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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Melanie K. Vanderhoof</dc:contributor>
  <dc:contributor>Jay R. Christensen</dc:contributor>
  <dc:contributor>Heather E. Golden</dc:contributor>
  <dc:contributor>Charles R. Lane</dc:contributor>
  <dc:contributor>Adnan Rajib</dc:contributor>
  <dc:contributor>William Keenan</dc:contributor>
  <dc:contributor>Qianjin Zheng</dc:contributor>
  <dc:contributor>Arushi Khare</dc:contributor>
  <dc:creator>Wayana Dolan</dc:creator>
  <dc:date>2026</dc:date>
  <dc:description>&lt;p&gt;&lt;span id="_mce_caret" data-mce-bogus="1" data-mce-type="format-caret"&gt;&lt;span&gt;Quantifying and projecting the downstream benefits of water stored in lakes and wetlands (SW&lt;/span&gt;&lt;sub&gt;storage&lt;/sub&gt;&lt;span&gt;) requires watershed hydrologic models, which often parameterize surface water storage in topographic depressions using static digital elevation model (DEM) data. Calibration and validation of modeled SW&lt;/span&gt;&lt;sub&gt;storage&lt;/sub&gt;&lt;span&gt;&amp;nbsp;dynamics using external data sets is uncommon, particularly across major river basins, with model calibration typically focused on observed discharge. Here, we develop and assess a novel remote sensing-based (RS) SW&lt;/span&gt;&lt;sub&gt;storage&lt;/sub&gt;&lt;span&gt;&amp;nbsp;data set (Sentinel-1 and Sentinel-2) for verifying simulated SW&lt;/span&gt;&lt;sub&gt;storage&lt;/sub&gt;&lt;span&gt;&amp;nbsp;estimates from a Soil and Water Assessment Tool (SWAT) model of the Upper Mississippi River Basin (UMRB; ∼440,000&amp;nbsp;km&lt;/span&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;). Our results suggest that static DEM-based parameterization as well as model calibration based solely on discharge do not adequately capture spatial and temporal SW&lt;/span&gt;&lt;sub&gt;storage&lt;/sub&gt;&lt;span&gt;&amp;nbsp;dynamics in the UMRB. Mean SW&lt;/span&gt;&lt;sub&gt;storage&lt;/sub&gt;&lt;span&gt;&amp;nbsp;as estimated by SWAT was 74%&amp;nbsp;±&amp;nbsp;122% (mean&amp;nbsp;±&amp;nbsp;standard deviation) higher than RS SW&lt;/span&gt;&lt;sub&gt;storage&lt;/sub&gt;&lt;span&gt;, where SW&lt;/span&gt;&lt;sub&gt;storage&lt;/sub&gt;&lt;span&gt;&amp;nbsp;in SWAT was underestimated in wetland-rich subbasins and overestimated in agricultural, tile-drained subbasins. Time series of SWAT SW&lt;/span&gt;&lt;sub&gt;storage&lt;/sub&gt;&lt;span&gt;&amp;nbsp;and RS SW&lt;/span&gt;&lt;sub&gt;storage&lt;/sub&gt;&lt;span&gt;&amp;nbsp;were positively correlated in only 38.8% of subbasins. As RS SW&lt;/span&gt;&lt;sub&gt;storage&lt;/sub&gt;&lt;span&gt;&amp;nbsp;is also vulnerable to error, storage estimates were compared to bathymetric data in select small wetlands. While uncertainty remains in the conversion from extent to storage for RS SW&lt;/span&gt;&lt;sub&gt;storage&lt;/sub&gt;&lt;span&gt;, the method and data set presented here are a promising option for improved parameterization and calibration of SW&lt;/span&gt;&lt;sub&gt;storage&lt;/sub&gt;&lt;span&gt;&amp;nbsp;processes in SWAT and other process-based hydrologic models. Further consideration of these storage processes can potentially improve the accuracy of simulated streamflow in wetland-rich model domains.&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1029/2025WR040206</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Geophysical Union</dc:publisher>
  <dc:title>Remotely sensed surface water storage shows distinct patterns from SWAT-simulated data</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>