APPLICATION OF REMOTE SENSING FOR HYDROLOGICAL STUDIES IN THE NEBRASKA SANDHILLS
Distribution of uncorrected surface temperatures was evaluated using processed Landsat thermal infrared data, acquired in summer and early fall. Each lake exhibits one or several zones with warm season patterns. These findings are consistent with data from Thermal Infrared Multispectral Scanner (Rundquist et al., 1985). They are also consistent with the results of reconnaissance of the Crescent Lake in January 2002, when the first ice melting was found in the same zones. We attribute this phenomenon to warmer lake temperatures near the groundwater inflow zones. In this case, temperature distribution was less affected by wind or solar radiation.
To corroborate the remote sensing-based methodology with ground-based data, spatially and temporally distributed measurements of the lakes temperatures were conducted in the summer 2002 on the dates of the Landsat-7 ETM+ sensor data acquisition. Spatial distributions of lake temperatures at different depths in three lakes were obtained and compared with the surface temperatures. In most cases, lake temperatures at some depths are correlated to the surface temperatures obtained from Landsat data. As a result, the hypothetical hydrological model of small portion of Sandhills was constructed. This model correlates well with hydrostratigraphic data inferred from previous studies in the area.