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降水观测误差修正对降水变化趋势的影响
  • 期刊名称:冰川冻土
  • 时间:0
  • 页码:717-725
  • 语言:中文
  • 分类:P343.6[天文地球—水文科学;天文地球—地球物理学] P467[天文地球—大气科学及气象学]
  • 作者机构:[1]Institute of Climate System, Chinese Academy of Meteorological Sciences, Beijing 100081, China, [2]State Key Laboratory of Cryospheric Science, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China
  • 相关基金:We would like to thank all anonymous reviewers for their constructive suggestions. This work was supported by the National Natural Science Foundation of China (40871036), the Open Foundation of the State Key Laboratory of Cryospheric Science, Chinese Academy of Sciences (SKLCS0904), the China Postdoctoral Science Foundation (20110490062) and the National Natural Science Foundation of China (41001006).
  • 相关项目:乌鲁木齐河源多年冻土的水文效应研究
中文摘要:

自从 1961,这研究在冰河地区和在中国的 Tianshan 山的冰河号码 1 的雪作文分析变化,并且他们有气候的可能的关系。降水统治了雪作文和那空气温度,降水控制了冰河地区的分发,这被发现,但是在降水的 interannual 变化在 19631981 期间在冰河地区和雪作文上有相对大的效果(P10 ) 并且 19631989 (P11 ) 。然而,在 19822007 期间(P20 ) 并且 19902007 (P21 ) ,空气温度上升(0.57 ?????????  ??????????? T

英文摘要:

This study analyzes the changes in glacier zones and snow composition of Glacier No. 1 in the Tianshan Mountains of China since 1961, and their possible relations with climate. It is found that precipitation dominated the snow composition and that air temperature and precipitation controlled the distribution of glacier zones, but interannual change in precipitation had a relatively large effect on glacier zones and snow composition during 1963-1981 (P10) and 1963-1989 (P1 1). However, during 1982-2007 (P2 0) and 1990-2007 (P21), the air temperature rise (0.57℃/10 a for P2 0, 0.76℃/10 a for P21) was more influential than the precipitation increase (51.3 mm/10 a for P20), and air temperature was principally responsible for the evolution of glacier zones and snow composition most probably resulting from recent climate warming.

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