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作 者:Zhiwen Dong Hongchen Jiang Giovanni Baccolo Biagio Di Mauro Krzysztof Zawierucha
机构地区:[1]State Key Laboratory of Cryosphere Sciences,Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,China [2]State Key Laboratory of Biogeology and Environmental Geology,China University of Geosciences,Wuhan 430078,China [3]Laboratory of Environmental Chemistry,Paul Scherrer Institut,Villigen 5234,Switzerland [4]Institute of Polar Sciences,National Research Council of Italy,Milan 20121,Italy [5]Department of Animal Taxonomy and Ecology,Faculty of Biology,Adam Mickiewicz University,Poznan 61-614,Poland
出 处:《Journal of Earth Science》2023年第6期1951-1956,共6页地球科学学刊(英文版)
基 金:supported by the National Natural Science Foundation of China(Nos.42022002,42201152,42371139,41941005);the State Key Laboratory of Cryosphere Sciences(No.SKLCS-ZZ-2023);the Gansu Province Natural Science Foundation Key Project(No.23JRRA858);the Excellent Doctoral Program of Gansu Province(No.23JRRA626).
摘 要:1 BACKGROUND The cryosphere covers a relevant portion of the Earth’s surface,playing a major role for terrestrial and marine biomes(Bosson et al.,2023;Sands et al.,2023;Anesio et al.,2017).Glacierets,glaciers and ice sheets represent together 10%of the global land surface,while the annual average maximum of snow cover during the winter accounts for up to 49%of the Northern Hemisphere’s surface (Qin,2017).Aerosols are another major component of the Earth system,playing pivotal roles in the biogeochemical cycles and in the Earth radiative mass balance (Bellouin et al.,2020;Carslaw et al.,2010).A complex network of interactions links aerosols and glaciers.
关 键 词:ATMOSPHERE Earth WINTER
分 类 号:X513[环境科学与工程—环境工程] P343.6[天文地球—水文科学]
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