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近50年新疆冬季热量资源时空变化
普宗朝1,张山清2,李景林2,徐文修3,王命全2,伊力哈木4
0
((1.新疆乌鲁木齐市气象局, 新疆 乌鲁木齐 830002; 2.新疆农业气象台, 新疆 乌鲁木齐 830002;3.新疆农业大学农学院, 新疆 乌鲁木齐 830052; 4.新疆气象信息中心, 新疆 乌鲁木齐 830002))
摘要:
利用新疆101个气象站1961—2010年的逐日平均气温和逐年极端最低气温资料,使用线性趋势和Mann-Kendall法对最冷月1月平均气温、年极端最低气温、冬季负积温和越冬期日数等冬季热量要素变化趋势、突变特征进行分析,采用混合插值法,在ArcGIS平台上完成基于数字高程模型(DEM)数据的各热量要素多年平均值和突变前后变化量的空间分布式模拟。结果表明:(1) 新疆1月平均气温、年极端最低气温总体呈现“南疆高,北疆低;平原和盆地高,山区低”的特点,冬季负积温和越冬期日数总体呈现“南疆少,北疆多;平原和盆地少,山区多”的分布格局。(2) 在全球变暖背景下,1961—2010年新疆冬季热量资源呈明显的增多趋势,并且1月平均气温和年极端最低气温分别于19 79年和1980年发生了突变性的升高,冬季负积温和越冬期日数分别于1986年和1998年发生了突变性的减少。突变年前后,1月平均气温和年极端最低气温上升幅度的空间分布总体呈“从东南至西北递增”的格局,冬季负积温减少幅度的空间分布呈“由南向北递增”的特点,越冬期日数减少幅度的空间分布呈“南疆大,北疆小;盆地大,天山和阿勒泰山区小”的格局。
关键词:  新疆  冬季热量资源  时空变化  ArcGIS
DOI:
基金项目:国家自然科学基金项目(31260312);新疆气象局科研项目(201127,201312)
Spatial-temporal Variation of Heat Resources in Winter of Xinjiang near 50 years
PU Zong-chao1, ZHANG Shan-qing2, LI Jing-lin2, XU Wen-xiu3, WANG Ming-quan2, Yili-hamu4
()
Abstract:
Using the daily mean temperature and annual extreme minimum temperature data from 101 meteorological stations during 1961 to 2010 in Xinjiang, were analyzed the changing trend and abruptly changing characteristic of heat element in winter for the January mean temperature, yearly extreme minimum temperature, accumulated negative temperature and the day numbers in winter by using the linear tendency method and Mann-Kendall method, and by using the mixed model, have finished the spacial distribution simulation for the average value in multi-years of each heat element in winter and the variation before and after abrupt change based on the digit elevation model(DEM) on the platform of the ArcGIS. The results showed that: (1) January mean temperature and annual extreme minimum temperature in Xinjiang were showed the characteristic of higher in southern Xinjiang, lower in northern Xinjiang; Higher in plain and valley, and lower in mountain areas; The accumulated negative temperature and the day numbers in winter were showed the distribution style as less in southern Xinjiang, more in northern Xinjiang; And less in plain and valley, more in mountain areas. (2) Under the background of global warming, the heat resource in winter of Xinjiang was showed a significant increasing trend during 1961 to 2010, also January mean temperature and annual extreme minimum temperature occurred abruptly increase in 1979 and 1980 respectively, but the accumulated negative temperature and the day numbers in winter were abruptly decreased in 1986 and 1998 respectively. Before and after the abruptly change year, the spatial distribution of rise range for January mean temperature and annual extreme minimum temperature totally assumed the pattern as increase from southeast to northwest, the spatial distribution of reduced range for accumulated negative temperature assumed the characteristic as rise from south to north, and the spatial distribution of reduced range for the day numbers in winter assumed the pattern as more in southern Xinjiang, less in northern Xinjiang, plains, and more in plains and basins area, less in Tianshan Mountain and Altai Mountains areas.
Key words:  Xinjiang  heat resource in winter  spatial-temporal change  ArcGIS

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