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ERDDAP - IPMA
Easier access to scientific data |
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Cedido por: NOAA NMFS SWFSC ERD |
| griddap | Subset | tabledap | Make A Graph | wms | files | Title | Summary | FGDC | ISO 19115 | Info | Background Info | RSS | Institution | Dataset ID | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| https://erddap.ipma.pt/erddap/tabledap/erdGtsppBest.subset | https://erddap.ipma.pt/erddap/tabledap/erdGtsppBest | https://erddap.ipma.pt/erddap/tabledap/erdGtsppBest.graph | https://erddap.ipma.pt/erddap/files/erdGtsppBest/ | Global Temperature and Salinity Profile Programme (GTSPP) Data, 1985-present | The Global Temperature-Salinity Profile Programme (GTSPP) develops and maintains a global ocean temperature and salinity resource with data that are both up-to-date and of the highest quality. It is a joint World Meteorological Organization (WMO) and Intergovernmental Oceanographic Commission (IOC) program. It includes data from XBTs, CTDs, moored and drifting buoys, and PALACE floats. For information about organizations contributing data to GTSPP, see http://gosic.org/goos/GTSPP-data-flow.htm . The U.S. National Oceanographic Data Center (NODC) maintains the GTSPP Continuously Managed Data Base and releases new 'best-copy' data once per month.\n\nWARNING: This dataset has a *lot* of data. If you request too much data, your request will fail.\n* If you don't specify a longitude and latitude bounding box, don't request more than a month's data at a time.\n* If you do specify a longitude and latitude bounding box, you can request data for a proportionally longer time period.\nRequesting data for a specific station_id may be slow, but it works.\n\n*** This ERDDAP dataset has data for the entire world for all available times (currently, up to and including the May 2026 data) but is a subset of the original NODC 'best-copy' data. It only includes data where the quality flags indicate the data is 1=CORRECT, 2=PROBABLY GOOD, or 5=MODIFIED. It does not include some of the metadata, any of the history data, or any of the quality flag data of the original dataset. You can always get the complete, up-to-date dataset (and additional, near-real-time data) from the source: https://www.nodc.noaa.gov/GTSPP/ . Specific differences are:\n* Profiles with a position_quality_flag or a time_quality_flag other than 1|2|5 were removed.\n* Rows with a depth (z) value less than -0.4 or greater than 10000 or a z_variable_quality_flag other than 1|2|5 were removed.\n* Temperature values less than -4 or greater than 40 or with a temperature_quality_flag other than 1|2|5 were set to NaN.\n* Salinity values less than 0 or greater than 41 or with a salinity_quality_flag other than 1|2|5 were set to NaN.\n* Time values were converted from \"days since 1900-01-01 00:00:00\" to \"seconds since 1970-01-01T00:00:00\".\n\nSee the Quality Flag definitions on page 5 and \"Table 2.1: Global Impossible Parameter Values\" on page 61 of\nhttps://www.nodc.noaa.gov/GTSPP/document/qcmans/GTSPP_RT_QC_Manual_20090916.pdf .\nThe Quality Flag definitions are also at\nhttps://www.nodc.noaa.gov/GTSPP/document/qcmans/qcflags.htm .\n\ncdm_data_type = TrajectoryProfile\nVARIABLES:\ntrajectory (Trajectory ID)\n... (11 more variables)\n
| https://erddap.ipma.pt/erddap/metadata/fgdc/xml/erdGtsppBest_fgdc.xml | https://erddap.ipma.pt/erddap/metadata/iso19115/xml/erdGtsppBest_iso19115.xml | https://erddap.ipma.pt/erddap/info/erdGtsppBest/index.htmlTable | https://www.nodc.noaa.gov/GTSPP/
