Rivers and lakes serve as vital sources of freshwater for ecosystems and civilizations worldwide (Everard & Powell, 2002;Macklin & Lewin, 2015;Yevjevich, 1992). While rivers and lakes are often treated as separate systems in large-scale remote sensing studies, their hydrologies are intimately related such that hydrologic changes in one water body type can be used to constrain the hydrology of an adjacent water body of a different type (Vörösmarty et al., 2000). For example, the relationship between inflow and outflow of a natural lake or human-made reservoir (hereinafter collectively referred to as a "lake" unless otherwise stated) can control the lake's volumetric water storage and water surface elevation. Natural lakes located along river networks can attenuate local discharge downstream and actively managed reservoirs can significantly affect downstream flow regime by altering the natural timing and quantity of river discharge (Doll et al., 2009;Wang et al., 2017;Yang et al., 2022). Reservoir inflow and outflow dynamics are key for modeling reservoir operations, which can be difficult to simulate from water mass balance alone, especially at the continental to global scale (Cohen et al., 2014;Harrigan et al., 2020). At these large scales, understanding of the hydrologic interplay between rivers and lakes has largely been developed through the analysis of streamflow gauges located on lake inflows and outflows (i.e., the rivers flowing into and out of a lake), as well as lake-level gauges (Batalla et al., 2004;Shiklomanov & Lammers, 2009;Yang et al., 2008). Unfortunately, most lakes do not have publicly available gauge data and those that do are primarily located on large lakes or in a few geographically isolated regions (