990 Mediterranean Sea - Po River - DIVAnd 4D seasonal analysis of Water body dissolved oxygen concentration 1960/2020 v2023. Water body chlorophyll-a - Seasonal Climatology for Po River for the period 1960-2020 on the domain: Lon E12.0-14.0deg., Lat N44.0-46.0deg.\nData Sources: observational data from SeaDataNet/EMODNet Chemistry Data Network.\nDescription of DIVA analysis: The computation was done with the DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.9, using GEBCO 30sec topography for the spatial connectivity of water masses.\nThe horizontal resolution of the produced DIVAnd maps grids is dx=dy=0.009 degrees (around 975m and 708m accordingly).\nThe vertical resolution is 14 depth levels: [0., 2., 4., 6., 8., 10., 15., 20., 25., 30., 40., 50., 60., 70.].\nA relative correlation length used based on topography gradients and the horizontal correlation length varies from 25 km to 12.5 km. The vertical correlation length (in meters) is:  [4.,4.,4.,4.,4.,10.,10.,10.,10.,20.,20.,20.,20.,20.]. \nDuplicates check was performed using the following criteria for space and time: dlon=0.01deg., dlat=0.01deg., ddepth=0.01m, dtime=1min, dvalue=0.01.\nThe error variance (epsilon2) was set equal to 1. Data weight was reduced at shallow waters. Data weighting was applied with the following threshold values: lon=0.03, lat=0.03, depth=2.\nAn anamorphosis transformation was applied to the data (function DIVAnd.Anam.loglin) to avoid unrealistic negative values: threshold value=200.\nThe mean value was used as background analysis field.\nQuality control of the observations was applied using the interpolated field (QCMETHOD=3). Residuals (differences between the observations and the analysis (interpolated linearly to the location of the observations) were calculated. Observations with residuals outside the minimum and maximum values of the 99% quantile were discarded from the analysis. \nSeasons definition: Winter=Jan-Mar, Spring=Apr-Jun, Summer=Jul-Sep, Autumn=Oct-Dec.\nOriginators of Italian data sets-List of contributors:\n- Brunetti Fabio (OGS)\n- Cardin Vanessa, Bensi Manuel doi:10.6092/36728450-4296-4e6a-967d-d5b6da55f306\n- Cardin Vanessa, Bensi Manuel, Ursella Laura, Siena Giuseppe doi:10.6092/f8e6d18e-f877-4aa5-a983-a03b06ccb987\n- Cataletto Bruno (OGS)\n- Cinzia Comici Cinzia (OGS)\n- Civitarese Giuseppe (OGS)\n- DeVittor Cinzia (OGS)\n- Giani Michele (OGS)\n- Kovacevic Vedrana (OGS)\n- Mosetti Renzo (OGS)\n- Solidoro C.,Beran A.,Cataletto B.,Celussi M.,Cibic T.,Comici C.,Del Negro P.,De Vittor C.,Minocci M.,Monti M.,Fabbro C.,Falconi C.,Franzo A.,Libralato S.,Lipizer M.,Negussanti J.S.,Russel H.,Valli G., doi:10.6092/e5518899-b914-43b0-8139-023718aa63f5\n- Celio Massimo (ARPA FVG)\n- Malaguti Antonella (ENEA)\n- Fonda Umani Serena (UNITS)\n- Bignami Francesco (ISAC/National Research Council (CNR))\n- Boldrini Alfredo (ISMAR/CNR)\n- Marini Mauro (ISMAR/CNR)\n- Miserocchi Stefano (ISMAR/CNR)\n- Zaccone Renata (IAMC/CNR)\n- Lavezza, R., Dubroca, L. F. C., Ludicone, D., Kress, N., Herut, B., Civitarese, G., Cruzado, A., Lefevre, D.,Souvermezoglou, E., Yilmaz, A., Tugrul, S., and Ribera d'Alcala, M.: Compilation of quality controlled nutrient profiles from the Mediterranean Sea, doi:10.1594/PANGAEA.771907, 2011.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][latitude][longitude]):\nWater_body_dissolved_oxygen_concentration_deepest (Deepest values of Water body dissolved oxygen concentration, umol/l)\n /erddap/metadata/fgdc/xml/V2023_chemistry_a23a_6507_7724_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_a23a_6507_7724_iso19115.xml /erddap/info/V2023_chemistry_a23a_6507_7724/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Mediterranean_Sea_-_Po_River/Water_body_dissolved_oxygen_concentration.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_a23a_6507_7724.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_a23a_6507_7724&showErrors=false&email= Hellenic Centre for Marine Research, Hellenic National Oceanographic Data Centre V2023_chemistry_a23a_6507_7724
/erddap/griddap/V2023_chemistry_9e0f_baa0_fe7d /erddap/griddap/V2023_chemistry_9e0f_baa0_fe7d.graph /erddap/wms/V2023_chemistry_9e0f_baa0_fe7d/request Mediterranean Sea, Po River, DIVAnd 4D seasonal analysis of Water body phosphate 1960/2020 v2023 [time][depth][lat][lon], 0.009°, 1990 Mediterranean Sea - Po River - DIVAnd 4D seasonal analysis of Water body phosphate 1960/2020 v2023. Water body chlorophyll-a - Seasonal Climatology for Po River for the period 1960-2020 on the domain: Lon E12.0-14.0deg., Lat N44.0-46.0deg.\nData Sources: observational data from SeaDataNet/EMODNet Chemistry Data Network.\nDescription of DIVA analysis: The computation was done with the DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.9, using GEBCO 30sec topography for the spatial connectivity of water masses.\nThe horizontal resolution of the produced DIVAnd maps grids is dx=dy=0.009 degrees (around 975m and 708m accordingly).\nThe vertical resolution is 14 depth levels: [0., 2., 4., 6., 8., 10., 15., 20., 25., 30., 40., 50., 60., 70.].\nA relative correlation length used based on topography gradients and the horizontal correlation length varies from 25 km to 12.5 km. The vertical correlation length (in meters) is:  [4.,4.,4.,4.,4.,10.,10.,10.,10.,20.,20.,20.,20.,20.]. \nDuplicates check was performed using the following criteria for space and time: dlon=0.01deg., dlat=0.01deg., ddepth=0.01m, dtime=1min, dvalue=0.01.\nThe error variance (epsilon2) was set equal to 1. Data weight was reduced at shallow waters. Data weighting was applied with the following threshold values: lon=0.03, lat=0.03, depth=2.\nAn anamorphosis transformation was applied to the data (function DIVAnd.Anam.loglin) to avoid unrealistic negative values: threshold value=200.\nThe mean value was used as background analysis field.\nQuality control of the observations was applied using the interpolated field (QCMETHOD=3). Residuals (differences between the observations and the analysis (interpolated linearly to the location of the observations) were calculated. Observations with residuals outside the minimum and maximum values of the 99% quantile were discarded from the analysis. \nSeasons definition: Winter=Jan-Mar, Spring=Apr-Jun, Summer=Jul-Sep, Autumn=Oct-Dec.\nOriginators of Italian data sets-List of contributors:\n- Brunetti Fabio (OGS)\n- Cardin Vanessa, Bensi Manuel doi:10.6092/36728450-4296-4e6a-967d-d5b6da55f306\n- Cardin Vanessa, Bensi Manuel, Ursella Laura, Siena Giuseppe doi:10.6092/f8e6d18e-f877-4aa5-a983-a03b06ccb987\n- Cataletto Bruno (OGS)\n- Cinzia Comici Cinzia (OGS)\n- Civitarese Giuseppe (OGS)\n- DeVittor Cinzia (OGS)\n- Giani Michele (OGS)\n- Kovacevic Vedrana (OGS)\n- Mosetti Renzo (OGS)\n- Solidoro C.,Beran A.,Cataletto B.,Celussi M.,Cibic T.,Comici C.,Del Negro P.,De Vittor C.,Minocci M.,Monti M.,Fabbro C.,Falconi C.,Franzo A.,Libralato S.,Lipizer M.,Negussanti J.S.,Russel H.,Valli G., doi:10.6092/e5518899-b914-43b0-8139-023718aa63f5\n- Celio Massimo (ARPA FVG)\n- Malaguti Antonella (ENEA)\n- Fonda Umani Serena (UNITS)\n- Bignami Francesco (ISAC/National Research Council (CNR))\n- Boldrini Alfredo (ISMAR/CNR)\n- Marini Mauro (ISMAR/CNR)\n- Miserocchi Stefano (ISMAR/CNR)\n- Zaccone Renata (IAMC/CNR)\n- Lavezza, R., Dubroca, L. F. C., Ludicone, D., Kress, N., Herut, B., Civitarese, G., Cruzado, A., Lefevre, D.,Souvermezoglou, E., Yilmaz, A., Tugrul, S., and Ribera d'Alcala, M.: Compilation of quality controlled nutrient profiles from the Mediterranean Sea, doi:10.1594/PANGAEA.771907, 2011.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\nWater_body_phosphate_L1 (Water body phosphate masked using relative error threshold 0.3, umol/l)\nWater_body_phosphate_L2 (Water body phosphate masked using relative error threshold 0.5, umol/l)\nWater_body_phosphate_relerr (Relative error of Water body phosphate, 1)\n /erddap/metadata/fgdc/xml/V2023_chemistry_9e0f_baa0_fe7d_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_9e0f_baa0_fe7d_iso19115.xml /erddap/info/V2023_chemistry_9e0f_baa0_fe7d/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Mediterranean_Sea_-_Po_River/Water_body_phosphate.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_9e0f_baa0_fe7d.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_9e0f_baa0_fe7d&showErrors=false&email= Hellenic Centre for Marine Research, Hellenic National Oceanographic Data Centre V2023_chemistry_9e0f_baa0_fe7d