| https://erddap.ipma.pt/erddap/rss/erdGtsppBest.rss | https://erddap.ipma.pt/erddap/subscriptions/add.html?datasetID=erdGtsppBest&showErrors=false&email= | NOAA NODC | erdGtsppBest | ||
| https://erddap.ipma.pt/erddap/griddap/hawaii_d90f_20ee_c4cb | https://erddap.ipma.pt/erddap/griddap/hawaii_d90f_20ee_c4cb.graph | SODA - POP 2.2.4 Monthly Means, 1871-2010 (At Depths) | Simple Ocean Data Assimilation (SODA) version 2.2.4 - A reanalysis of ocean \nclimate. SODA uses the GFDL modular ocean model version 2.2. The model is \nforced by observed surface wind stresses from the COADS data set (from 1958 \nto 1992) and from NCEP (after 1992). Note that the wind stresses were \ndetrended before use due to inconsistencies with observed sea level pressure \ntrends. The model is also constrained by constant assimilation of observed \ntemperatures, salinities, and altimetry using an optimal data assimilation \ntechnique. The observed data comes from: 1) The World Ocean Atlas 1994 which \ncontains ocean temperatures and salinities from mechanical \nbathythermographs, expendable bathythermographs and conductivity-temperature-\ndepth probes. 2) The expendable bathythermograph archive 3) The TOGA-TAO \nthermistor array 4) The Soviet SECTIONS tropical program 5) Satellite \naltimetry from Geosat, ERS/1 and TOPEX/Poseidon. \nWe are now exploring an eddy-permitting reanalysis based on the Parallel \nOcean Program POP-1.4 model with 40 levels in the vertical and a 0.4x0.25 \ndegree displaced pole grid (25 km resolution in the western North \nAtlantic). The first version of this we will release is SODA1.2, a \nreanalysis driven by ERA-40 winds covering the period 1958-2001 (extended to \nthe current year using available altimetry).\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\ntemp (Sea Water Temperature, degree_C)\nsalt (Sea Water Practical Salinity, PSU)\nu (Eastward Sea Water Velocity, m s-1)\nv (Northward Sea Water Velocity, m s-1)\nw (Upward Sea Water Velocity, m s-1)\n | https://erddap.ipma.pt/erddap/metadata/fgdc/xml/hawaii_d90f_20ee_c4cb_fgdc.xml | https://erddap.ipma.pt/erddap/metadata/iso19115/xml/hawaii_d90f_20ee_c4cb_iso19115.xml | https://erddap.ipma.pt/erddap/info/hawaii_d90f_20ee_c4cb/index.htmlTable | https://www.atmos.umd.edu/~ocean/
| https://erddap.ipma.pt/erddap/rss/hawaii_d90f_20ee_c4cb.rss | https://erddap.ipma.pt/erddap/subscriptions/add.html?datasetID=hawaii_d90f_20ee_c4cb&showErrors=false&email= | TAMU/UMD | hawaii_d90f_20ee_c4cb | ||||
| https://erddap.ipma.pt/erddap/griddap/hawaii_d90f_20ee_c4cb_LonPM180 | https://erddap.ipma.pt/erddap/griddap/hawaii_d90f_20ee_c4cb_LonPM180.graph | https://erddap.ipma.pt/erddap/wms/hawaii_d90f_20ee_c4cb_LonPM180/request | SODA - POP 2.2.4 Monthly Means, 1871-2010 (At Depths), Lon+/-180 | Simple Ocean Data Assimilation (SODA) version 2.2.4 - A reanalysis of ocean \nclimate. SODA uses the GFDL modular ocean model version 2.2. The model is \nforced by observed surface wind stresses from the COADS data set (from 1958 \nto 1992) and from NCEP (after 1992). Note that the wind stresses were \ndetrended before use due to inconsistencies with observed sea level pressure \ntrends. The model is also constrained by constant assimilation of observed \ntemperatures, salinities, and altimetry using an optimal data assimilation \ntechnique. The observed data comes from: 1) The World Ocean Atlas 1994 which \ncontains ocean temperatures and salinities from mechanical \nbathythermographs, expendable bathythermographs and conductivity-temperature-\ndepth probes. 