Biological albedo reduction on ice sheets, glaciers, and snowfields Scott Hotaling1, Stefanie Lutz2, Roman J. Dial3, Alexandre M. Anesio4, Liane G. Benning2,5, Andrew G. Fountain6, Joanna L. Kelley1, Jenine McCutcheon7, S. McKenzie Skiles8, Nozomu Takeuchi9, and Trinity L. Hamilton10 Affiliations: 1 School of Biological Sciences, Washington State University, Pullman, WA, USA 2 GFZ German Research Center for Geosciences, Telegrafenberg, 14473 Potsdam, Germany 3 Institute of Culture and Environment, Alaska Pacific University, Anchorage, AK, USA 4 Department of Environmental Science, Aarhus University, 4000 Roskilde, Denmark 5 Department of Earth Sciences, Free University of Berlin, 12249 Berlin, Germany 6 Departments of Geology and Geography, Portland State University, Portland, OR, USA 7 Department of Earth and Environmental Sciences, University of Waterloo, Waterloo, Canada 8 Department of Geography, University of Utah, Salt Lake City, UT, USA 9 Department of Earth Sciences, Graduate School of Science, Chiba University, Chiba, Japan 10 Department of Plant and Microbial Biology and The BioTechnology Institute, University of Minnesota, Saint Paul, MN, USA Correspondence: Scott Hotaling, School of Biological Sciences, Washington State University, Pullman, WA, 99164, USA; Email:
[email protected]; Phone: (828) 507-9950; ORCID: 0000-0002-5965- 0986 Trinity Hamilton, Department of Plant and Microbial Biology and the BioTechnology Institute, University of Minnesota, Saint Paul, MN, USA; Email:
[email protected]; Phone: (612) 625- 6372; ORCID: 0000-0002-2282-4655 Note: This article is a non-peer reviewed preprint submitted to EarthArXiv. It was submitted for peer review to Earth-Science Reviews in January 2021. 1 Abstract: 2 The global cryosphere, Earth’s frozen water, is in precipitous decline.