Drought intensity is often characterized using meteorological observations, such as precipitation, rather than hydrologic observations, such as reservoir levels and groundwater levels. While precipitation indicates the amount of water entering an area, precipitation models do not determine the amount of water retained in a watershed or the amount lost due to runoff and evapotranspiration, which are important factors for drought management. Researchers from the University of Montana addressed this need by producing a drought index that captures changes in both surface and subsurface hydrologic reservoirs/pools using a rapidly growing interdisciplinary field called hydrogeodesy.