/erddap/griddap/V2023_chemistry_2053_0031_2533 /erddap/griddap/V2023_chemistry_2053_0031_2533.graph /erddap/wms/V2023_chemistry_2053_0031_2533/request Mediterranean Sea, Po River, DIVAnd 4D seasonal analysis of Water body phosphate 1960/2020 v2023 [time][lat][lon], 0.009°, 1990 Mediterranean Sea - Po River - DIVAnd 4D seasonal analysis of Water body phosphate 1960/2020 v2023. Water body chlorophyll-a - Seasonal Climatology for Po River for the period 1960-2020 on the domain: Lon E12.0-14.0deg., Lat N44.0-46.0deg.\nData Sources: observational data from SeaDataNet/EMODNet Chemistry Data Network.\nDescription of DIVA analysis: The computation was done with the DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.9, using GEBCO 30sec topography for the spatial connectivity of water masses.\nThe horizontal resolution of the produced DIVAnd maps grids is dx=dy=0.009 degrees (around 975m and 708m accordingly).\nThe vertical resolution is 14 depth levels: [0., 2., 4., 6., 8., 10., 15., 20., 25., 30., 40., 50., 60., 70.].\nA relative correlation length used based on topography gradients and the horizontal correlation length varies from 25 km to 12.5 km. The vertical correlation length (in meters) is:  [4.,4.,4.,4.,4.,10.,10.,10.,10.,20.,20.,20.,20.,20.]. \nDuplicates check was performed using the following criteria for space and time: dlon=0.01deg., dlat=0.01deg., ddepth=0.01m, dtime=1min, dvalue=0.01.\nThe error variance (epsilon2) was set equal to 1. Data weight was reduced at shallow waters. Data weighting was applied with the following threshold values: lon=0.03, lat=0.03, depth=2.\nAn anamorphosis transformation was applied to the data (function DIVAnd.Anam.loglin) to avoid unrealistic negative values: threshold value=200.\nThe mean value was used as background analysis field.\nQuality control of the observations was applied using the interpolated field (QCMETHOD=3). Residuals (differences between the observations and the analysis (interpolated linearly to the location of the observations) were calculated. Observations with residuals outside the minimum and maximum values of the 99% quantile were discarded from the analysis. \nSeasons definition: Winter=Jan-Mar, Spring=Apr-Jun, Summer=Jul-Sep, Autumn=Oct-Dec.\nOriginators of Italian data sets-List of contributors:\n- Brunetti Fabio (OGS)\n- Cardin Vanessa, Bensi Manuel doi:10.6092/36728450-4296-4e6a-967d-d5b6da55f306\n- Cardin Vanessa, Bensi Manuel, Ursella Laura, Siena Giuseppe doi:10.6092/f8e6d18e-f877-4aa5-a983-a03b06ccb987\n- Cataletto Bruno (OGS)\n- Cinzia Comici Cinzia (OGS)\n- Civitarese Giuseppe (OGS)\n- DeVittor Cinzia (OGS)\n- Giani Michele (OGS)\n- Kovacevic Vedrana (OGS)\n- Mosetti Renzo (OGS)\n- Solidoro C.,Beran A.,Cataletto B.,Celussi M.,Cibic T.,Comici C.,Del Negro P.,De Vittor C.,Minocci M.,Monti M.,Fabbro C.,Falconi C.,Franzo A.,Libralato S.,Lipizer M.,Negussanti J.S.,Russel H.,Valli G., doi:10.6092/e5518899-b914-43b0-8139-023718aa63f5\n- Celio Massimo (ARPA FVG)\n- Malaguti Antonella (ENEA)\n- Fonda Umani Serena (UNITS)\n- Bignami Francesco (ISAC/National Research Council (CNR))\n- Boldrini Alfredo (ISMAR/CNR)\n- Marini Mauro (ISMAR/CNR)\n- Miserocchi Stefano (ISMAR/CNR)\n- Zaccone Renata (IAMC/CNR)\n- Lavezza, R., Dubroca, L. F. C., Ludicone, D., Kress, N., Herut, B., Civitarese, G., Cruzado, A., Lefevre, D.,Souvermezoglou, E., Yilmaz, A., Tugrul, S., and Ribera d'Alcala, M.: Compilation of quality controlled nutrient profiles from the Mediterranean Sea, doi:10.1594/PANGAEA.771907, 2011.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][latitude][longitude]):\nWater_body_phosphate_deepest (Deepest values of Water body phosphate, umol/l)\n /erddap/metadata/fgdc/xml/V2023_chemistry_2053_0031_2533_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_2053_0031_2533_iso19115.xml /erddap/info/V2023_chemistry_2053_0031_2533/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Mediterranean_Sea_-_Po_River/Water_body_phosphate.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_2053_0031_2533.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_2053_0031_2533&showErrors=false&email= Hellenic Centre for Marine Research, Hellenic National Oceanographic Data Centre V2023_chemistry_2053_0031_2533
/erddap/griddap/V2023_chemistry_ebf0_015f_78bd /erddap/griddap/V2023_chemistry_ebf0_015f_78bd.graph /erddap/wms/V2023_chemistry_ebf0_015f_78bd/request Mediterranean Sea, Po River, DIVAnd 4D seasonal analysis of Water body silicate 1980/2021 v2023 [time][depth][lat][lon], 0.009°, 2000 Mediterranean Sea - Po River - DIVAnd 4D seasonal analysis of Water body silicate 1980/2021 v2023. Water body chlorophyll-a - Seasonal Climatology for Po River for the period 1960-2020 on the domain: Lon E12.0-14.0deg., Lat N44.0-46.0deg.\nData Sources: observational data from SeaDataNet/EMODNet Chemistry Data Network.\nDescription of DIVA analysis: The computation was done with the DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.9, using GEBCO 30sec topography for the spatial connectivity of water masses.\nThe horizontal resolution of the produced DIVAnd maps grids is dx=dy=0.009 degrees (around 975m and 708m accordingly).\nThe vertical resolution is 14 depth levels: [0., 2., 4., 6., 8., 10., 15., 20., 25., 30., 40., 50., 60., 70.].\nA relative correlation length used based on topography gradients and the horizontal correlation length varies from 25 km to 12.5 km. The vertical correlation length (in meters) is:  [4.,4.,4.,4.,4.,10.,10.,10.,10.,20.,20.,20.,20.,20.]. \nDuplicates check was performed using the following criteria for space and time: dlon=0.01deg., dlat=0.01deg., ddepth=0.01m, dtime=1min, dvalue=0.01.\nThe error variance (epsilon2) was set equal to 1. Data weight was reduced at shallow waters. Data weighting was applied with the following threshold values: lon=0.03, lat=0.03, depth=2.\nAn anamorphosis transformation was applied to the data (function DIVAnd.Anam.loglin) to avoid unrealistic negative values: threshold value=200.\nThe mean value was used as background analysis field.\nQuality control of the observations was applied using the interpolated field (QCMETHOD=3). Residuals (differences between the observations and the analysis (interpolated linearly to the location of the observations) were calculated. Observations with residuals outside the minimum and maximum values of the 99% quantile were discarded from the analysis. \nSeasons definition: Winter=Jan-Mar, Spring=Apr-Jun, Summer=Jul-Sep, Autumn=Oct-Dec.\nOriginators of Italian data sets-List of contributors:\n- Brunetti Fabio (OGS)\n- Cardin Vanessa, Bensi Manuel doi:10.6092/36728450-4296-4e6a-967d-d5b6da55f306\n- Cardin Vanessa, Bensi Manuel, Ursella Laura, Siena Giuseppe doi:10.6092/f8e6d18e-f877-4aa5-a983-a03b06ccb987\n- Cataletto Bruno (OGS)\n- Cinzia Comici Cinzia (OGS)\n- Civitarese Giuseppe (OGS)\n- DeVittor Cinzia (OGS)\n- Giani Michele (OGS)\n- Kovacevic Vedrana (OGS)\n- Mosetti Renzo (OGS)\n- Solidoro C.,Beran A.,Cataletto B.,Celussi M.,Cibic T.,Comici C.,Del Negro P.,De Vittor C.,Minocci M.,Monti M.,Fabbro C.,Falconi C.,Franzo A.,Libralato S.,Lipizer M.,Negussanti J.S.,Russel H.,Valli G., doi:10.6092/e5518899-b914-43b0-8139-023718aa63f5\n- Celio Massimo (ARPA FVG)\n- Malaguti Antonella (ENEA)\n- Fonda Umani Serena (UNITS)\n- Bignami Francesco (ISAC/National Research Council (CNR))\n- Boldrini Alfredo (ISMAR/CNR)\n- Marini Mauro (ISMAR/CNR)\n- Miserocchi Stefano (ISMAR/CNR)\n- Zaccone Renata (IAMC/CNR)\n- Lavezza, R., Dubroca, L. F. C., Ludicone, D., Kress, N., Herut, B., Civitarese, G., Cruzado, A., Lefevre, D.,Souvermezoglou, E., Yilmaz, A., Tugrul, S., and Ribera d'Alcala, M.: Compilation of quality controlled nutrient profiles from the Mediterranean Sea, doi:10.1594/PANGAEA.771907, 2011.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\nWater_body_silicate_L1 (Water body silicate masked using relative error threshold 0.3, umol/l)\nWater_body_silicate_L2 (Water body silicate masked using relative error threshold 0.5, umol/l)\nWater_body_silicate_relerr (Relative error of Water body silicate, 1)\n /erddap/metadata/fgdc/xml/V2023_chemistry_ebf0_015f_78bd_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_ebf0_015f_78bd_iso19115.xml /erddap/info/V2023_chemistry_ebf0_015f_78bd/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Mediterranean_Sea_-_Po_River/Water_body_silicate.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_ebf0_015f_78bd.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_ebf0_015f_78bd&showErrors=false&email= Hellenic Centre for Marine Research, Hellenic National Oceanographic Data Centre V2023_chemistry_ebf0_015f_78bd
