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1961-2002年新疆季节冻土多年变化及突变分析
引用本文:王秋香,李红军,魏荣庆,王晓梅. 1961-2002年新疆季节冻土多年变化及突变分析[J]. 冰川冻土, 2005, 27(6): 820-826. DOI: 10.7522/j.issn.1000-0240.2005.0122
作者姓名:王秋香  李红军  魏荣庆  王晓梅
作者单位:1. 新疆气象局, 环境气象中心, 新疆, 乌鲁木齐, 830002;2. 中国气象局, 乌鲁木齐沙漠气象研究所, 新疆, 乌鲁木齐, 830002
摘    要:对新疆41 a(1961/1962-2001/2002年)冬季平均冻土深度、最大冻土深度、土壤10 cm深度封冻时段资料分析表明,随着全疆气候的变暖,各地的平均冻土深度、最大冻土深度趋向变浅,土壤封冻时间缩短.尤其是1986年以后,暖湿化特征十分明显,冻土深度和封冻时间变化更为显著.最大冻土深度南、北疆分别在1982/1983年和1986/1987年冬季发生了明显的突变.

关 键 词:季节性冻土  气候变化  土壤封冻时间  突变  新疆  
文章编号:1000-0240(2005)06-0820-07
收稿时间:2005-08-11
修稿时间:2005-08-11

Annual Change and Abrupt Change of the Seasonal Frozen Soil in Xinjiang, China during 1961-2002
WANG Qiu-xiang,LI Hong-jun,WEI Rong-qing,WANG Xiao-mei. Annual Change and Abrupt Change of the Seasonal Frozen Soil in Xinjiang, China during 1961-2002[J]. Journal of Glaciology and Geocryology, 2005, 27(6): 820-826. DOI: 10.7522/j.issn.1000-0240.2005.0122
Authors:WANG Qiu-xiang  LI Hong-jun  WEI Rong-qing  WANG Xiao-mei
Affiliation:1. Environmental Meteorological Center, Xinjiang Meteorological Bureau, Ürümqi Xinjiang 830002, China;2. Ürümqi Instituteof Desert Meteorology, China Meteorological Administration, Ürümqi Xinjiang 830002, China
Abstract:In this paper,the average and maximum depths of seasonal frozen soil and the frozen duration of soil at 10 cm deep in Xinjiang during the 40-year period of 1961-2002 are analyzed.The results show that the average and maximum depths of seasonal frozen soil decrease and the frozen duration of soil becomes short under climate warming in Xinjiang.Such changes become more significant after climate warming-wetting since 1986.A significant mutation of the maximum depth of frozen soil occurred in both south Xinjiang and north Xinjiang in the mid-1980s.
Keywords:seasonal frozen soil  climate change  frozen duration of soil  mutation  Xinjiang
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