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DOI10.1016/j.earscirev.2021.103728
Biological albedo reduction on ice sheets, glaciers, and snowfields
Hotaling S.; Lutz S.; Dial R.J.; Anesio A.M.; Benning L.G.; Fountain A.G.; Kelley J.L.; McCutcheon J.; Skiles S.M.; Takeuchi N.; Hamilton T.L.
发表日期2021
ISSN00128252
卷号220
英文摘要The global cryosphere, Earth's frozen water, is in precipitous decline. The ongoing and predicted impacts of cryosphere loss are diverse, ranging from disappearance of entire biomes to crises of water availability. Covering approximately one-fifth of the planet, mass loss from the terrestrial cryosphere is driven primarily by a warming atmosphere but reductions in albedo (the proportion of reflected light) also contribute by increasing absorption of solar radiation. In addition to dust and other abiotic impurities, biological communities substantially reduce albedo worldwide. In this review, we provide a global synthesis of biological albedo reduction (BAR) in terrestrial snow and ice ecosystems. We first focus on known drivers—algal blooms and cryoconite (granular sediment on the ice that includes both mineral and biological material)—as they account for much of the biological albedo variability in snow and ice habitats. We then consider an array of potential drivers of BAR whose impacts may be overlooked, such as arthropod deposition, resident organisms (e.g., dark-bodied glacier ice worms), and larger vertebrates, including humans, that transiently visit the cryosphere. We consider both primary (e.g., BAR due to the presence of pigmented algal cells) and indirect (e.g., nutrient addition from arthropod deposition) effects, as well as interactions among biological groups (e.g., birds feeding on ice worms). Collectively, we highlight that in many cases, overlooked drivers and interactions among factors have considerable potential to alter BAR, perhaps rivaling the direct effects of algal blooms and cryoconite. We conclude by highlighting knowledge gaps for the field with an emphasis on the underrepresentation of genomic tools, understudied areas (particularly high-elevation glaciers at tropical latitudes), and a dearth of temporal sampling in current efforts. We detail a global framework for long-term BAR monitoring that, if implemented, would yield a tremendous amount of insight for BAR and would be particularly valuable in light of the rapid ecological and physical changes occurring in the contemporary cryosphere. © 2021
关键词Biogeophysical feedbackCryoconiteCryosphereGlacier biologyIce algaeSnow algae
英文关键词Arthropoda; Vertebrata
语种英语
来源期刊Earth Science Reviews
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/204050
作者单位School of Biological Sciences, Washington State University, Pullman, WA, United States; GFZ German Research Center for Geosciences, Telegrafenberg, Potsdam, 14473, Germany; Institute of Culture and Environment, Alaska Pacific University, Anchorage, AK, United States; Department of Environmental Science, Aarhus University, Roskilde, 4000, Denmark; Department of Earth Sciences, Free University of Berlin, Berlin, 12249, Germany; Departments of Geology and Geography, Portland State University, Portland, OR, United States; Department of Earth and Environmental Sciences, University of Waterloo, Waterloo, Canada; Department of Geography, University of Utah, Salt Lake City, UT, United States; Department of Earth Sciences, Graduate School of Science, Chiba University, Chiba, Japan; Department of Plant and Microbial Biology and The BioTechnology Institute, University of Minnesota, Saint Paul, MN, United States
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Hotaling S.,Lutz S.,Dial R.J.,et al. Biological albedo reduction on ice sheets, glaciers, and snowfields[J],2021,220.
APA Hotaling S..,Lutz S..,Dial R.J..,Anesio A.M..,Benning L.G..,...&Hamilton T.L..(2021).Biological albedo reduction on ice sheets, glaciers, and snowfields.Earth Science Reviews,220.
MLA Hotaling S.,et al."Biological albedo reduction on ice sheets, glaciers, and snowfields".Earth Science Reviews 220(2021).
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