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Due to their shallow vertical support, remotely sensedsurface soil moisture retrievals are commonly regarded as being of limitedvalue for water budget applications requiring the characterization oftemporal variations in total terrestrial water storage (dS ∕ dt). However, advancesin our ability to estimate evapotranspiration remotely now allow for thedirect evaluation of approaches for quantifying dS ∕ dt via water budget closureconsiderations. By applying an annual water budget analysis within a seriesof medium-scale (2000–10 000 km2) basins within the United States, wedemonstrate that, despite their clear theoretical limitations, surface soilmoisture retrievals derived from passive microwave remote sensing containstatistically significant information concerning dS ∕ dt. This suggests thepossibility of using (relatively) higher-resolution microwave remote sensingproducts to enhance the spatial resolution of dS ∕ dt estimates acquired fromgravity remote sensing

hydrology and earth system sciences

Estimating annual water storage variations in medium-scale (2000–10 000 km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) basins using microwave-based soil moisture retrievals