/erddap/griddap/V2023_chemistry_0b22_b380_452e /erddap/griddap/V2023_chemistry_0b22_b380_452e.graph /erddap/wms/V2023_chemistry_0b22_b380_452e/request Mediterranean Sea, Po River, DIVAnd 4D seasonal analysis of Water body silicate 1980/2021 v2023 [time][lat][lon], 0.009°, 2000 Mediterranean Sea - Po River - DIVAnd 4D seasonal analysis of Water body silicate 1980/2021 v2023. Water body chlorophyll-a - Seasonal Climatology for Po River for the period 1960-2020 on the domain: Lon E12.0-14.0deg., Lat N44.0-46.0deg.\nData Sources: observational data from SeaDataNet/EMODNet Chemistry Data Network.\nDescription of DIVA analysis: The computation was done with the DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.9, using GEBCO 30sec topography for the spatial connectivity of water masses.\nThe horizontal resolution of the produced DIVAnd maps grids is dx=dy=0.009 degrees (around 975m and 708m accordingly).\nThe vertical resolution is 14 depth levels: [0., 2., 4., 6., 8., 10., 15., 20., 25., 30., 40., 50., 60., 70.].\nA relative correlation length used based on topography gradients and the horizontal correlation length varies from 25 km to 12.5 km. The vertical correlation length (in meters) is:  [4.,4.,4.,4.,4.,10.,10.,10.,10.,20.,20.,20.,20.,20.]. \nDuplicates check was performed using the following criteria for space and time: dlon=0.01deg., dlat=0.01deg., ddepth=0.01m, dtime=1min, dvalue=0.01.\nThe error variance (epsilon2) was set equal to 1. Data weight was reduced at shallow waters. Data weighting was applied with the following threshold values: lon=0.03, lat=0.03, depth=2.\nAn anamorphosis transformation was applied to the data (function DIVAnd.Anam.loglin) to avoid unrealistic negative values: threshold value=200.\nThe mean value was used as background analysis field.\nQuality control of the observations was applied using the interpolated field (QCMETHOD=3). Residuals (differences between the observations and the analysis (interpolated linearly to the location of the observations) were calculated. Observations with residuals outside the minimum and maximum values of the 99% quantile were discarded from the analysis. \nSeasons definition: Winter=Jan-Mar, Spring=Apr-Jun, Summer=Jul-Sep, Autumn=Oct-Dec.\nOriginators of Italian data sets-List of contributors:\n- Brunetti Fabio (OGS)\n- Cardin Vanessa, Bensi Manuel doi:10.6092/36728450-4296-4e6a-967d-d5b6da55f306\n- Cardin Vanessa, Bensi Manuel, Ursella Laura, Siena Giuseppe doi:10.6092/f8e6d18e-f877-4aa5-a983-a03b06ccb987\n- Cataletto Bruno (OGS)\n- Cinzia Comici Cinzia (OGS)\n- Civitarese Giuseppe (OGS)\n- DeVittor Cinzia (OGS)\n- Giani Michele (OGS)\n- Kovacevic Vedrana (OGS)\n- Mosetti Renzo (OGS)\n- Solidoro C.,Beran A.,Cataletto B.,Celussi M.,Cibic T.,Comici C.,Del Negro P.,De Vittor C.,Minocci M.,Monti M.,Fabbro C.,Falconi C.,Franzo A.,Libralato S.,Lipizer M.,Negussanti J.S.,Russel H.,Valli G., doi:10.6092/e5518899-b914-43b0-8139-023718aa63f5\n- Celio Massimo (ARPA FVG)\n- Malaguti Antonella (ENEA)\n- Fonda Umani Serena (UNITS)\n- Bignami Francesco (ISAC/National Research Council (CNR))\n- Boldrini Alfredo (ISMAR/CNR)\n- Marini Mauro (ISMAR/CNR)\n- Miserocchi Stefano (ISMAR/CNR)\n- Zaccone Renata (IAMC/CNR)\n- Lavezza, R., Dubroca, L. F. C., Ludicone, D., Kress, N., Herut, B., Civitarese, G., Cruzado, A., Lefevre, D.,Souvermezoglou, E., Yilmaz, A., Tugrul, S., and Ribera d'Alcala, M.: Compilation of quality controlled nutrient profiles from the Mediterranean Sea, doi:10.1594/PANGAEA.771907, 2011.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][latitude][longitude]):\nWater_body_silicate_deepest (Deepest values of Water body silicate, umol/l)\n /erddap/metadata/fgdc/xml/V2023_chemistry_0b22_b380_452e_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_0b22_b380_452e_iso19115.xml /erddap/info/V2023_chemistry_0b22_b380_452e/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Mediterranean_Sea_-_Po_River/Water_body_silicate.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_0b22_b380_452e.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_0b22_b380_452e&showErrors=false&email= Hellenic Centre for Marine Research, Hellenic National Oceanographic Data Centre V2023_chemistry_0b22_b380_452e
/erddap/griddap/Po_River_Chl_4D_06e1_24c4_8bde /erddap/griddap/Po_River_Chl_4D_06e1_24c4_8bde.graph /erddap/wms/Po_River_Chl_4D_06e1_24c4_8bde/request Mediterranean Sea, Po River, Water body chlorophyll-a [time][depth][lat][lon], 0.009deg, 1999 DIVAnd analysis of Water body chlorophyll-a. Water body chlorophyll-a - Seasonal Climatology for Po River for the period 1980-2019 on the domain: Lon E12.0-14.0 deg.E, Lat N44.0-46.00 deg.N. \nData Sources: observational data from SeaDataNet/EMODNet Chemistry Data Network.\nDescription of DIVA analysis: The computation was done with the DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.4, using GEBCO 30sec topography for the spatial connectivity of water masses. A relative correlation length used based on topography gradients and the horizontal correlation length varies from 25 km to 12.5 km. The vertical correlation length (in meters) is:  [4.,4.,4.,4.,4.,10.,10.,10.,10.,20.,20.,20.,20.,20.]. Depth range: [0., 2., 4., 6., 8., 10., 15., 20., 25., 30., 40., 50., 60., 70.]. Units: mg/m3. \nThe horizontal resolution of the produced DIVAnd maps grids is dx=dy=0.009 degrees (around 975m and 708m accordingly).\nAdditional analysis parameters: The error variance (epsilon2) was set equal to 1. Data weight was reduced near the coasts. Data weighting was applied with the following threshold values: lon=0.03, lat=0.03, depth=2. Threshold value for log transformation=200.\nSeasons definition: Winter=Jan-Mar, Spring=Apr-Jun, Summer=Jul-Sep, Autumn=Oct-Dec.\nDOI: 10.6092/nv0n-4996\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\nWater_body_chlorophyll_a (mg/m3)\nWater_body_chlorophyll_a_L1 (Water body chlorophyll-a masked using relative error threshold 0.3, mg/m3)\nWater_body_chlorophyll_a_L2 (Water body chlorophyll-a masked using relative error threshold 0.5, mg/m3)\nWater_body_chlorophyll_a_relerr (Relative error of Water body chlorophyll-a, 1)\n /erddap/metadata/fgdc/xml/Po_River_Chl_4D_06e1_24c4_8bde_fgdc.xml /erddap/metadata/iso19115/xml/Po_River_Chl_4D_06e1_24c4_8bde_iso19115.xml /erddap/info/Po_River_Chl_4D_06e1_24c4_8bde/index.htmlTable https://dx.doi.org/10.6092/a8cfb472-10db-4225-9737-5a60da9af523 (external link) https://erddap.emodnet.eu/erddap/rss/Po_River_Chl_4D_06e1_24c4_8bde.rss /erddap/subscriptions/add.html?datasetID=Po_River_Chl_4D_06e1_24c4_8bde&showErrors=false&email= HCMR/HNODC Po_River_Chl_4D_06e1_24c4_8bde
/erddap/griddap/Po_River_Chl_3D_9c0c_4b3a_d981 /erddap/griddap/Po_River_Chl_3D_9c0c_4b3a_d981.graph /erddap/wms/Po_River_Chl_3D_9c0c_4b3a_d981/request Mediterranean Sea, Po River, Water body chlorophyll-a [time][lat][lon], 0.009deg, 1999 DIVAnd analysis of Water body chlorophyll-a. Water body chlorophyll-a - Seasonal Climatology for Po River for the period 1980-2019 on the domain: Lon E12.0-14.0 deg.E, Lat N44.0-46.00 deg.N. \nData Sources: observational data from SeaDataNet/EMODNet Chemistry Data Network.\nDescription of DIVA analysis: The computation was done with the DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.4, using GEBCO 30sec topography for the spatial connectivity of water masses. A relative correlation length used based on topography gradients and the horizontal correlation length varies from 25 km to 12.5 km. The vertical correlation length (in meters) is:  [4.,4.,4.,4.,4.,10.,10.,10.,10.,20.,20.,20.,20.,20.]. Depth range: [0., 2., 4., 6., 8., 10., 15., 20., 25., 30., 40., 50., 60., 70.]. Units: mg/m3. \nThe horizontal resolution of the produced DIVAnd maps grids is dx=dy=0.009 degrees (around 975m and 708m accordingly).\nAdditional analysis parameters: The error variance (epsilon2) was set equal to 1. Data weight was reduced near the coasts. Data weighting was applied with the following threshold values: lon=0.03, lat=0.03, depth=2. Threshold value for log transformation=200.\nSeasons definition: Winter=Jan-Mar, Spring=Apr-Jun, Summer=Jul-Sep, Autumn=Oct-Dec.\nDOI: 10.6092/nv0n-4996\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][latitude][longitude]):\nWater_body_chlorophyll_a_deepest (Deepest values of Water body chlorophyll-a, mg/m3)\nWater_body_chlorophyll_a_deepest_L1 (Deepest values of Water body chlorophyll-a masked using relative error threshold 0.3, mg/m3)\nWater_body_chlorophyll_a_deepest_L2 (Deepest values of Water body chlorophyll-a masked using relative error threshold 0.5, mg/m3)\n /erddap/metadata/fgdc/xml/Po_River_Chl_3D_9c0c_4b3a_d981_fgdc.xml /erddap/metadata/iso19115/xml/Po_River_Chl_3D_9c0c_4b3a_d981_iso19115.xml /erddap/info/Po_River_Chl_3D_9c0c_4b3a_d981/index.htmlTable https://dx.doi.org/10.6092/a8cfb472-10db-4225-9737-5a60da9af523 (external link) https://erddap.emodnet.eu/erddap/rss/Po_River_Chl_3D_9c0c_4b3a_d981.rss /erddap/subscriptions/add.html?datasetID=Po_River_Chl_3D_9c0c_4b3a_d981&showErrors=false&email= HCMR/HNODC Po_River_Chl_3D_9c0c_4b3a_d981
