The Landsat-Multispectral Scanner (MSS) data were used to measure lake area
fluctuations (1972-1989) for 130 groundwater dominated lakes in the Wester
n Lakes Region of the Nebraska Sand Hills. In general, the pattern shown in
lake area hydrographs was similar to that for in-situ lake elevations. In-
situ lake-elevation data verify that remote monitoring of surface-area fluc
tuations, even at relatively coarse spatial resolution, is not only practic
al and useful, but also it elucidates the hydrologic characteristics of gro
undwater-dominated lakes of the Sand Hills. The apparent differences in beh
avior between lakes in the northern and southern portions of the study area
may be related to both their location in the regional ground water system
and the substantial local hydrologic complexity.