2) The expendable bathythermograph archive 3) The TOGA-TAO \nthermistor array 4) The Soviet SECTIONS tropical program 5) Satellite \naltimetry from Geosat, ERS/1 and TOPEX/Poseidon. \nWe are now exploring an eddy-permitting reanalysis based on the Parallel \nOcean Program POP-1.4 model with 40 levels in the vertical and a 0.4x0.25 \ndegree displaced pole grid (25 km resolution in the western North \nAtlantic). The first version of this we will release is SODA1.2, a \nreanalysis driven by ERA-40 winds covering the period 1958-2001 (extended to \nthe current year using available altimetry).\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\ntemp (Sea Water Temperature, degree_C)\nsalt (Sea Water Practical Salinity, PSU)\nu (Eastward Sea Water Velocity, m s-1)\nv (Northward Sea Water Velocity, m s-1)\nw (Upward Sea Water Velocity, m s-1)\n | https://erddap.ipma.pt/erddap/metadata/fgdc/xml/hawaii_d90f_20ee_c4cb_LonPM180_fgdc.xml | https://erddap.ipma.pt/erddap/metadata/iso19115/xml/hawaii_d90f_20ee_c4cb_LonPM180_iso19115.xml | https://erddap.ipma.pt/erddap/info/hawaii_d90f_20ee_c4cb_LonPM180/index.htmlTable | https://www.atmos.umd.edu/~ocean/
| https://erddap.ipma.pt/erddap/rss/hawaii_d90f_20ee_c4cb_LonPM180.rss | https://erddap.ipma.pt/erddap/subscriptions/add.html?datasetID=hawaii_d90f_20ee_c4cb_LonPM180&showErrors=false&email= | TAMU/UMD | hawaii_d90f_20ee_c4cb_LonPM180 | |||
| https://erddap.ipma.pt/erddap/tabledap/pmelTaoDyS.subset | https://erddap.ipma.pt/erddap/tabledap/pmelTaoDyS | https://erddap.ipma.pt/erddap/tabledap/pmelTaoDyS.graph | https://erddap.ipma.pt/erddap/files/pmelTaoDyS/ | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1987-present, Salinity | This dataset has daily Salinity data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nS_41 (Sea Water Practical Salinity, PSU)\nQS_5041 (Salinity Quality)\nSS_6041 (Salinity Source)\nSIC_8041 (Salinity Instrument Code)\n
| https://erddap.ipma.pt/erddap/metadata/fgdc/xml/pmelTaoDyS_fgdc.xml | https://erddap.ipma.pt/erddap/metadata/iso19115/xml/pmelTaoDyS_iso19115.xml | https://erddap.ipma.pt/erddap/info/pmelTaoDyS/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://erddap.ipma.pt/erddap/rss/pmelTaoDyS.rss | https://erddap.ipma.pt/erddap/subscriptions/add.html?datasetID=pmelTaoDyS&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyS | ||
| https://erddap.ipma.pt/erddap/tabledap/pmelTaoDySss.subset | https://erddap.ipma.pt/erddap/tabledap/pmelTaoDySss | https://erddap.ipma.pt/erddap/tabledap/pmelTaoDySss.graph | https://erddap.ipma.pt/erddap/files/pmelTaoDySss/ | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1992-present, Sea Surface Salinity | This dataset has daily Sea Surface Salinity data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nS_41 (Sea Water Practical Salinity, PSU)\nQS_5041 (Salinity Quality)\nSS_6041 (Salinity Source)\nSIC_7041 (Salinity Instrument Code)\n
| https://erddap.ipma.pt/erddap/metadata/fgdc/xml/pmelTaoDySss_fgdc.xml | https://erddap.ipma.pt/erddap/metadata/iso19115/xml/pmelTaoDySss_iso19115.xml | https://erddap.ipma.pt/erddap/info/pmelTaoDySss/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://erddap.ipma.pt/erddap/rss/pmelTaoDySss.rss | https://erddap.ipma.pt/erddap/subscriptions/add.html?datasetID=pmelTaoDySss&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDySss |