2024-03-28T13:43:08.449Zhttps://cmr.earthdata.nasa.gov/opensearch/collections.atomCMRechodev@echo.nasa.govECHO dataset metadataSearch parameters: satellite => NOAA-6 boundingBox => startTime => endTime => 381021https://cmr.earthdata.nasa.gov/opensearch/collections.atom?uid=C2586786218-POCLOUDCMRechodev@echo.nasa.govGEOSSEOSDISGHRSST Level 4 OSTIA Global Historical Reprocessed Foundation Sea Surface Temperature Analysis produced by the UK Meteorological OfficeThe Operational Sea Surface Temperature and Sea Ice Analysis Reprocessed (OSTIA-REP) is a GHRSST reprocessed Level-4 sea surface temperature and ice-concentration analysis produced by the UK Met Office (UKMO) using optimal interpolation (OI) on a global 0.05 degree grid. It is a sister product of the Near Real Time version (OSTIA-NRT), but incorporates satellite data from over 25 different SST sensors as well as in situ data from drifting and moored buoys. The OSTIA-REP is produced on a biannual frequency when more satellite and climatology observations are available from existing geostationary IR, and polar orbiting IR and MW satellites in addition to the data used in OSTIA-NRT. <br><br>
While OSTIA-NRT is produced to mainly serve as a lower boundary condition in Numerical Weather Prediction (NWP) models, this OSTIA-REP aims to provide a more accurate and consistent record of SST measurements over time, which is crucial for detecting long-term climate trends and variability. Both versions follow GHRSST Data Processing Specification (GDS) version 2 format guidelines.<br><br>
Data to June 2022 are also distributed through the E.U. Copernicus Marine Service Information (https://marine.copernicus.eu/, DOI: https://doi.org/10.48670/moi-00168 with the following license). Please refer to the user guide for more information. 2017-04-28T05:01:46.000ZC2586786218-POCLOUD1982-01-01T00:00:00.000Z/GHRSST Level 4 OSTIA Global Historical Reprocessed Foundation Sea Surface Temperature Analysis produced by the UK Meteorological OfficeOSTIA-UKMO-L4-GLOB-REP-v2.02.0POCLOUDNASA/JPL/PODAACNASA/JPL/PODAACUK/MOD/MET4CARTESIAN-90 -180 90 180truetruetruefalsetruetruetruetrue0.65gov.nasa.eosdistruehttps://cmr.earthdata.nasa.gov/opensearch/collections.atom?uid=C1261530310-GES_DISCCMRechodev@echo.nasa.govGEOSSEOSDISMSU Ch 2/3 Daily Lower Troposphere Temps with Limb93 Correction L3 1 day 2.5 degree x 2.5 degree V001 (MSULTT) at GES DISCThe Microwave Sounding Unit (MSU) Lower Troposphere Deep Layer Temperature product (MSULTT) provides gridded lower tropospheric temperatures derived from MSU instruments on several different platforms. The temperatures are derived using a combination of MSU
channels 2 and 3 which has an averaging kernel that peaks near 500 hecto Pascals. The algorithm is based on Spencer and Christy (1990) with the LIMB 93 limb
correction based on latitude, longitude, month, and scan angle. The MSU instruments measure the thermal emission of radiation by molecular oxygen at four frequencies near 60 GHz. North (south) of 66.7N (S) the footprint data are assigned to grid boxes in a
weighted method depending on footprint latitude. Horizontal averaging is used1970-01-01T00:00:00.000ZC1261530310-GES_DISC1979-01-01T00:00:00.000Z/1994-12-31T23:59:59.999ZMSU Ch 2/3 Daily Lower Troposphere Temps with Limb93 Correction L3 1 day 2.5 degree x 2.5 degree V001 (MSULTT) at GES DISCMSULTT001GES_DISCNASA/GSFC/SED/ESD/GCDC/GESDISCNASA/GSFC/SED/ESD/GCDC/GESDISC3CARTESIAN-89 -180 89 180truefalsefalsefalsefalsefalsefalsefalse0.65org.ceos.wgiss.cwic.granules.provider"NASA"org.ceos.wgiss.cwic.granules.native_id"MSU Ch 2/3 Daily Lower Troposphere Temps with Limb93 Correction L3 1 day 2.5 degree x 2.5 degree V001 (MSULTT) at GES DISC"org.ceos.wgiss.cwic.granules.prodorg.geoss.geoss_data-coregov.nasa.eosdistruetruehttps://cmr.earthdata.nasa.gov/opensearch/collections.atom?uid=C1261530423-GES_DISCCMRechodev@echo.nasa.govGEOSSEOSDISMSU Ch 3/4 Daily Upper Troposphere Temps with Limb93 Correction V001 L3 1 day 2.5 degree x 2.5 degree (MSUUTT) at GES DISCThe Microwave Sounding Unit (MSU) Upper Troposphere Temperature product (MSUUTT) provides gridded upper tropospheric temperatures derived from MSU instruments on several different platforms. The temperatures are derived using a combination of MSU channels 3 and 4 which has an averaging kernel that peaks near 250 hecto Pascals. The algorithm is based on Spencer and Christy (1990) with the LIMB 93 limb correction based on latitude, longitude, month, and scan angle. The MSU instruments measure the thermal emission of radiation by molecular oxygen at four frequencies near 60 GHz. North (south) of 66.7N (S) the footprint data are assigned to grid boxes in a weighted method depending on footprint latitude. Horizontal averaging is used to fill some of the empty grid boxes.1970-01-01T00:00:00.000ZC1261530423-GES_DISC1979-01-01T00:00:00.000Z/1994-12-31T23:59:59.999ZMSU Ch 3/4 Daily Upper Troposphere Temps with Limb93 Correction V001 L3 1 day 2.5 degree x 2.5 degree (MSUUTT) at GES DISCMSUUTT001GES_DISCNASA/GSFC/SED/ESD/GCDC/GESDISCNASA/GSFC/SED/ESD/GCDC/GESDISC3CARTESIAN-30 -180 30 180truefalsefalsefalsefalsefalsefalsefalse0.65org.ceos.wgiss.cwic.granules.provider"NASA"org.ceos.wgiss.cwic.granules.native_id"MSU Ch 3/4 Daily Upper Troposphere Temps with Limb93 Correction V001 L3 1 day 2.5 degree x 2.5 degree (MSUUTT) at GES DISC"org.ceos.wgiss.cwic.granules.prodorg.geoss.geoss_data-coregov.nasa.eosdistruetruehttps://cmr.earthdata.nasa.gov/opensearch/collections.atom?uid=C1261530244-GES_DISCCMRechodev@echo.nasa.govGEOSSEOSDISMSU Ch 4 Daily Lower Stratosphere Temps with Limb93 Correction L3 1 day 2.5 degree x 2.5 degree V001 (MSULST) at GES DISCThe Microwave Sounding Unit (MSU) Lower Stratosphere Deep Layer Mean Temperature product (MSULST) provides gridded lower stratospheric temperatures for each day derived from MSU instruments on several different platforms. The temperatures are derived from MSU channel 4 using the method of Spencer and Christy (1990) with the LIMB 93 limb correction based on latitude, longitude, month, and scan angle. The MSU instruments measure the thermal emission of radiation by molecular oxygen at four frequencies near 60 GHz. North (south) of 66.7N (S) the footprint data are assigned to grid boxes in a weighted method depending on footprint latitude. Horizontal averaging is used
to fill some of the empty grid boxes.1970-01-01T00:00:00.000ZC1261530244-GES_DISC1979-01-01T00:00:00.000Z/1994-12-31T23:59:59.999ZMSU Ch 4 Daily Lower Stratosphere Temps with Limb93 Correction L3 1 day 2.5 degree x 2.5 degree V001 (MSULST) at GES DISCMSULST001GES_DISCNASA/GSFC/SED/ESD/GCDC/GESDISCNASA/GSFC/SED/ESD/GCDC/GESDISC3CARTESIAN-90 -180 90 180truefalsefalsefalsefalsefalsefalsefalse0.65org.ceos.wgiss.cwic.granules.provider"NASA"org.ceos.wgiss.cwic.granules.native_id"MSU Ch 4 Daily Lower Stratosphere Temps with Limb93 Correction L3 1 day 2.5 degree x 2.5 degree V001 (MSULST) at GES DISC"org.ceos.wgiss.cwic.granules.prodorg.geoss.geoss_data-coregov.nasa.eosdistruetruehttps://cmr.earthdata.nasa.gov/opensearch/collections.atom?uid=C1261530370-GES_DISCCMRechodev@echo.nasa.govGEOSSEOSDISMSU Daily Oceanic Precipitation with Limb93 Correction L3 1 day 2.5 degree x 2.5 degree V001 (MSUOP) at GES DISCThe Microwave Sounding Unit (MSU) Ocean Precipitation product (MSUOP) provides gridded upper tropospheric temperatures derived from MSU instruments on several different platforms. The precipitation estimates follow the method of Spencer (1993). Oceanic precipitation is estimated by increased warming in MSU channel 1 over a threshold. The increased warming is attributable to emission by liquid water in the lower troposphere. MSU channels 2 and 3 are used to remove warming due to air mass differences. The MSU instruments measure the thermal emission of radiation by molecular oxygen at four frequencies near 60 GHz.1970-01-01T00:00:00.000ZC1261530370-GES_DISC1979-01-01T00:00:00.000Z/1994-12-31T23:59:59.999ZMSU Daily Oceanic Precipitation with Limb93 Correction L3 1 day 2.5 degree x 2.5 degree V001 (MSUOP) at GES DISCMSUOP001GES_DISCNASA/GSFC/SED/ESD/GCDC/GESDISCNASA/GSFC/SED/ESD/GCDC/GESDISC3CARTESIAN-60 -180 60 180truefalsefalsefalsefalsefalsefalsefalse0.65org.ceos.wgiss.cwic.granules.provider"NASA"org.ceos.wgiss.cwic.granules.native_id"MSU Daily Oceanic Precipitation with Limb93 Correction L3 1 day 2.5 degree x 2.5 degree V001 (MSUOP) at GES DISC"org.geoss.geoss_data-coregov.nasa.eosdisorg.ceos.wgiss.cwic.granules.prodtruetruehttps://cmr.earthdata.nasa.gov/opensearch/collections.atom?uid=C2107093304-NOAA_NCEICMRechodev@echo.nasa.govCEOSNOAA Climate Data Record (CDR) of MSU and AMSU-A Mean Layer Temperatures, UAH Version 5.4 (Superseded)*Please note: this dataset has been superseded by a newer version (see below). This version is archived offline by NOAA NCEI.* This Climate Data Record (CDR) includes lower tropospheric, mid-tropospheric, and lower stratospheric temperatures over land and ocean derived from microwave radiometers on NOAA and NASA polar orbiting satellites. The temperatures are from measurements produced by Microwave Sounding Units (MSU) since 1978 and Advanced Microwave Sounding Unit-A (AMSU-A) since 1998 flying on NOAA polar orbiting satellites, on NASA Aqua satellite (operating since mid-1998) and on the European MetOp satellite (operating since late 2006). The instruments are cross-track through-nadir scanning externally-calibrated passive microwave radiometers. Brightness temperature measurements are derived at microwave frequencies within the 50-60 GHz oxygen absorption complex, and (in the case of AMSU-A) at a few microwave frequencies above and below that absorption complex. There are three atmospheric layers for which intermediate products are processed: (1) lower-tropospheric (TLT) deep-layer average temperature, computed as a weighted difference between view angles of AMSU-A channel 5, whose heritage comes from MSU channel 2, (2) mid-tropospheric (TMT) deep-layer temperature, computed as an average of the central portion of the scan of AMSU-A channel 5, whose heritage also comes from MSU channel 2, and (3) lower-stratospheric (TLS) deep layer temperatures, computed from the central portion of the scan of AMSU channel 9, whose heritage comes from MSU channel 4. This CDR includes several products. The global monthly anomaly data data are averaged onto a 2.5 x 2.5 degree latitude-longitude grid for each of the three atmospheric layers. Monthly anomalies are averaged for each of the three atmospheric layers over multiple regions, including Global, hemispheric, tropic, extratropic, polar and contiguous U.S. A mean annual cycle of monthly mean layer temperatures is also included. Anomalies are deviations from 1981-2010 mean. The datasets have been converted from the native ASCII format to CF-compliant netCDF-4 format.C2107093304-NOAA_NCEI1978-12-01T00:00:00.000Z/2010-12-01T00:00:00.000ZNOAA Climate Data Record (CDR) of MSU and AMSU-A Mean Layer Temperatures, UAH Version 5.4 (Superseded)NCEI DSI 3688_01Version 5.4NOAA_NCEIDOC/NOAA/NESDIS/NCEICARTESIAN-90 -180 90 180falsefalsefalsefalsefalsefalsefalsefalse0.65https://cmr.earthdata.nasa.gov/opensearch/collections.atom?uid=C2107093828-NOAA_NCEICMRechodev@echo.nasa.govCEOSNOAA Climate Data Record (CDR) of MSU and AMSU-A Mean Layer Temperatures, UAH Version 6.0This dataset includes monthly gridded temperature anomalies on a global 2.5 x 2.5 degree grid derived from Microwave Sounding Unit (MSU) and Advanced Microwave Sounding Unit (AMSU) radiance data since December 1978. In addition, there are monthly regional anomalies and monthly mean annual cycle temperatures. All products are derived for four bulk layers of the atmosphere: the Lower Troposphere (TLT), Mid-Troposphere (TMT), Tropopause (TTP) and Lower Stratosphere (TLS). Version 6.0 is the latest UAH version archived at NOAA and is updated monthly. It utilizes the linear calibration equation with hot-target correction for the MSU series (TIROS-N through NOAA-14) rather than other non-linear calibration equations. Gridded values of absolute temperature are calculated from a polynomial fit in the vertical coordinate of all view angle temperatures binned into each grid over a month. The selected temperature is calculated from a prescribed view-angle where it intersects the polynomial fit of the temperature vs. view-angle relationship or each grid. The diurnal adjustment is completely empirical, calculated by comparing a diurnally-drifting spacecraft against one that is not drifting during their overlap comparison period (for a.m. spacecraft, NOAA-15 vs. (non-drifting) AQUA, and for p.m., NOAA-18 vs. (non-drifting) NOAA-19 during 4 years). The calculated diurnal relationship of temperature change vs. time of day is then applied to all drifting satellites. The Lower Troposphere is calculated from a linear combination of TMT, TTP and TLS rather than from a linear combination of view-angles from the single channel (MSU2 or AMSU5) as was done in versions 5.6 and earlier. A new bulk layer centered on the Tropopause was added in version 6.0. These products were converted from the native text file format to netCDF-4 following CF metadata conventions, and they are accompanied by algorithm documentation, data flow diagram and source code for the NOAA CDR Program.C2107093828-NOAA_NCEI1978-12-01T00:00:00.000Z/NOAA Climate Data Record (CDR) of MSU and AMSU-A Mean Layer Temperatures, UAH Version 6.0doi:10.7289/V5MC8X31Version 6.0NOAA_NCEIDOC/NOAA/NESDIS/NCEIEarth System Science Center, University of Alabama in HuntsvilleCARTESIAN-90 -180 90 180falsefalsefalsefalsefalsefalsefalsefalse0.65https://cmr.earthdata.nasa.gov/opensearch/collections.atom?uid=C2231553312-CEOS_EXTRACMRechodev@echo.nasa.govCEOSNOAA Digital AVHRR Satellite Data; USGS, AlaskaThis digital data set contains selected NOAA 6, 7, 8 and 9
Advanced Very High Resolution Radiometer (AVHRR) imagery of
Alaska; AVHRR is carried on NOAA's polar orbiting satellites.
