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Seasonal variation in total water storage in California inferred from GPS observations of vertical land motion

Argus, Donald F., Fu, Yuning, and Landerer, Felix W., 2014. Seasonal variation in total water storage in California inferred from GPS observations of vertical land motion. Geophysical Research Letters, 41(6):1971–1980, doi:10.1002/2014GL059570.

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@ARTICLE{2014GeoRL..41.1971A,
       author = {{Argus}, Donald F. and {Fu}, Yuning and {Landerer}, Felix W.},
        title = "{Seasonal variation in total water storage in California inferred from GPS observations of vertical land motion}",
      journal = {\grl},
     keywords = {California, GPS, hydrology, water, snow},
         year = 2014,
        month = mar,
       volume = {41},
       number = {6},
        pages = {1971-1980},
     abstract = "{GPS is accurately recording vertical motion of Earth's surface in
        elastic response to seasonal changes in surface water storage in
        California. California's mountains subside up to 12 mm in the
        fall and winter due to the load of snow and rain and then rise
        an identical amount in the spring and summer when the snow
        melts, the rain runs off, and soil moisture evaporates. We
        invert the GPS observations of seasonal vertical motions to
        infer changes in equivalent water thickness. GPS resolves the
        distribution of change in total water across California's
        physiographic provinces at a resolution of 50 km, compared to
        200 km resolution from the Gravity Recovery and Climate
        Experiment. The seasonal surface water thickness change is 0.6 m
        in the Sierra Nevada, Klamath, and southern Cascade Mountains
        and decreases sharply to about 0.1 m east into the Great Basin
        and west toward the Pacific coast. GPS provides an independent
        inference of change in total surface water, indicating water
        storage to be on average 50\% larger than in the NLDAS-Noah
        hydrology model, likely due to larger changes in snow and
        reservoir water than in the model. Seismicity and land uplift
        produced by groundwater loss in California's Central Valley is
        also being evaluated.}",
          doi = {10.1002/2014GL059570},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2014GeoRL..41.1971A},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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