How land slowly rebounds after ancient ice sheets (GRACE)
What it measures. Maps the slow, ongoing rebound of Earth's crust as it continues rising after the heavy ice sheets of the last ice age melted away—a steady geophysical drift, not a weather signal.
How it's made. A modeled correction product, gridded to half-degree resolution and filtered to match the processing of GRACE and GRACE-FO gravity-satellite data.
How & where you'd use it. Scientists subtract this from satellite gravity measurements so that present-day changes—like melting glaciers and groundwater loss—stand out clearly rather than being masked by the ancient rebound signal.
What's measured
Coverage & cadence
- Time span1900-01-01 → 2100-12-31
- Measured byGRACE
- Processing levelLevel 3
- Spatial extent-180, -90, 180, 90
- FormatsNETCDF
- StatusCOMPLETE
What you can do with it
- Measure ground motion and subsidence (InSAR)
- Track earthquakes, volcanoes and landslides
- Map elevation and terrain change
Official 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.
Get the data
import earthaccess
earthaccess.login(strategy="netrc") # free Earthdata Login
results = earthaccess.search_data(
short_name="TELLUS_GIA_L3_0.5-DEG_V1.0",
version="1.0",
bounding_box=(-122.5, 37.2, -121.8, 37.9), # your area (W,S,E,N)
temporal=("2024-01-01", "2024-12-31"), # your dates
)
files = earthaccess.open(results) # stream straight from POCLOUD Browsing CMR needs no login. Downloading or streaming bytes needs a free Earthdata Login + the earthaccess package. Official links
- Data Use and Citation Guidelines VIEW RELATED INFORMATION
- Comment on the paper by Purcell et al. 2016 entitled An assessment of ICE-6G_C (VM5a) glacial isostatic adjustment model VIEW RELATED INFORMATION
- Generic Data Readers VIEW RELATED INFORMATION
- GRACE Project VIEW RELATED INFORMATION
- PODAAC GRACE Mission-Page VIEW RELATED INFORMATION
- GIA model statistics for GRACE hydrology VIEW RELATED INFORMATION
- Glacial Isostatic Adjustment (GIA) VIEW RELATED INFORMATION
- Computations of the viscoelastic response of a 3-D compressible Earth to surface loading: an application to Glacial Isostatic Adjustment in Antarctica and Canada VIEW RELATED INFORMATION