/erddap/griddap/Po_River_DO_4D_dcba_3cdd_31e2 /erddap/griddap/Po_River_DO_4D_dcba_3cdd_31e2.graph /erddap/wms/Po_River_DO_4D_dcba_3cdd_31e2/request Mediterranean Sea, Po River, Water body dissolved oxygen concentration [time][depth][lat][lon], 0.009deg, 1989 DIVAnd analysis of Water body dissolved oxygen concentration. Water body dissolved oxygen concentration - Seasonal Climatology for Po River for the period 1960-2019 on the domain: Lon E12.0-14.0 deg.E, Lat N44.0-46.00 deg.N. \nData Sources: observational data from SeaDataNet/EMODNet Chemistry Data Network.\nDescription of DIVA analysis: The computation was done with the DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.4, using GEBCO 30sec topography for the spatial connectivity of water masses. A relative correlation length used based on topography gradients and the horizontal correlation length varies from 25 km to 12.5 km. The vertical correlation length (in meters) is:  [4.,4.,4.,4.,4.,10.,10.,10.,10.,20.,20.,20.,20.,20.]. Depth range: [0., 2., 4., 6., 8., 10., 15., 20., 25., 30., 40., 50., 60., 70.]. Units: umol/l. \nThe horizontal resolution of the produced DIVAnd maps grids is dx=dy=0.009 degrees (around 975m and 708m accordingly).\nAdditional analysis parameters: The error variance (epsilon2) was set equal to 1. Data weight was reduced near the coasts. Data weighting was applied with the following threshold values: lon=0.03, lat=0.03, depth=2. Threshold value for log transformation=200.\nSeasons definition: Winter=Jan-Mar, Spring=Apr-Jun, Summer=Jul-Sep, Autumn=Oct-Dec.\nDOI: 10.6092/tasv-9066\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\nWater_body_dissolved_oxygen_concentration (umol/l)\nWater_body_dissolved_oxygen_concentration_L1 (Water body dissolved oxygen concentration masked using relative error threshold 0.3, umol/l)\nWater_body_dissolved_oxygen_concentration_L2 (Water body dissolved oxygen concentration masked using relative error threshold 0.5, umol/l)\nWater_body_dissolved_oxygen_concentration_relerr (Relative error of Water body dissolved oxygen concentration, 1)\n /erddap/metadata/fgdc/xml/Po_River_DO_4D_dcba_3cdd_31e2_fgdc.xml /erddap/metadata/iso19115/xml/Po_River_DO_4D_dcba_3cdd_31e2_iso19115.xml /erddap/info/Po_River_DO_4D_dcba_3cdd_31e2/index.htmlTable https://dx.doi.org/10.6092/a8cfb472-10db-4225-9737-5a60da9af523 (external link) https://erddap.emodnet.eu/erddap/rss/Po_River_DO_4D_dcba_3cdd_31e2.rss /erddap/subscriptions/add.html?datasetID=Po_River_DO_4D_dcba_3cdd_31e2&showErrors=false&email= HCMR/HNODC Po_River_DO_4D_dcba_3cdd_31e2
/erddap/griddap/Po_River_DO_3D_2a2b_954d_a6a3 /erddap/griddap/Po_River_DO_3D_2a2b_954d_a6a3.graph /erddap/wms/Po_River_DO_3D_2a2b_954d_a6a3/request Mediterranean Sea, Po River, Water body dissolved oxygen concentration [time][lat][lon], 0.009deg, 1989 DIVAnd analysis of Water body dissolved oxygen concentration. Water body dissolved oxygen concentration - Seasonal Climatology for Po River for the period 1960-2019 on the domain: Lon E12.0-14.0 deg.E, Lat N44.0-46.00 deg.N. \nData Sources: observational data from SeaDataNet/EMODNet Chemistry Data Network.\nDescription of DIVA analysis: The computation was done with the DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.4, using GEBCO 30sec topography for the spatial connectivity of water masses. A relative correlation length used based on topography gradients and the horizontal correlation length varies from 25 km to 12.5 km. The vertical correlation length (in meters) is:  [4.,4.,4.,4.,4.,10.,10.,10.,10.,20.,20.,20.,20.,20.]. Depth range: [0., 2., 4., 6., 8., 10., 15., 20., 25., 30., 40., 50., 60., 70.]. Units: umol/l. \nThe horizontal resolution of the produced DIVAnd maps grids is dx=dy=0.009 degrees (around 975m and 708m accordingly).\nAdditional analysis parameters: The error variance (epsilon2) was set equal to 1. Data weight was reduced near the coasts. Data weighting was applied with the following threshold values: lon=0.03, lat=0.03, depth=2. Threshold value for log transformation=200.\nSeasons definition: Winter=Jan-Mar, Spring=Apr-Jun, Summer=Jul-Sep, Autumn=Oct-Dec.\nDOI: 10.6092/tasv-9066\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][latitude][longitude]):\nWater_body_dissolved_oxygen_concentration_deepest (Deepest values of Water body dissolved oxygen concentration, umol/l)\nWater_body_dissolved_oxygen_concentration_deepest_L1 (Deepest values of Water body dissolved oxygen concentration masked using relative error threshold 0.3, umol/l)\nWater_body_dissolved_oxygen_concentration_deepest_L2 (Deepest values of Water body dissolved oxygen concentration masked using relative error threshold 0.5, umol/l)\n /erddap/metadata/fgdc/xml/Po_River_DO_3D_2a2b_954d_a6a3_fgdc.xml /erddap/metadata/iso19115/xml/Po_River_DO_3D_2a2b_954d_a6a3_iso19115.xml /erddap/info/Po_River_DO_3D_2a2b_954d_a6a3/index.htmlTable https://dx.doi.org/10.6092/a8cfb472-10db-4225-9737-5a60da9af523 (external link) https://erddap.emodnet.eu/erddap/rss/Po_River_DO_3D_2a2b_954d_a6a3.rss /erddap/subscriptions/add.html?datasetID=Po_River_DO_3D_2a2b_954d_a6a3&showErrors=false&email= HCMR/HNODC Po_River_DO_3D_2a2b_954d_a6a3
/erddap/griddap/Po_River_PO_4D_75c4_4094_e91e /erddap/griddap/Po_River_PO_4D_75c4_4094_e91e.graph /erddap/wms/Po_River_PO_4D_75c4_4094_e91e/request Mediterranean Sea, Po River, Water body phosphate (DIVAnd analysis of Water body phosphate) [time][depth][lat][lon], 0.009deg, 1989 DIVAnd analysis of Water body phosphate. Water body phosphate - Seasonal Climatology for Po River for the period 1980-2019 on the domain: Lon E12.0-14.0 deg.E, Lat N44.0-46.00 deg.N. \nData Sources: observational data from SeaDataNet/EMODNet Chemistry Data Network.\nDescription of DIVA analysis: The computation was done with the DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.4, using GEBCO 30sec topography for the spatial connectivity of water masses. A relative correlation length used based on topography gradients and the horizontal correlation length varies from 25 km to 12.5 km. The vertical correlation length (in meters) is:  [4.,4.,4.,4.,4.,10.,10.,10.,10.,20.,20.,20.,20.,20.]. Depth range: [0., 2., 4., 6., 8., 10., 15., 20., 25., 30., 40., 50., 60., 70.]. Units: umol/l. \nThe horizontal resolution of the produced DIVAnd maps grids is dx=dy=0.009 degrees (around 975m and 708m accordingly).\nAdditional analysis parameters: The error variance (epsilon2) was set equal to 1. Data weight was reduced near the coasts. Data weighting was applied with the following threshold values: lon=0.03, lat=0.03, depth=2. Threshold value for log transformation=200.\nSeasons definition: Winter=Jan-Mar, Spring=Apr-Jun, Summer=Jul-Sep, Autumn=Oct-Dec.\nDOI: 10.6092/jb28-9k33\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\nWater_body_phosphate (umol/l)\nWater_body_phosphate_L1 (Water body phosphate masked using relative error threshold 0.3, umol/l)\nWater_body_phosphate_L2 (Water body phosphate masked using relative error threshold 0.5, umol/l)\nWater_body_phosphate_relerr (Relative error of Water body phosphate, 1)\n /erddap/metadata/fgdc/xml/Po_River_PO_4D_75c4_4094_e91e_fgdc.xml /erddap/metadata/iso19115/xml/Po_River_PO_4D_75c4_4094_e91e_iso19115.xml /erddap/info/Po_River_PO_4D_75c4_4094_e91e/index.htmlTable https://dx.doi.org/10.6092/a8cfb472-10db-4225-9737-5a60da9af523 (external link) https://erddap.emodnet.eu/erddap/rss/Po_River_PO_4D_75c4_4094_e91e.rss /erddap/subscriptions/add.html?datasetID=Po_River_PO_4D_75c4_4094_e91e&showErrors=false&email= HCMR/HNODC Po_River_PO_4D_75c4_4094_e91e
