N: 90 S: -90 E: 180 W: -180
Description
Glacial isostatic adjustment (GIA) is an ongoing geophysical process and is measured by gravimetry satellites like GRACE and GRACE-FO. To isolate signals of contemporary surface mass loss in the cumulative satellite gravimetry measurements, contemporary GIA rates are computed and subtracted from the satellite gravimetry observations. The GIA correction models provided here are filtered such that they are compatible with Level-3 post-processing filters applied to GRACE(-FO) data as indicated in the [product_id]. In this way, user can effectively assess the impact of the applied GIA correction, and substitute different GIA models should that be desired. This GIA dataset is mapped into 0.5-degree global grid compatible with the JPL Mascon solution, provided in netCDF format.
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Citation
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Variables
The table below lists the variables contained within a single granule for this dataset. Variables often contain observed or derived geophysical measurements collected from a variety of sources, including remote sensing instruments on satellite and airborne platforms, field campaigns, in situ measurements, and model outputs. The terms variable, parameter, scientific data set, layer, and band have been used across NASA’s Earth science disciplines; however, variable is the designated nomenclature in NASA’s Common Metadata Repository (CMR). Variable metadata attributes such as Name, Description, Units, Data Type, Fill Value, Valid Range, and Scale Factor allow users to efficiently process and analyze the data. The full range of attributes may not be applicable to all variables. Additional information on variable attributes is typically available in the data, user guide, and/or other product documentation.
For questions on a specific variable, please use the Earthdata Forum.
| Name Sort descending | Description | Units | Data Type | Fill Value | Valid Range | Scale Factor | Offset |
|---|---|---|---|---|---|---|---|
| GIA_geoid_rate_3degJPL_MSCN | GIA geoid rate and uplift rate coefficients for a compressible Earth,computed (by Geruo A) using the ICE5G ice history and VM2 viscosity profile. The normalization of the harmonics, for both the geoid rate and the uplift rate,is the conventional normalization used for the Stokes coefficients of the geoid.From: A, G., J. Wahr, and S. Zhong,"Computations of the viscoelastic response of a 3-D compressible Earth to surface loading: an application to Glacial Isostatic Adjustment in Antarctica and Canada", submitted to Geophys. J. Int. | m/year | double | -99999 | -0.0003 to 0.002 | 1 | N/A |
| GIA_mass_rate_3degJPL_MSCN | GIA geoid rate and uplift rate coefficients for a compressible Earth,computed (by Geruo A) using the ICE5G ice history and VM2 viscosity profile. The normalization of the harmonics, for both the geoid rate and the uplift rate,is the conventional normalization used for the Stokes coefficients of the geoid.From: A, G., J. Wahr, and S. Zhong,"Computations of the viscoelastic response of a 3-D compressible Earth to surface loading: an application to Glacial Isostatic Adjustment in Antarctica and Canada", submitted to Geophys. J. Int. | m/year | double | -99999 | -0.02 to 0.06 | 1 | N/A |
| lat | latitude value at each pixel | degrees_north | double | N/A | -89.75 to 89.75 | 1 | N/A |
| lat_bounds | latitude values at the north and south bounds of each pixel | degrees_north | double | N/A | N/A | 1 | N/A |
| lon | longitude value at each pixel | degrees_east | double | N/A | 0.25 to 359.75 | 1 | N/A |
| lon_bounds | longitude values at the west and east bounds of each pixel | degrees_east | double | N/A | N/A | 1 | N/A |