Fiber optic remote sensing offers opportunities to bridge the gap between
point-scale (~1 meter) and satellite-scale (>1000 meters) observations. The
scattering behavior of laser light along a fiber optic cable serves as an effective
proxy for such hydrologically relevant states as soil temperature, soil moisture,
and snow water equivalent. These measurements are not only useful for
enhancing our understanding of hydrologic processes, but can also be used to
improve satellite retrieval algorithms.