/erddap/griddap/Po_River_PO_3D_8f89_8297_d148 /erddap/griddap/Po_River_PO_3D_8f89_8297_d148.graph /erddap/wms/Po_River_PO_3D_8f89_8297_d148/request Mediterranean Sea, Po River, Water body phosphate (DIVAnd analysis of Water body phosphate) [time][lat][lon], 0.009deg, 1989 DIVAnd analysis of Water body phosphate. Water body phosphate - Seasonal Climatology for Po River for the period 1980-2019 on the domain: Lon E12.0-14.0 deg.E, Lat N44.0-46.00 deg.N. \nData Sources: observational data from SeaDataNet/EMODNet Chemistry Data Network.\nDescription of DIVA analysis: The computation was done with the DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.4, using GEBCO 30sec topography for the spatial connectivity of water masses. A relative correlation length used based on topography gradients and the horizontal correlation length varies from 25 km to 12.5 km. The vertical correlation length (in meters) is:  [4.,4.,4.,4.,4.,10.,10.,10.,10.,20.,20.,20.,20.,20.]. Depth range: [0., 2., 4., 6., 8., 10., 15., 20., 25., 30., 40., 50., 60., 70.]. Units: umol/l. \nThe horizontal resolution of the produced DIVAnd maps grids is dx=dy=0.009 degrees (around 975m and 708m accordingly).\nAdditional analysis parameters: The error variance (epsilon2) was set equal to 1. Data weight was reduced near the coasts. Data weighting was applied with the following threshold values: lon=0.03, lat=0.03, depth=2. Threshold value for log transformation=200.\nSeasons definition: Winter=Jan-Mar, Spring=Apr-Jun, Summer=Jul-Sep, Autumn=Oct-Dec.\nDOI: 10.6092/jb28-9k33\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][latitude][longitude]):\nWater_body_phosphate_deepest (Deepest values of Water body phosphate, umol/l)\nWater_body_phosphate_deepest_L1 (Deepest values of Water body phosphate masked using relative error threshold 0.3, umol/l)\nWater_body_phosphate_deepest_L2 (Deepest values of Water body phosphate masked using relative error threshold 0.5, umol/l)\n /erddap/metadata/fgdc/xml/Po_River_PO_3D_8f89_8297_d148_fgdc.xml /erddap/metadata/iso19115/xml/Po_River_PO_3D_8f89_8297_d148_iso19115.xml /erddap/info/Po_River_PO_3D_8f89_8297_d148/index.htmlTable https://dx.doi.org/10.6092/a8cfb472-10db-4225-9737-5a60da9af523 (external link) https://erddap.emodnet.eu/erddap/rss/Po_River_PO_3D_8f89_8297_d148.rss /erddap/subscriptions/add.html?datasetID=Po_River_PO_3D_8f89_8297_d148&showErrors=false&email= HCMR/HNODC Po_River_PO_3D_8f89_8297_d148
/erddap/griddap/Po_River_Si_4D_393e_92ca_073c /erddap/griddap/Po_River_Si_4D_393e_92ca_073c.graph /erddap/wms/Po_River_Si_4D_393e_92ca_073c/request Mediterranean Sea, Po River, Water body silicate (DIVAnd analysis of Water body silicate) [time][depth][lat][lon], 0.009deg, 1999 DIVAnd analysis of Water body silicate. Water body silicate - Seasonal Climatology for Po River for the period 1980-2019 on the domain: Lon E12.0-14.0 deg.E, Lat N44.0-46.00 deg.N. \nData Sources: observational data from SeaDataNet/EMODNet Chemistry Data Network.\nDescription of DIVA analysis: The computation was done with the DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.4, using GEBCO 30sec topography for the spatial connectivity of water masses. A relative correlation length used based on topography gradients and the horizontal correlation length varies from 25 km to 12.5 km. The vertical correlation length (in meters) is:  [4.,4.,4.,4.,4.,10.,10.,10.,10.,20.,20.,20.,20.,20.]. Depth range: [0., 2., 4., 6., 8., 10., 15., 20., 25., 30., 40., 50., 60., 70.]. Units: umol/l. \nThe horizontal resolution of the produced DIVAnd maps grids is dx=dy=0.009 degrees (around 975m and 708m accordingly).\nAdditional analysis parameters: The error variance (epsilon2) was set equal to 1. Data weight was reduced near the coasts. Data weighting was applied with the following threshold values: lon=0.03, lat=0.03, depth=2. Threshold value for log transformation=200.\nSeasons definition: Winter=Jan-Mar, Spring=Apr-Jun, Summer=Jul-Sep, Autumn=Oct-Dec.\nDOI: 10.6092/njvc-n987\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\nWater_body_silicate (umol/l)\nWater_body_silicate_L1 (Water body silicate masked using relative error threshold 0.3, umol/l)\nWater_body_silicate_L2 (Water body silicate masked using relative error threshold 0.5, umol/l)\nWater_body_silicate_relerr (Relative error of Water body silicate, 1)\n /erddap/metadata/fgdc/xml/Po_River_Si_4D_393e_92ca_073c_fgdc.xml /erddap/metadata/iso19115/xml/Po_River_Si_4D_393e_92ca_073c_iso19115.xml /erddap/info/Po_River_Si_4D_393e_92ca_073c/index.htmlTable https://dx.doi.org/10.6092/a8cfb472-10db-4225-9737-5a60da9af523 (external link) https://erddap.emodnet.eu/erddap/rss/Po_River_Si_4D_393e_92ca_073c.rss /erddap/subscriptions/add.html?datasetID=Po_River_Si_4D_393e_92ca_073c&showErrors=false&email= HCMR/HNODC Po_River_Si_4D_393e_92ca_073c
/erddap/griddap/Po_River_Si_3D_3499_eaa1_1119 /erddap/griddap/Po_River_Si_3D_3499_eaa1_1119.graph /erddap/wms/Po_River_Si_3D_3499_eaa1_1119/request Mediterranean Sea, Po River, Water body silicate (DIVAnd analysis of Water body silicate) [time][lat][lon], 0.009deg, 1999 DIVAnd analysis of Water body silicate. Water body silicate - Seasonal Climatology for Po River for the period 1980-2019 on the domain: Lon E12.0-14.0 deg.E, Lat N44.0-46.00 deg.N. \nData Sources: observational data from SeaDataNet/EMODNet Chemistry Data Network.\nDescription of DIVA analysis: The computation was done with the DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.4, using GEBCO 30sec topography for the spatial connectivity of water masses. A relative correlation length used based on topography gradients and the horizontal correlation length varies from 25 km to 12.5 km. The vertical correlation length (in meters) is:  [4.,4.,4.,4.,4.,10.,10.,10.,10.,20.,20.,20.,20.,20.]. Depth range: [0., 2., 4., 6., 8., 10., 15., 20., 25., 30., 40., 50., 60., 70.]. Units: umol/l. \nThe horizontal resolution of the produced DIVAnd maps grids is dx=dy=0.009 degrees (around 975m and 708m accordingly).\nAdditional analysis parameters: The error variance (epsilon2) was set equal to 1. Data weight was reduced near the coasts. Data weighting was applied with the following threshold values: lon=0.03, lat=0.03, depth=2. Threshold value for log transformation=200.\nSeasons definition: Winter=Jan-Mar, Spring=Apr-Jun, Summer=Jul-Sep, Autumn=Oct-Dec.\nDOI: 10.6092/njvc-n987\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][latitude][longitude]):\nWater_body_silicate_deepest (Deepest values of Water body silicate, umol/l)\nWater_body_silicate_deepest_L1 (Deepest values of Water body silicate masked using relative error threshold 0.3, umol/l)\nWater_body_silicate_deepest_L2 (Deepest values of Water body silicate masked using relative error threshold 0.5, umol/l)\n /erddap/metadata/fgdc/xml/Po_River_Si_3D_3499_eaa1_1119_fgdc.xml /erddap/metadata/iso19115/xml/Po_River_Si_3D_3499_eaa1_1119_iso19115.xml /erddap/info/Po_River_Si_3D_3499_eaa1_1119/index.htmlTable https://dx.doi.org/10.6092/a8cfb472-10db-4225-9737-5a60da9af523 (external link) https://erddap.emodnet.eu/erddap/rss/Po_River_Si_3D_3499_eaa1_1119.rss /erddap/subscriptions/add.html?datasetID=Po_River_Si_3D_3499_eaa1_1119&showErrors=false&email= HCMR/HNODC Po_River_Si_3D_3499_eaa1_1119
/erddap/griddap/V2023_chemistry_2017_e873_a8c5 /erddap/griddap/V2023_chemistry_2017_e873_a8c5.graph /erddap/wms/V2023_chemistry_2017_e873_a8c5/request Northeast Atlantic Ocean, Loire River, DIVAnd 4D seasonal analysis of Water body chlorophyll-a 1971/2021 v2023 [time][depth][lat][lon], 1996 Northeast Atlantic Ocean - Loire River - DIVAnd 4D seasonal analysis of Water body chlorophyll-a 1971/2021 v2023. Seasonal climatology of Water body chlorophyll-a for Loire river for the period 1971-2021 and for the following seasons:\n - winter: January-March,\n - spring: April-June,\n - summer: July-September,\n - autumn: October-December. \nObservation data span from 1971 to 2021. \nDepth levels (m): [0.0, 2.0, 4.0, 6.0, 8.0, 10.0, 15.0, 20.0, 25.0, 30.0, 35.0, 40.0, 45.0, 50.0, 60.0, 70.0, 80.0, 90.0, 100.0, 110.0, 120.0, 130.0]. \nData sources: observational data from SeaDataNet/EMODNet Chemistry Data Network. \nDescription of DIVAnd analysis: the computation was done with DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.4, using GEBCO 15 sec topography for the spatial connectivity of water masses. The horizontal resolution of the produced DIVAnd maps is 0.01 degrees. Horizontal correlation length is defined seasonally (in meters): 14000 (winter), 52000 (spring), 42000 (summer), 125000 (autumn). Vertical correlation length was optimized and vertically filtered and a seasonally-averaged profile was used (DIVAnd.fitvertlen). Signal-to-noise ratio was fixed to 1 for vertical profiles and 0.1 for time series to account for the redundancy in the time series observations. A logarithmic transformation (DIVAnd.loglin) was applied to the data prior to the analysis. Background field: the vertically-filtered data mean profile is substracted from the data. Detrending of data: no, advection constraint applied: no. \nUnits: mg/m3.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\nWater_body_chlorophyll_a_L1 (Water body chlorophyll-a masked using relative error threshold 0.3, mg/m3)\nWater_body_chlorophyll_a_L2 (Water body chlorophyll-a masked using relative error threshold 0.5, mg/m3)\nWater_body_chlorophyll_a_relerr (Relative error of Water body chlorophyll-a, 1)\n /erddap/metadata/fgdc/xml/V2023_chemistry_2017_e873_a8c5_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_2017_e873_a8c5_iso19115.xml /erddap/info/V2023_chemistry_2017_e873_a8c5/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Northeast_Atlantic_Ocean_-_Loire_River/Water_body_chlorophyll-a.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_2017_e873_a8c5.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_2017_e873_a8c5&showErrors=false&email= IFREMER, SISMER, Scientific Information Systems for the SEA V2023_chemistry_2017_e873_a8c5
