“…As a result, researchers may seek to produce adequate models for vulnerable areas without extensive in situ data on soils, channel morphology, and/or streamflow records, not to mention the regular measurements of pathogen or sediment concentrations needed to calibrate fate and transport models (Coffey, et al 2010). Remotely sensed Synthetic Aperture Radar (SAR) and LIDAR images of flood extent and topographical features have proven useful for parameterizing and validating a number of flood inundation models at high spatial resolutions (Bates 2004, Horritt and Bates 2002, Bates, et al 2003, Straatsma and Baptist 2007, Smith 1997, Patro, et al 2009, Bates, et al 1997). However, the use of such image-based techniques to describe the dynamics of inundation over the duration of a flood event, and thus establish credible estimates of flow velocities and other transport-relevant parameters, requires high resolution imagery, both spatially and temporally (Bates 2012, Di Baldassarre and Uhlenbrook 2012).…”