干旱区生态环境知识资源中心(Arid): 新疆乌-昌地区干湿气候要素时空变化分析

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	新疆乌-昌地区干湿气候要素时空变化分析
其他题名	Spatiotemporal Variations in Dry-Wet Climatic Variables over the Urumqi-Changji Region of Xinjiang
	普宗朝; 张山清; 宾建华; 窦新英
来源期刊	资源科学
ISSN	1007-7588
出版年	2011
卷号	33 期号:12 页码:2314-2322
中文摘要	利用新疆乌鲁木齐市和昌吉回族自治州16个气象站1961年-2009年的逐月气候资料，使用线性趋势分析、Mann-Kendall检测以及基于ArcGis的混合插值法对年降水量、潜在蒸散量、干湿指数、水分亏缺量等干湿气候要素的变化趋势、突变特征以及各要素多年平均值、突变前后变化量的空间分布进行了分析，结果表明：乌昌地区年降水量和年干湿指数在空间分布上表现为山区大，平原小；西部大，东部小的格局，年潜在蒸散量和水分亏缺量表现为平原大，山区小；东部大，西部小的格局。近49a，乌昌地区年降水量和干湿指数分别以13.843mm/10a和0.016/10a的倾向率呈极显著(p=0.001)的上升趋势，并分别于1990年和1987年发生了突变性的增大；年潜在蒸散量和水分亏缺量分别以-16.07mm/10a和-29.909mm/10a的倾向率呈极显著的下降趋势，并分别于1983年和1986年发生了突变性的减小，气候总体呈较明显的变湿趋势。但各地的变化具有明显的区域性差异，突变后较突变前，年降水量和干湿指数的增加幅度表现为山区大，平原小，年潜在蒸散量和年水分亏缺量的减小幅度表现为中部平原大，南部山区和北部沙漠边缘地带小的空间分布格局。
英文摘要	Urumqi City and Changji Hui national autonomous prefecture (Urumqi-Changji region) is located in the northern slope of the Tianshan Mountains and southern edge of the Junggar Basin of Xinjiang. The precipitation is extremely less and evaporation is high over this region. Dry climate and water shortage are the major factors restricting local socio-economic development, especially agricultural production and environmental protection. To investigate characteristics of dry-wet climate change in the past 49 years in the Urumqi-Changji region, based on monthly climate data from 1961 to 2009 at 16 meteorological stations across the Urumqi-Changji region, fundamental characteristics of spatial-temporal change in various dry-wet climate variables, such as annual precipitation, potential evapotranspiration (ETo), dry-wet index, and water deficiency, were comprehensively analyzed using methods of linear regression, Mann-Kendall test, three-dimensional and quadratic trend surface simulation, and inverse distance weighting interpolation. Results show that the dry-wet climate is completely different for varying regions in the Urumqi-Changji region. In general, the annual precipitation and dry-wet index are larger in the Tianshan Mountain areas and western areas than in plain and eastern areas. ETo and water deficiency are generally larger in plain and eastern areas than in the Tianshan mountain areas and western areas in the Urumqi-Changji region. A climate wetting trend was evident in recent 49 years. The annual precipitation and dry-wet index showed a significant increasing trend at a rate of 13.843 mm/10a and 0.016/10a, respectively, showing a significantly abrupt increase in 1990 and 1987, respectively. ETo and water deficiency showed a significantly decreasing trend at a rate of-16.07mm/10a and-29.909mm/10a, respectively, with abrupt decreases occurring in 1983 and 1986, respectively. In general, the climate showed an obvious wetting trend over the recent 49 years. The increasing range of precipitation and the dry-wet index in the Tianshan Mountain areas was larger than in plain areas. The decreasing range of ETo and water deficiency in central plain areas was larger than in the Tianshan mountain areas and Gurbantunggut desert edge areas. It was found that the climate has become humid, which would lead to increases in water resources, decreases in evapotranspiration from farmland and natural vegetation, reductions in crop water requirement, and be conducive to easing fierce contradictions between water supply and demand and improving the fragile environment over the study region.
中文关键词	乌昌地区 ; 干湿气候 ; 时空变化
英文关键词	GIS Urumqi-Changji region of Xinjiang Dry-wet climate Spatial-temporal change
语种	中文
国家	中国
收录类别	CSCD
WOS类目	METEOROLOGY ATMOSPHERIC SCIENCES
WOS研究方向	Meteorology & Atmospheric Sciences
CSCD记录号	CSCD:4397451
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/227670
作者单位	新疆乌鲁木齐市气象局, 乌鲁木齐, 新疆 830001, 中国
推荐引用方式 GB/T 7714	普宗朝,张山清,宾建华,等. 新疆乌-昌地区干湿气候要素时空变化分析[J],2011,33(12):2314-2322.
APA	普宗朝,张山清,宾建华,&窦新英.(2011).新疆乌-昌地区干湿气候要素时空变化分析.资源科学,33(12),2314-2322.
MLA	普宗朝,et al."新疆乌-昌地区干湿气候要素时空变化分析".资源科学 33.12(2011):2314-2322.