/erddap/griddap/V2023_chemistry_b2a6_a73e_c754 /erddap/griddap/V2023_chemistry_b2a6_a73e_c754.graph /erddap/wms/V2023_chemistry_b2a6_a73e_c754/request Northeast Atlantic Ocean, Loire River, DIVAnd 4D seasonal analysis of Water body chlorophyll-a 1971/2021 v2023 [time][lat][lon], 1996 Northeast Atlantic Ocean - Loire River - DIVAnd 4D seasonal analysis of Water body chlorophyll-a 1971/2021 v2023. Seasonal climatology of Water body chlorophyll-a for Loire river for the period 1971-2021 and for the following seasons:\n - winter: January-March,\n - spring: April-June,\n - summer: July-September,\n - autumn: October-December. \nObservation data span from 1971 to 2021. \nDepth levels (m): [0.0, 2.0, 4.0, 6.0, 8.0, 10.0, 15.0, 20.0, 25.0, 30.0, 35.0, 40.0, 45.0, 50.0, 60.0, 70.0, 80.0, 90.0, 100.0, 110.0, 120.0, 130.0]. \nData sources: observational data from SeaDataNet/EMODNet Chemistry Data Network. \nDescription of DIVAnd analysis: the computation was done with DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.4, using GEBCO 15 sec topography for the spatial connectivity of water masses. The horizontal resolution of the produced DIVAnd maps is 0.01 degrees. Horizontal correlation length is defined seasonally (in meters): 14000 (winter), 52000 (spring), 42000 (summer), 125000 (autumn). Vertical correlation length was optimized and vertically filtered and a seasonally-averaged profile was used (DIVAnd.fitvertlen). Signal-to-noise ratio was fixed to 1 for vertical profiles and 0.1 for time series to account for the redundancy in the time series observations. A logarithmic transformation (DIVAnd.loglin) was applied to the data prior to the analysis. Background field: the vertically-filtered data mean profile is substracted from the data. Detrending of data: no, advection constraint applied: no. \nUnits: mg/m3.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][latitude][longitude]):\nWater_body_chlorophyll_a_deepest (Deepest values of Water body chlorophyll-a, mg/m3)\n /erddap/metadata/fgdc/xml/V2023_chemistry_b2a6_a73e_c754_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_b2a6_a73e_c754_iso19115.xml /erddap/info/V2023_chemistry_b2a6_a73e_c754/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Northeast_Atlantic_Ocean_-_Loire_River/Water_body_chlorophyll-a.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_b2a6_a73e_c754.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_b2a6_a73e_c754&showErrors=false&email= IFREMER, SISMER, Scientific Information Systems for the SEA V2023_chemistry_b2a6_a73e_c754
/erddap/griddap/V2023_chemistry_cfa2_241c_32d8 /erddap/griddap/V2023_chemistry_cfa2_241c_32d8.graph /erddap/wms/V2023_chemistry_cfa2_241c_32d8/request Northeast Atlantic Ocean, Loire River, DIVAnd 4D seasonal analysis of Water body dissolved inorganic nitrogen 1971/2021 v2023 [time][depth][lat][lon], 1996 Northeast Atlantic Ocean - Loire River - DIVAnd 4D seasonal analysis of Water body dissolved inorganic nitrogen 1971/2021 v2023. Seasonal climatology of Water body dissolved inorganic nitrogen for Loire river for the period 1971-2021 and for the following seasons:\n - winter: January-March,\n - spring: April-June,\n - summer: July-September,\n - autumn: October-December. \nObservation data span from 1971 to 2021. \nDepth levels (m): [0.0, 2.0, 4.0, 6.0, 8.0, 10.0, 15.0, 20.0, 25.0, 30.0, 35.0, 40.0, 45.0, 50.0, 60.0, 70.0, 80.0, 90.0, 100.0, 110.0, 120.0, 130.0]. \nData sources: observational data from SeaDataNet/EMODNet Chemistry Data Network. \nDescription of DIVAnd analysis: the computation was done with DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.4, using GEBCO 15 sec topography for the spatial connectivity of water masses. The horizontal resolution of the produced DIVAnd maps is 0.01 degrees. Horizontal correlation length is defined seasonally (in meters): 72000 (winter), 43000 (spring), 215000 (summer), 150000 (autumn). Vertical correlation length was optimized and vertically filtered and a seasonally-averaged profile was used (DIVAnd.fitvertlen). Signal-to-noise ratio was fixed to 1 for vertical profiles and 0.1 for time series to account for the redundancy in the time series observations. A logarithmic transformation (DIVAnd.loglin) was applied to the data prior to the analysis. Background field: the vertically-filtered data mean profile is substracted from the data. Detrending of data: no, advection constraint applied: no. \nUnits: umol/l.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\nWater_body_dissolved_inorganic_nitrogen_L1 (Water body dissolved inorganic nitrogen masked using relative error threshold 0.3, umol/l)\nWater_body_dissolved_inorganic_nitrogen_L2 (Water body dissolved inorganic nitrogen masked using relative error threshold 0.5, umol/l)\nWater_body_dissolved_inorganic_nitrogen_relerr (Relative error of Water body dissolved inorganic nitrogen, 1)\n /erddap/metadata/fgdc/xml/V2023_chemistry_cfa2_241c_32d8_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_cfa2_241c_32d8_iso19115.xml /erddap/info/V2023_chemistry_cfa2_241c_32d8/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Northeast_Atlantic_Ocean_-_Loire_River/Water_body_dissolved_inorganic_nitrogen.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_cfa2_241c_32d8.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_cfa2_241c_32d8&showErrors=false&email= IFREMER, SISMER, Scientific Information Systems for the SEA V2023_chemistry_cfa2_241c_32d8
/erddap/griddap/V2023_chemistry_fa1c_0df9_0a3a /erddap/griddap/V2023_chemistry_fa1c_0df9_0a3a.graph Northeast Atlantic Ocean, Loire River, DIVAnd 4D seasonal analysis of Water body dissolved inorganic nitrogen 1971/2021 v2023 [time][lat][lon], 1996 Northeast Atlantic Ocean - Loire River - DIVAnd 4D seasonal analysis of Water body dissolved inorganic nitrogen 1971/2021 v2023. Seasonal climatology of Water body dissolved inorganic nitrogen for Loire river for the period 1971-2021 and for the following seasons:\n - winter: January-March,\n - spring: April-June,\n - summer: July-September,\n - autumn: October-December. \nObservation data span from 1971 to 2021. \nDepth levels (m): [0.0, 2.0, 4.0, 6.0, 8.0, 10.0, 15.0, 20.0, 25.0, 30.0, 35.0, 40.0, 45.0, 50.0, 60.0, 70.0, 80.0, 90.0, 100.0, 110.0, 120.0, 130.0]. \nData sources: observational data from SeaDataNet/EMODNet Chemistry Data Network. \nDescription of DIVAnd analysis: the computation was done with DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.4, using GEBCO 15 sec topography for the spatial connectivity of water masses. The horizontal resolution of the produced DIVAnd maps is 0.01 degrees. Horizontal correlation length is defined seasonally (in meters): 72000 (winter), 43000 (spring), 215000 (summer), 150000 (autumn). Vertical correlation length was optimized and vertically filtered and a seasonally-averaged profile was used (DIVAnd.fitvertlen). Signal-to-noise ratio was fixed to 1 for vertical profiles and 0.1 for time series to account for the redundancy in the time series observations. A logarithmic transformation (DIVAnd.loglin) was applied to the data prior to the analysis. Background field: the vertically-filtered data mean profile is substracted from the data. Detrending of data: no, advection constraint applied: no. \nUnits: umol/l.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][latitude][longitude]):\nWater_body_dissolved_inorganic_nitrogen_deepest (Deepest values of Water body dissolved inorganic nitrogen, umol/l)\n /erddap/metadata/fgdc/xml/V2023_chemistry_fa1c_0df9_0a3a_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_fa1c_0df9_0a3a_iso19115.xml /erddap/info/V2023_chemistry_fa1c_0df9_0a3a/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Northeast_Atlantic_Ocean_-_Loire_River/Water_body_dissolved_inorganic_nitrogen.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_fa1c_0df9_0a3a.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_fa1c_0df9_0a3a&showErrors=false&email= IFREMER, SISMER, Scientific Information Systems for the SEA V2023_chemistry_fa1c_0df9_0a3a
