01957nas a2200133   4500008004100000245010200041210006900143260005300212490000900265520146100274100002201735700002401757856004201781       2020                        eng d00aGlacial meltwater modeling to simulate lake water budget (1996-2013) in Taylor Valley, Antarctica0 aGlacial meltwater modeling to simulate lake water budget 1996201  aPortland, ORbPortland State Universityc01/20200 vM.S.3 a<p>The McMurdo Dry Valleys (MDV), the largest ice-free region (4,500 km2) in Antarctica, are a polar desert with an average annual temperature of -18 ̊C. In Taylor Valley, one of the MDV, closed-basin, perennially ice-covered lakes occupy the valley floor. Their water balance is controlled by inflow from glacial meltwater runoff and loss due to sublimation, making them sensitive indicators of climate. In this study, a physically-based model of glacier meltwater and lake ice sublimation is adapted to explain modern (1996 to 2013) lake-level variations. Meltwater model results were improved by the inclusion of MODIS remotely-sensed albedo measurements (E = 0.47; nRMSE = 0.73). After 2008 the meltwater model significantly under-predicted streamflow and only through decreasing albedo by -30% (equivalent to a decrease of -0.18 on average) did the results match observations (E = 0.79; nRMSE = 0.45). This study provides the first estimate of direct (unmeasured) glacier inflow to the lakes, 69%, 73% and 28%, and sublimation loss rates, 0.37 m yr<sup>-1</sup>, 0.24 m yr<sup>-1</sup> and 0.16 m yr<sup>-1</sup>, for Lakes Bonney, Hoare and Fryxell, respectively. Despite similar meltwater volumes entering Lakes Bonney and Fryxell, the difference in basin hypsometry results in a much faster lake rise at Bonney from 2002-13. If future climate conditions match current (1996-2013) conditions, all lakes will rise through the end of the century.</p>1 aCross, Julian, M.1 aFountain, Andrew, G  uhttps://archives.pdx.edu/ds/psu/30806