Spatial referencing is 1.1 km at nadir. Data source is National
Oceanic and Atmospheric Administration (NOAA). The data set
includes 47 records with estimated growth rate of 100 records per
year. Storage required varies by storage medium and selected
scene. The file structure is sequential. Data are available
on 9-track, 800 bpi, 1600 bpi, 6250 bpi, unlabeled, unblocked,
BCD, fixed record length tape. Subsets and customs formats are
available. Limited documentation is available. Data is organized
by 7 1/2 ' or 15 ' quads. Uses include fuel mapping, vegetation
monitoring, large area mosaic, and monitoring of ice/snow dynamics.C2231553312-CEOS_EXTRA1984-01-01T00:00:00.000Z/NOAA Digital AVHRR Satellite Data; USGS, AlaskaEARTH_LAND_USGS_AK_NOAA_AVHRRNot providedCEOS_EXTRADOI/USGS/GEOG/WRGDOI/USGS/GEOG/WRGCARTESIAN52 170 72 -130falsefalsefalsefalsefalsefalsefalsefalse0.65https://cmr.earthdata.nasa.gov/opensearch/collections.atom?uid=C1214607960-SCIOPSCMRechodev@echo.nasa.govNRSC European Mosaic created from AVHRR ImagesNOAA AVHRR cloud-free summer images from 1979 to 1985 (NOAA 6-9) in
channels 1, 2 and 4 with a resolution of 1.1km were used to construct
this mosaic. The categories of major vegetation, from polar through
subtropical to desert, are visible. This mosaic is often used as a
backdrop for other projects.
The processed mosaic is available as a digital product on CCT, Exabyte
or CD-ROM, or as positive or negative photographic products. A poster
is also available. The products and current price lists may be
obtained from the National Remote Sensing Centre (NRSC).C1214607960-SCIOPS1979-06-27T00:00:00.000Z/1985-05-22T23:59:59.999ZNRSC European Mosaic created from AVHRR ImagesUK-NRSC-SAT-2008Not providedSCIOPSINFOTERRAINFOTERRACARTESIAN25 -25 70 40falsefalsefalsefalsefalsefalsefalsefalse0.65https://cmr.earthdata.nasa.gov/opensearch/collections.atom?uid=C1214585542-SCIOPSCMRechodev@echo.nasa.govPolar Orbiting and Geostationary Satellite Data from Dundee University via WWWThe National Environment Research Council (NERC) Satellite Station at Dundee
University (UK) server address on the WWW is 'http://www.sat.dundee.ac.uk/'.
The Natural Environment Research Council, established by Royal Charter in 1965,
has responsibility for planning, encouraging and carrying out research in the
physical and biological sciences which explain the natural processes of the
environment.
The NERC satellite station at Dundee University has been systematically
recording HRPT data from NOAA satellites on a daily basis since the launch of
the prototype 3rd generation NOAA satellite TIROS-N in October 1978. It also
recorded data from the CZCS on NIMBUS-7 between August 1979 and the end of the
mission in December 1986. SeaWiFS, NIMBUS-7's replacement was launched on 1st
August 1997 and Dundee is receiving and archiving this data. MODIS data from
EOS AM/PM satellites (Terra, Aqua) will also be archived.
HRPT data is stored on magnetic tape and optical disk and is available from
Dundee for all NOAA satellite passes from 1978 onwards. Formats include raw
data on exabytes and CD-ROMs, processed images, high quality enhanced
photographic enlargments, photographic browse files etc. Data is also available
over the network from the web site.
The quicklook archive contains sampled images from every NOAA satellite pass
received at Dundee. The images are sampled to contain the complete pass in
each of the 5 AVHRR channels plus a Normalized Difference Vegetation Index. The
images are also corrected for earth curvature and have a grid overlay showing
coastlines and latitude/longitude lines. Browsing the archive to search for
specific areas or features is made easier with access to our database of all
passes we have received. Thumbnail images allow those with slow network
connections to view a series of small images for quick comparisons or when
searching for major features.C1214585542-SCIOPS1978-01-01T00:00:00.000Z/Polar Orbiting and Geostationary Satellite Data from Dundee University via WWWDUNDEE_UKNot providedSCIOPSUK/NERC/DSRSUK/NERC/DSRSCARTESIAN20 -100 80 90falsefalsefalsefalsefalsefalsefalsefalse0.65