/erddap/griddap/V2023_chemistry_ab50_4820_731f /erddap/griddap/V2023_chemistry_ab50_4820_731f.graph /erddap/wms/V2023_chemistry_ab50_4820_731f/request Northeast Atlantic Ocean, Loire River, DIVAnd 4D seasonal analysis of Water body dissolved oxygen concentration 1950/2021 v2023 [time][depth][lat][lon], 1985 Northeast Atlantic Ocean - Loire River - DIVAnd 4D seasonal analysis of Water body dissolved oxygen concentration 1950/2021 v2023. Seasonal climatology of Water body dissolved oxygen concentration for Loire river for the period 1950-2021 and for the following seasons:\n - winter: January-March,\n - spring: April-June,\n - summer: July-September,\n - autumn: October-December. \nObservation data span from 1950 to 2021. \nDepth levels (m): [0.0, 2.0, 4.0, 6.0, 8.0, 10.0, 15.0, 20.0, 25.0, 30.0, 35.0, 40.0, 45.0, 50.0, 60.0, 70.0, 80.0, 90.0, 100.0, 110.0, 120.0, 130.0]. \nData sources: observational data from SeaDataNet/EMODNet Chemistry Data Network. \nDescription of DIVAnd analysis: the computation was done with DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.4, using GEBCO 15 sec topography for the spatial connectivity of water masses. The horizontal resolution of the produced DIVAnd maps is 0.01 degrees. Horizontal correlation length is defined seasonally (in meters): 150000 (winter), 100000 (spring), 70000 (summer), 115000 (autumn). Vertical correlation length was optimized and vertically filtered and a seasonally-averaged profile was used (DIVAnd.fitvertlen). Signal-to-noise ratio was fixed to 1 for vertical profiles and 0.1 for time series to account for the redundancy in the time series observations. A logarithmic transformation (DIVAnd.loglin) was applied to the data prior to the analysis. Background field: the vertically-filtered data mean profile is substracted from the data. Detrending of data: no, advection constraint applied: no. \nUnits: umol/l.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\nWater_body_dissolved_oxygen_concentration_L1 (Water body dissolved oxygen concentration masked using relative error threshold 0.3, umol/l)\nWater_body_dissolved_oxygen_concentration_L2 (Water body dissolved oxygen concentration masked using relative error threshold 0.5, umol/l)\nWater_body_dissolved_oxygen_concentration_relerr (Relative error of Water body dissolved oxygen concentration, 1)\n /erddap/metadata/fgdc/xml/V2023_chemistry_ab50_4820_731f_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_ab50_4820_731f_iso19115.xml /erddap/info/V2023_chemistry_ab50_4820_731f/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Northeast_Atlantic_Ocean_-_Loire_River/Water_body_dissolved_oxygen_concentration.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_ab50_4820_731f.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_ab50_4820_731f&showErrors=false&email= IFREMER, SISMER, Scientific Information Systems for the SEA V2023_chemistry_ab50_4820_731f
/erddap/griddap/V2023_chemistry_3a82_17ce_c808 /erddap/griddap/V2023_chemistry_3a82_17ce_c808.graph /erddap/wms/V2023_chemistry_3a82_17ce_c808/request Northeast Atlantic Ocean, Loire River, DIVAnd 4D seasonal analysis of Water body dissolved oxygen concentration 1950/2021 v2023 [time][lat][lon], 1985 Northeast Atlantic Ocean - Loire River - DIVAnd 4D seasonal analysis of Water body dissolved oxygen concentration 1950/2021 v2023. Seasonal climatology of Water body dissolved oxygen concentration for Loire river for the period 1950-2021 and for the following seasons:\n - winter: January-March,\n - spring: April-June,\n - summer: July-September,\n - autumn: October-December. \nObservation data span from 1950 to 2021. \nDepth levels (m): [0.0, 2.0, 4.0, 6.0, 8.0, 10.0, 15.0, 20.0, 25.0, 30.0, 35.0, 40.0, 45.0, 50.0, 60.0, 70.0, 80.0, 90.0, 100.0, 110.0, 120.0, 130.0]. \nData sources: observational data from SeaDataNet/EMODNet Chemistry Data Network. \nDescription of DIVAnd analysis: the computation was done with DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.4, using GEBCO 15 sec topography for the spatial connectivity of water masses. The horizontal resolution of the produced DIVAnd maps is 0.01 degrees. Horizontal correlation length is defined seasonally (in meters): 150000 (winter), 100000 (spring), 70000 (summer), 115000 (autumn). Vertical correlation length was optimized and vertically filtered and a seasonally-averaged profile was used (DIVAnd.fitvertlen). Signal-to-noise ratio was fixed to 1 for vertical profiles and 0.1 for time series to account for the redundancy in the time series observations. A logarithmic transformation (DIVAnd.loglin) was applied to the data prior to the analysis. Background field: the vertically-filtered data mean profile is substracted from the data. Detrending of data: no, advection constraint applied: no. \nUnits: umol/l.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][latitude][longitude]):\nWater_body_dissolved_oxygen_concentration_deepest (Deepest values of Water body dissolved oxygen concentration, umol/l)\n /erddap/metadata/fgdc/xml/V2023_chemistry_3a82_17ce_c808_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_3a82_17ce_c808_iso19115.xml /erddap/info/V2023_chemistry_3a82_17ce_c808/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Northeast_Atlantic_Ocean_-_Loire_River/Water_body_dissolved_oxygen_concentration.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_3a82_17ce_c808.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_3a82_17ce_c808&showErrors=false&email= IFREMER, SISMER, Scientific Information Systems for the SEA V2023_chemistry_3a82_17ce_c808
/erddap/griddap/V2023_chemistry_cbb4_5c8a_d36f /erddap/griddap/V2023_chemistry_cbb4_5c8a_d36f.graph /erddap/wms/V2023_chemistry_cbb4_5c8a_d36f/request Northeast Atlantic Ocean, Loire River, DIVAnd 4D seasonal analysis of Water body phosphate 1950/2021 v2023 [time][depth][lat][lon], 1985 Northeast Atlantic Ocean - Loire River - DIVAnd 4D seasonal analysis of Water body phosphate 1950/2021 v2023. Seasonal climatology of Water body phosphate for Loire river for the period 1950-2021 and for the following seasons:\n - winter: January-March,\n - spring: April-June,\n - summer: July-September,\n - autumn: October-December. \nObservation data span from 1950 to 2021. \nDepth levels (m): [0.0, 2.0, 4.0, 6.0, 8.0, 10.0, 15.0, 20.0, 25.0, 30.0, 35.0, 40.0, 45.0, 50.0, 60.0, 70.0, 80.0, 90.0, 100.0, 110.0, 120.0, 130.0]. \nData sources: observational data from SeaDataNet/EMODNet Chemistry Data Network. \nDescription of DIVAnd analysis: the computation was done with DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.4, using GEBCO 15 sec topography for the spatial connectivity of water masses. The horizontal resolution of the produced DIVAnd maps is 0.01 degrees. Horizontal correlation length is defined seasonally (in meters): 230000 (winter), 264000 (spring), 140000 (summer), 135000 (autumn). Vertical correlation length was optimized and vertically filtered and a seasonally-averaged profile was used (DIVAnd.fitvertlen). Signal-to-noise ratio was fixed to 1 for vertical profiles and 0.1 for time series to account for the redundancy in the time series observations. A logarithmic transformation (DIVAnd.loglin) was applied to the data prior to the analysis. Background field: the vertically-filtered data mean profile is substracted from the data. Detrending of data: no, advection constraint applied: no. \nUnits: umol/l.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\nWater_body_phosphate_L1 (Water body phosphate masked using relative error threshold 0.3, umol/l)\nWater_body_phosphate_L2 (Water body phosphate masked using relative error threshold 0.5, umol/l)\nWater_body_phosphate_relerr (Relative error of Water body phosphate, 1)\n /erddap/metadata/fgdc/xml/V2023_chemistry_cbb4_5c8a_d36f_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_cbb4_5c8a_d36f_iso19115.xml /erddap/info/V2023_chemistry_cbb4_5c8a_d36f/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Northeast_Atlantic_Ocean_-_Loire_River/Water_body_phosphate.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_cbb4_5c8a_d36f.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_cbb4_5c8a_d36f&showErrors=false&email= IFREMER, SISMER, Scientific Information Systems for the SEA V2023_chemistry_cbb4_5c8a_d36f
