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Accuracy of scaled GRACE terrestrial water storage estimates
Abstract
We assess the accuracy of global‐gridded terrestrial water storage (TWS) estimates derived from temporal gravity field variations observed by the Gravity Recovery and Climate Experiment (GRACE) satellites. The TWS data set has been corrected for signal modification due to filtering and truncation. Simulations of terrestrial water storage variations from land‐hydrology models are used to infer relationships between regional time series representing different spatial scales. These relationships, which are independent of the actual GRACE data, are used to extrapolate the GRACE TWS estimates from their effective spatial resolution (length scales of a few hundred kilometers) to finer spatial scales (∼100 km). Gridded, scaled data like these enable users who lack expertise in processing and filtering the standard GRACE spherical harmonic geopotential coefficients to estimate the time series of TWS over arbitrarily shaped regions. In addition, we provide gridded fields of leakage and GRACE measurement errors that allow users to rigorously estimate the associated regional TWS uncertainties. These fields are available for download from the GRACE project website (available at http://grace.jpl.nasa.gov ). Three scaling relationships are examined: a single gain factor based on regionally averaged time series, spatially distributed (i.e., gridded) gain factors based on time series at each grid point, and gridded‐gain factors estimated as a function of temporal frequency. While regional gain factors have typically been used in previously published studies, we find that comparable accuracies can be obtained from scaled time series based on gridded gain factors. In regions where different temporal modes of TWS variability have significantly different spatial scales, gain factors based on the first two methods may reduce the accuracy of the scaled time series. In these cases, gain factors estimated separately as a function of frequency may be necessary to achieve accurate results.
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“These measurements can be used to detect changes in the distribution of water across the planet and estimate terrestrial water storage (Landerer and Swenson, 2012).”
From AlphaEarth Foundations: An embedding field model for accurate and efficient global mapping from sparse label data (2025) · cites this paper as Landerer and Swenson, 2012
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Research works printed but not linked: 22
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“As described in Landerer and Swenson (2012), the gain factors derived from the model outputs used to scale the GRACE data are intended to reduce small errors in the GRACE data from signal modification (e.g., attenuation).”
Method
Metadata
- Authors
- Landerer, F. W., & Swenson, S. C.
- Venue
- Water Resources Research
- Publisher
- American Geophysical Union (AGU)
- Published
- 2012-04
- Volume
- 48
- Issue
- 4
- ISSN
- 0043-1397
- 1944-7973
- Cited by
- 1,219
- References
- 0
- Language
- en
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