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Changes of Monsoonal Temperate Glaciers in China during the Past Several Decades under the Background of Global Warming 被引量:1

Changes of Monsoonal Temperate Glaciers in China during the Past Several Decades under the Background of Global Warming
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摘要 Based on various data,it can be concluded that eight monsoonal temperate glaciers in China were in stationary or ad-vancing between 1900s;930s and 1960s;980s,and were in retreating during 1930s;960s and 1980s;resent under the background of climate warming.The total glacier area has reduced by 3.11 km2 with a mean front altitude rise of 3.2 m/yr and 4 glaciers have disappeared in Mt.Yulong during 1957;999.Mass balance records indicated that glaciers had suf-fered a constant mass loss of snow and ice during the last several decades,and the accumulated mass balance in Hailuogou basin in Mt.Gongga was 10.83 m water equivalent in the past 45 years with a annual mean value of-0.24 m,and the value at Baishui glacier No.1 was-11.38 m water equivalent in the past 52 years with-0.22 m/yr.The inverse variation between mass balance and temperature in China and the Northern Hemisphere reflected that climate warming is mainly corresponding to constant ice and snow mass loss in the past 50 years.The change of the glaciers’ surface mor-phology has occurred since the 1980s,such as enlargement of glacier-lake and ice falls,resulted from the accelrative cli-mate warming. Based on various data,it can be concluded that eight monsoonal temperate glaciers in China were in stationary or ad-vancing between 1900s^1930s and 1960s^1980s,and were in retreating during 1930s^1960s and 1980s^present under the background of climate warming.The total glacier area has reduced by 3.11 km2 with a mean front altitude rise of 3.2 m/yr and 4 glaciers have disappeared in Mt.Yulong during 1957~1999.Mass balance records indicated that glaciers had suf-fered a constant mass loss of snow and ice during the last several decades,and the accumulated mass balance in Hailuogou basin in Mt.Gongga was 10.83 m water equivalent in the past 45 years with a annual mean value of-0.24 m,and the value at Baishui glacier No.1 was-11.38 m water equivalent in the past 52 years with-0.22 m/yr.The inverse variation between mass balance and temperature in China and the Northern Hemisphere reflected that climate warming is mainly corresponding to constant ice and snow mass loss in the past 50 years.The change of the glaciers' surface mor-phology has occurred since the 1980s,such as enlargement of glacier-lake and ice falls,resulted from the accelrative cli-mate warming.
出处 《Research in Cold and Arid Regions》 2008年第1期59-67,共9页 寒旱区科学(英文版)
基金 supported by a Major Directionality Program of Chinese Academy of Sciences (KZCXZ-YW-317) a National Basic Re-search Program of China (2007CB411201) a Key Project of the National Natural Science Foundation of China (90511007) an Innovative Research Interna-tional Partnership Project of Chinese Academy of Sciences (CXTD-Z2005-2) a Project for Outstanding Young Scientists of Chinese Natural Science Founda-tion (40121101) a West Light Foundation of Chinese Academy of Sciences (O828A11001) the Foun-dation from The State Key Laboratory of Cryosphere Science and Lijiang City Government
关键词 glacial change temperate glaciers climate warming glacial change temperate glaciers climate warming
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