globalchange  > 气候变化与战略
CSCD记录号: CSCD:5623953
论文题名:
近30年来乌鲁木齐河源区空冰斗季节性积雪对气候变暖的响应
其他题名: The response of seasonal snow accumulation to the global warming in Kong -Bingdou basin during the past 30 years
作者: 张鹏1; 李忠勤1; 金爽2; 怀保娟2
刊名: 干旱区资源与环境
ISSN: 1003-7578
出版年: 2016
卷: 30, 期:2, 页码:211-218
语种: 中文
中文关键词: 空冰斗流域 ; 积雪 ; 气温 ; 降水 ; 最大积雪深度 ; 乌鲁木齐河源区
英文关键词: Kong - Bingdou basin ; snow accumulation ; temperature ; precipitation ; maximum snow depth ; headwater of Urumqi River basin
WOS学科分类: METEOROLOGY ATMOSPHERIC SCIENCES
WOS研究方向: Meteorology & Atmospheric Sciences
中文摘要: 利用中国科学院天山冰川观测试验站提供的1987 - 2014年的乌鲁木齐河源区空冰斗的气象观测资料,同时结合1987 - 1993/2006 - 2007/2014 - 2015对空冰斗季节性积雪的观测资料,分析了该区域积雪厚度,积雪日数的变化特征以及最大积雪深度与气温降水的关系。结果表明: 1)在积雪稳定期,气温和降水总体呈增加趋势,且这种趋势主要发生在春季。2)稳定期积雪的持续时间有明显的缩短趋势。积雪的最大深度出现在海拔3865m处,这一高度以下,积雪深度随海拔升高呈现上升趋势,而这一高度以上的地区则相反。3)积雪稳定期,降水对最大积雪深度的影响远远大于气温等其他气象因素。
英文摘要: Based on data of Kong - Bingdou meteorological station in Urumqi River basin for the period of 1987 - 2014 and the seasonal snow cover data of 1987 - 1993 /2006 - 2007 /2014 - 2015 of the Kong - Bingdou observations, we analyzed the relationships between the thickness of snow in the region,the number of days of snow cover variation and the temperature and precipitation. The results showed that: 1) In the snow stable periods, temperature and precipitation increased generally,and this trends occurred mainly in the spring. 2) The stable snow cover duration was decreasing significantly. The maximum depth of snow occurred at an altitude of 3865m; below the altitude,the snow depth showed rising trend with elevation rise,and above the altitude 3865m,it was opposite. 3) In the snow stable period,the impact of precipitation on maximum snow depth was far greater than other meteorological factors such as temperature.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/150848
Appears in Collections:气候变化与战略

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作者单位: 1.西北师范大学地理与环境科学学院, 兰州, 甘肃 730070, 中国
2.中国科学院寒区旱区环境与工程研究所, 兰州, 甘肃 730000, 中国

Recommended Citation:
张鹏,李忠勤,金爽,等. 近30年来乌鲁木齐河源区空冰斗季节性积雪对气候变暖的响应[J]. 干旱区资源与环境,2016-01-01,30(2):211-218
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