Understanding the spatial and temporal dynamics of surface water extent is essential for water management planning and for monitoring drought and flood events. For instance, dam release schedules may take into account historical reservoir water levels and past responses to major precipitation events, while adjusting for active water resource needs (Bureau of Reclamation, 2020;Pulwarty & Melis, 2001). Daily streamflow data have been used to build a comprehensive multi-decadal record of droughts in the conterminous United States (hereafter US) (Austin et al., 2017;Zou et al., 2018). Investigations of surface water peaks over time may also help construct flood chronologies (Smith et al., 2018). Flooding has caused major monetary impacts across the US over the past century (Downton et al., 2005); identifying the patterns and causes of flooding can help estimate future damages (Wobus et al., 2014). While the U.S. Geological Survey (USGS) maintains streamgages that sample representative locations to support regional water management, flood forecasting, and trend detection (National Research Council, 2004), measurements from discrete locations may not provide a complete picture of surface