Global water withdrawal and usage have risen nearly sixfold since 1900. Approximately 69% of water withdrawals are used in agriculture, 19% in industries, and 12% for municipal purposes (Food and Agriculture Organization of the United Nations, 2020). Anthropogenic disturbances and climate change affect the water cycle, water supply and demand, and impose stress on the global water systems (Haddeland et al., 2014). As such, hydrologists, geologists, agronomists, soil scientists, and engineers need reliable tools to monitor and manage surface and groundwater resources, particularly in locations where traditional monitoring is inadequate.Traditional water monitoring and measurement techniques are time-consuming, costly, and typify an inadequate and disproportionate spatial and temporal range. Over the past few decades, airplanes and satellites have been the chief source of remotely sensed water resource data. However, the usefulness of these platforms is mainly restricted to the largest spatial scales. The low frequency of temporal sampling is dictated by logistical costs (aerial imagery) or tasking schedules (satellites; Becker et al., 2009;Xue & Su, 2017). The dearth of finer resolution data and temporal inflexibility of these platforms precludes the possibility of on-demand data acquisition that is often necessary to capture the highly transient processes operating at fine spatial scales necessary for the planning and management of water resources (e.g., freshwater abstraction) and the assessment of hazards (e.g., flood extents). However, with recent advances in sensors, cameras,