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Home — Metadata: GRACE LWE

Metadata

GRACE LWE
References
official web page https://grace.jpl.nasa.gov https://podaac.jpl.nasa.gov
Climate Explorer URLclimexp.knmi.nl/select.cgi?grace_all
Climate Explorer filenameGRACEData/grace_all.nc
Variable
namelwe_thickness
unitscm
long_nameLiquid_Water_Equivalent_Thickness
standard_nameLiquid_Water_Equivalent_Thickness
Netcdf global metadata
CDIClimate Data Interface version 1.9.10 (mpimet.mpg.de/cdi)
ConventionsCF-1.6, ACDD-1.3, ISO 8601
sourceGRACE and GRACE-FO JPL RL06Mv2-CRI
institutionNASA/JPL
Metadata_ConventionsUnidata Dataset Discovery v1.0
standard_name_vocabularyNetCDF Climate and Forecast (CF) Metadata Convention-1.6
titleJPL GRACE and GRACE-FO MASCON RL06Mv2 CRI
summaryMonthly gravity solutions from GRACE and GRACE-FO as determined from the JPL RL06Mv2 mascon solution - with CRI filter applied
keywordsSolid Earth, Geodetics/Gravity, Gravity, liquid_water_equivalent_thickness
keywords_vocabularyNASA Global Change Master Directory (GCMD) Science Keywords
platformGRACE and GRACE-FO
creator_nameDavid Wiese
creator_emailgrace@podaac.jpl.nasa.gov
creator_urlgrace.jpl.nasa.gov
creator_typegroup
creator_institutionNASA/JPL
publisher_namePhysical Oceanography Distributed Active Archive Center
publisher_emailpodaac@jpl.nasa.gov
publisher_urlpodaac.jpl.nasa.gov
publisher_typegroup
publisher_institutionNASA/JPL
projectNASA Gravity Recovery and Climate Experiment (GRACE) and NASA Gravity Recovery and Climate Experiment Follow-On (GRACE-FO)
programNASA Earth Science System Pathfinder and NASA Earth Systematic Missions Program
id10.5067/TEMSC-3JC62
naming_authorityorg.doi.dx
processing_level2 and 3
acknowledgementGRACE is a joint mission of NASA (USA) and DLR (Germany). GRACE-FO is a joint mission of NASA (USA) and the German Research Center for Geosciences (GFZ). Use the digital object identifier provided in the id attribute when citing this data. See podaac.jpl.nasa.gov/CitingPODAAC
licensescience.nasa.gov/earth-science/earth-science-data/data-information-policy
product_versionv2.0
time_epoch2002-01-01T00:00:00Z
time_coverage_start2002-04-16T00:00:00Z
time_coverage_end2021-07-16T23:59:59Z
geospatial_lat_min-89.75
geospatial_lat_max89.75
geospatial_lat_unitsdegrees_north
geospatial_lat_resolution0.5 degree grid; however the native resolution of the data is 3-degree equal-area mascons
geospatial_lon_min0.25
geospatial_lon_max359.75
geospatial_lon_unitsdegrees_east
geospatial_lon_resolution0.5 degree grid; however the native resolution of the data is 3-degree equal-area mascons
time_mean_removed2004.000 to 2009.999
months_missing2002-06;2002-07;2003-06;2011-01;2011-06;2012-05;2012-10;2013-03;2013-08;2013-09;2014-02;2014-07;2014-12;2015-06;2015-10;2015-11;2016-04;2016-09;2016-10;2017-02;2017-07;2017-08;2017-09;2017-10;2017-11;2017-12;2018-01;2018-02;2018-03;2018-04;2018-05;2018-08-2018-09
postprocess_1 OCEAN_ATMOSPHERE_DEALIAS_MODEL (GAD), MONTHLY_AVE, ADDED BACK TO OCEAN PIXELS ONLY
postprocess_2Water density used to convert to equivalent water height: 1000 kg/m^3
postprocess_3Coastline Resolution Improvement (CRI) filter has been applied to separate land/ocean mass within mascons that span coastlines
GIA_removedICE6G-D; Peltier, W. R., D. F. Argus, and R. Drummond (2018) Comment on the paper by Purcell et al. 2016 entitled An assessment of ICE-6G_C (VM5a) glacial isostatic adjustment model, J. Geophys. Res. Solid Earth, 122.
geocenter_correctionWe use a version of TN-13 based on the JPL mascons
C_20_substitutionTN-14; Loomis et al., 2019, Geophys. Res. Lett., doi:10.1029/2019GL082929
C_30_substitutionTN-14; Loomis et al., 2019, Geophys. Res. Lett., doi:10.1029/2019GL082929. This substitution is made for all months after August 2016.
user_note_1The accelerometer on the GRACE-B spacecraft was turned off after August 2016. After this date, the accelerometer on GRACE-A was used to derive the non-gravitational accelerations acting on GRACE-B using a transplant procedure. This has led to a subsequent degradation in the quality of the gravity fields derived. The uncertainties in this file have been scaled to accomodate this degradation.
user_note_2The accelerometer on the GRACE-D spacecraft began performing sub-optimally after June 21, 2018. After this date, the accelerometer on GRACE-C is used to derive the non-gravitational accelerations acting on GRACE-D using a transplant procedure. The uncertainties in the file have been scaled to accomodate this degradation using the current best state of knowledge.
journal_referenceWatkins, M. M., D. N. Wiese, D.-N. Yuan, C. Boening, and F. W. Landerer (2015) Improved methods for observing Earth\'s time variable mass distribution with GRACE using spherical cap mascons, J. Geophys. Res., 120, doi:10.1002/2014JB011547.
CRI_filter_journal_referenceWiese, D. N., F. W. Landerer, and M. M. Watkins (2016) Quantifying and reducing leakage errors in the JPL RL05M GRACE mascon solution, Water Resour. Res., 52, doi:10.1002/2016WR019344.
date_created2021-09-01T16:09:15Z
historyMon Oct 04 10:12:02 2021: cdo mul grace_all_tmp1.nc scalefactor.nc grace_all.nc
Mon Oct 04 10:11:50 2021: cdo settaxis,2002-04-15,0:00,1mon grace_all_tmp0.nc grace_all_tmp1.nc
Mon Oct 4 10:11:39 2021: ncks -O -v lwe_thickness GRCTellus.JPL.200204_202107.GLO.RL06M.MSCNv02CRI.nc grace_all_tmp0.nc
NCO = netCDF Operators version 4.9.3 (Homepage = nco.sf.net, Codehttp://github.com/nco/nco)
CDOClimate Data Operators version 1.9.10 (mpimet.mpg.de/cdo)
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