The Cryosphere, 9, 905–923, 2015 www.the-cryosphere.net/9/905/2015/ doi:10.5194/tc-9-905-2015 © Author(s) 2015. CC Attribution 3.0 License. Multi-modal albedo distributions in the ablation area of the southwestern Greenland Ice Sheet S. E. Moustafa1, A. K. Rennermalm1, L. C. Smith2, M. A. Miller3, J. R. Mioduszewski1, L. S. Koenig4,*, M. G. Hom5,6, and C. A. Shuman4,7 1Department of Geography, Rutgers, The State University of New Jersey, 54 Joyce Kilmer Avenue, Piscataway, NJ 08854-8045, USA 2Department of Geography, University of California, Los Angeles, 1255 Bunche Hall, P. O. Box 951524, Los Angeles, CA 90095-1524, USA 3Department of Environmental Sciences, Rutgers, The State University of New Jersey, 14 College Farm Rd, New Brunswick, NJ 08901-8551, USA 4Cryospheric Sciences Laboratory, NASA Goddard Space Flight Center, 8800 Greenbelt Road, Greenbelt, MD, 20771, USA 5Biospheric Sciences Laboratory, NASA Goddard Space Flight Center, 8800 Greenbelt Road, Greenbelt, MD, 20771, USA 6Science Systems and Applications, Inc., 10210 Greenbelt Rd, Lanham, MD, 20706, USA 7Joint Center for Earth Systems Technology (JCET), University of Maryland, Baltimore County, 1000 Hilltop Circle, Baltimore, MD, 21250, USA *now at: National Snow and Ice Data Center, University of Colorado, 1540 30th Ave., Boulder CO 80303, USA Correspondence to: S. E. Moustafa (
[email protected]) Received: 4 August 2014 – Published in The Cryosphere Discuss.: 5 September 2014 Revised: 1 March 2015 – Accepted: 26 March 2015 – Published: 7 May 2015 Abstract. Surface albedo is a key variable controlling solar and ice facies characterizing the two peaks. Our results show radiation absorbed at the Greenland Ice Sheet (GrIS) surface that a shift from a distribution dominated by high to low albe- and, thus, meltwater production.