Terrestrial Water Storage Anomalies

300 km
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Mean TWS (cm)
--
Trend (cm/yr)
--
Seasonal Amp. (cm)
--
Uncertainty (cm)

Groundwater Depletion Monitoring

California Central Valley

Intensive agricultural pumping

-2.1 cm/yr

Northwest India

Groundwater irrigation

-3.5 cm/yr

Middle East

Fossil aquifer mining

-1.8 cm/yr

Ogallala Aquifer

US Great Plains

-1.2 cm/yr
-2.1
GW Trend (cm/yr)
-15.2
Total Loss (km³)
--
Recovery Rate
95%
Confidence

Groundwater Isolation

GRACE TWS = Groundwater + Soil Moisture + Surface Water + Snow. GW is isolated by subtracting model estimates of other components (GLDAS, CLM).

Limitations

~300 km spatial resolution limits detection of local depletion. Separation uncertainty from hydrological models can reach 20-30% of signal.

Ice Sheet Mass Balance

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Mass Rate (Gt/yr)
--
SLR Contrib. (mm/yr)
--
Total Loss (Gt)
--
Acceleration

GRACE Ice Mass

Gravity changes over ice sheets directly measure mass changes. Must correct for post-glacial rebound (GIA) which causes apparent mass gain.

Sea Level Rise

1 Gt of ice = 0.0028 mm global sea level rise. Greenland and Antarctica together contribute ~1 mm/yr to global sea level.

Drought Monitoring

2022
--
Drought Area (%)
--
Severity Index
--
Duration (months)
--
Recovery Forecast

GRACE-DSI

Drought Severity Index derived from GRACE TWS anomalies normalized by historical variability. Provides integrated measure of total water deficit.

Advantages over SPI/PDSI

GRACE captures total column water storage including groundwater, providing earlier drought detection and more complete assessment than precipitation-only indices.

Operational Use

GRACE data assimilated into land surface models (NASA LIS) for operational drought monitoring by USDA and international agencies.