干旱区生态环境知识资源中心(Arid): 新疆地表水资源对气候变化的响应初探

Arid

	新疆地表水资源对气候变化的响应初探
其他题名	Probe into Response of Surface Water Resources to Climate Change in Xinjiang
	何清 1; 袁玉江 1; 魏文寿 1; 龚原 2
来源期刊	中国沙漠
ISSN	1000-694X
出版年	2003
卷号	23 期号:5 页码:493-496
中文摘要	计算新疆三大区域地表水资源与气候的相关性，建立两者间的回归方程，进而探讨新疆地表水资源对气候变化的响应，得到以下几点主要结论：①新疆地表水资源对气候变化的响应具有明显的地域特点：北疆以对水文年降水的正响应为主；南疆以对5～9月温度的正响应为主，以对高山区前年的水文年降水的正响应为辅；东疆对水文年降水的正响应及5～9月温度的负响应并重，对降水的响应更重要些。②北疆：当北疆8站水文年平均降水偏多(或偏少)lO％时，北疆地表水资源会偏多或偏少7．2％。③东疆：当沁城5～9月平均温度为多年平均值时，巴音布鲁克水文年降水变化lO％，东疆地表水资源会出现5．4％的变化；当巴音布鲁克水文年降水为多年平均值时，沁城5～9月平均温度偏高(或偏低)1℃，东疆地表水资源会减少(或增多)8．3％。④南疆：当南疆4站5～9月平均温度为多年平均值时，塔什库尔干前年的水文年降水变化lO％，南疆地表水资源会出现1．3％的变化；当塔什库尔干前年的水文年降水为多年平均值时，南疆4站5～9月平均温度偏高(或偏低)l℃，南疆地表水资源会增多(或减少)11．7％。
英文摘要	In this paper, the correlation between surface water resources and climate for three large regions of Xinjiang was established to study the response of surface water resources to climate change. Conclusions are as follows; ( 1 ) The response of surface water resources to climate change obviously has regional features. In northern Xinjiang, positive response of surface water resources lo precipitation of hyrlrological year is main; In southern Xinjiang, positive response of surface water resources lo mean temperature from May to September is the first, but positive response to precipitation of the former hydrological year for high mountain area is the second; In eastern Xinjiang, surface water resources responded to hydrological precipitation positively and to mean temperature from May to September negatively, but response lo precipitation is more important than that to temperature. (2) When mean precipitation of hydrological year for 8 stations in northern Xinjiang is more or less 10% than normal, the surface water resource is 7. 2% more or less than normal. (3) When mean temperature from May to September is in normal for Qincheng meteorological station in eastern Xinjiang, arid if precipitation of hydrological year change within 10% for Bayinbuluke meteorological station, the surface water resources for eastern Xinjiang will change by 5.4%; When precipitation is in normal for Bayinbuluke meteorological station, and if mean temperature from May to September for Qincheng meteorological station is I ’X] higher or lower than normal, the surface water resources for eastern Xinjiang will increase or decrease by 8. 3% . (4) When mean temperature from May to September for four meteorological station in southern Xinjiang is in normal, and if precipitation of former hydrological year change within 10% for Tashikuergan meteorological station, the surface water resources for southern Xinjiang will change by 1.3% ; When precipitation of former hydrological year is in normal, and if mean temperature from May to September for the four stations is 1 t higher or lower than normal, the surface water resources for southern Xinjiang will increase or decrease by 11.7%.
中文关键词	新疆 ; 地表水资源 ; 气候变化 ; 响应
英文关键词	Xinjiang surface water resources climate change response
语种	中文
国家	中国
收录类别	CSCD
WOS类目	AGRICULTURE MULTIDISCIPLINARY
WOS研究方向	Agriculture
CSCD记录号	CSCD:1310308
来源机构	中国气象局乌鲁木齐沙漠气象研究所
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/204675
作者单位	1.中国气象局乌鲁木齐沙漠气象研究所, 乌鲁木齐, 新疆 830002, 中国; 2.新疆水文水资源局, 乌鲁木齐, 新疆 830002, 中国
推荐引用方式 GB/T 7714	何清,袁玉江,魏文寿,等. 新疆地表水资源对气候变化的响应初探[J]. 中国气象局乌鲁木齐沙漠气象研究所,2003,23(5):493-496.
APA	何清,袁玉江,魏文寿,&龚原.(2003).新疆地表水资源对气候变化的响应初探.中国沙漠,23(5),493-496.
MLA	何清,et al."新疆地表水资源对气候变化的响应初探".中国沙漠 23.5(2003):493-496.