/erddap/griddap/V2023_chemistry_4782_b7d2_b597 /erddap/griddap/V2023_chemistry_4782_b7d2_b597.graph /erddap/wms/V2023_chemistry_4782_b7d2_b597/request Northeast Atlantic Ocean, Loire River, DIVAnd 4D seasonal analysis of Water body phosphate 1950/2021 v2023 [time][lat][lon], 1985 Northeast Atlantic Ocean - Loire River - DIVAnd 4D seasonal analysis of Water body phosphate 1950/2021 v2023. Seasonal climatology of Water body phosphate for Loire river for the period 1950-2021 and for the following seasons:\n - winter: January-March,\n - spring: April-June,\n - summer: July-September,\n - autumn: October-December. \nObservation data span from 1950 to 2021. \nDepth levels (m): [0.0, 2.0, 4.0, 6.0, 8.0, 10.0, 15.0, 20.0, 25.0, 30.0, 35.0, 40.0, 45.0, 50.0, 60.0, 70.0, 80.0, 90.0, 100.0, 110.0, 120.0, 130.0]. \nData sources: observational data from SeaDataNet/EMODNet Chemistry Data Network. \nDescription of DIVAnd analysis: the computation was done with DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.4, using GEBCO 15 sec topography for the spatial connectivity of water masses. The horizontal resolution of the produced DIVAnd maps is 0.01 degrees. Horizontal correlation length is defined seasonally (in meters): 230000 (winter), 264000 (spring), 140000 (summer), 135000 (autumn). Vertical correlation length was optimized and vertically filtered and a seasonally-averaged profile was used (DIVAnd.fitvertlen). Signal-to-noise ratio was fixed to 1 for vertical profiles and 0.1 for time series to account for the redundancy in the time series observations. A logarithmic transformation (DIVAnd.loglin) was applied to the data prior to the analysis. Background field: the vertically-filtered data mean profile is substracted from the data. Detrending of data: no, advection constraint applied: no. \nUnits: umol/l.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][latitude][longitude]):\nWater_body_phosphate_deepest (Deepest values of Water body phosphate, umol/l)\n /erddap/metadata/fgdc/xml/V2023_chemistry_4782_b7d2_b597_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_4782_b7d2_b597_iso19115.xml /erddap/info/V2023_chemistry_4782_b7d2_b597/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Northeast_Atlantic_Ocean_-_Loire_River/Water_body_phosphate.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_4782_b7d2_b597.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_4782_b7d2_b597&showErrors=false&email= IFREMER, SISMER, Scientific Information Systems for the SEA V2023_chemistry_4782_b7d2_b597
/erddap/griddap/V2023_chemistry_a936_c09f_8933 /erddap/griddap/V2023_chemistry_a936_c09f_8933.graph /erddap/wms/V2023_chemistry_a936_c09f_8933/request Northeast Atlantic Ocean, Loire River, DIVAnd 4D seasonal analysis of Water body silicate 1950/2021 v2023 [time][depth][lat][lon], 1985 Northeast Atlantic Ocean - Loire River - DIVAnd 4D seasonal analysis of Water body silicate 1950/2021 v2023. Seasonal climatology of Water body silicate for Loire river for the period 1950-2021 and for the following seasons:\n - winter: January-March,\n - spring: April-June,\n - summer: July-September,\n - autumn: October-December. \nObservation data span from 1950 to 2021. \nDepth levels (m): [0.0, 2.0, 4.0, 6.0, 8.0, 10.0, 15.0, 20.0, 25.0, 30.0, 35.0, 40.0, 45.0, 50.0, 60.0, 70.0, 80.0, 90.0, 100.0, 110.0, 120.0, 130.0]. \nData sources: observational data from SeaDataNet/EMODNet Chemistry Data Network. \nDescription of DIVAnd analysis: the computation was done with DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.4, using GEBCO 15 sec topography for the spatial connectivity of water masses. The horizontal resolution of the produced DIVAnd maps is 0.01 degrees. Horizontal correlation length is defined seasonally (in meters): 133000 (winter), 180000 (spring), 150000 (summer), 210000 (autumn). Vertical correlation length was optimized and vertically filtered and a seasonally-averaged profile was used (DIVAnd.fitvertlen). Signal-to-noise ratio was fixed to 1 for vertical profiles and 0.1 for time series to account for the redundancy in the time series observations. A logarithmic transformation (DIVAnd.loglin) was applied to the data prior to the analysis. Background field: the vertically-filtered data mean profile is substracted from the data. Detrending of data: no, advection constraint applied: no. \nUnits: umol/l.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\nWater_body_silicate_L1 (Water body silicate masked using relative error threshold 0.3, umol/l)\nWater_body_silicate_L2 (Water body silicate masked using relative error threshold 0.5, umol/l)\nWater_body_silicate_relerr (Relative error of Water body silicate, 1)\n /erddap/metadata/fgdc/xml/V2023_chemistry_a936_c09f_8933_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_a936_c09f_8933_iso19115.xml /erddap/info/V2023_chemistry_a936_c09f_8933/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Northeast_Atlantic_Ocean_-_Loire_River/Water_body_silicate.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_a936_c09f_8933.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_a936_c09f_8933&showErrors=false&email= IFREMER, SISMER, Scientific Information Systems for the SEA V2023_chemistry_a936_c09f_8933
/erddap/griddap/V2023_chemistry_972a_44bb_9bc0 /erddap/griddap/V2023_chemistry_972a_44bb_9bc0.graph /erddap/wms/V2023_chemistry_972a_44bb_9bc0/request Northeast Atlantic Ocean, Loire River, DIVAnd 4D seasonal analysis of Water body silicate 1950/2021 v2023 [time][lat][lon], 1985 Northeast Atlantic Ocean - Loire River - DIVAnd 4D seasonal analysis of Water body silicate 1950/2021 v2023. Seasonal climatology of Water body silicate for Loire river for the period 1950-2021 and for the following seasons:\n - winter: January-March,\n - spring: April-June,\n - summer: July-September,\n - autumn: October-December. \nObservation data span from 1950 to 2021. \nDepth levels (m): [0.0, 2.0, 4.0, 6.0, 8.0, 10.0, 15.0, 20.0, 25.0, 30.0, 35.0, 40.0, 45.0, 50.0, 60.0, 70.0, 80.0, 90.0, 100.0, 110.0, 120.0, 130.0]. \nData sources: observational data from SeaDataNet/EMODNet Chemistry Data Network. \nDescription of DIVAnd analysis: the computation was done with DIVAnd (Data-Interpolating Variational Analysis in n dimensions), version 2.7.4, using GEBCO 15 sec topography for the spatial connectivity of water masses. The horizontal resolution of the produced DIVAnd maps is 0.01 degrees. Horizontal correlation length is defined seasonally (in meters): 133000 (winter), 180000 (spring), 150000 (summer), 210000 (autumn). Vertical correlation length was optimized and vertically filtered and a seasonally-averaged profile was used (DIVAnd.fitvertlen). Signal-to-noise ratio was fixed to 1 for vertical profiles and 0.1 for time series to account for the redundancy in the time series observations. A logarithmic transformation (DIVAnd.loglin) was applied to the data prior to the analysis. Background field: the vertically-filtered data mean profile is substracted from the data. Detrending of data: no, advection constraint applied: no. \nUnits: umol/l.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][latitude][longitude]):\nWater_body_silicate_deepest (Deepest values of Water body silicate, umol/l)\n /erddap/metadata/fgdc/xml/V2023_chemistry_972a_44bb_9bc0_fgdc.xml /erddap/metadata/iso19115/xml/V2023_chemistry_972a_44bb_9bc0_iso19115.xml /erddap/info/V2023_chemistry_972a_44bb_9bc0/index.htmlTable http://opendap.oceanbrowser.net/thredds/dodsC/data/emodnet-projects/v2023/Coastal_areas/Northeast_Atlantic_Ocean_-_Loire_River/Water_body_silicate.nc.html (external link) https://erddap.emodnet.eu/erddap/rss/V2023_chemistry_972a_44bb_9bc0.rss /erddap/subscriptions/add.html?datasetID=V2023_chemistry_972a_44bb_9bc0&showErrors=false&email= IFREMER, SISMER, Scientific Information Systems for the SEA V2023_chemistry_972a_44bb_9bc0

 
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