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作 者:孙钦明[1] 刘彤[1] 董合干[1] 张荣[1] 李勇冠[1] 秦春明[2]
机构地区:[1]石河子大学生命科学学院,新疆石河子832003 [2]石河子气象局,新疆石河子832003
出 处:《生态学杂志》2012年第6期1508-1516,共9页Chinese Journal of Ecology
基 金:国家"十一五"科技支撑计划项目(2007BAC17B03)资助
摘 要:湿润指数揭示了地表干湿变化趋势,与降水变化相比,它更能客观地诠释在全球增暖背景下区域干湿演变特征及变化趋势。本文运用消除趋势波动分析、样条函数法和最小二乘法等方法,对天山以北5个不同区域1962—2009年的地表湿润指数的时空变化趋势和降水、气温变化趋势的空间分布进行统计,以分析各分区的不同年份、季节气候干湿变化特征。结果表明:各分区分季节湿润指数序列在48年的时间尺度上具有微弱的Hurst效应,即具有较弱的长期持续性和较强的随机性,并且各分区不同季节差异较明显;近48年来天山北部荒漠绿洲区降水整体呈现统计意义上的增加趋势,但地表湿润指数变化趋势差异较大;干化趋势最显著的地区与增暖最强烈的地区对应,干化趋势最显著的地区在伊犁谷地及其周围地区,准噶尔西部山地和东部边缘地区干化趋势次之;干湿变化表现出明显的季节差异,干化趋势最显著的季节为冬季和秋季,春季次之,夏季全区表现为明显的变湿趋势。Surface moisture index is more objective than precipitation in describing regional dr- ying-wetting feature and its changing trend under the background of global warming. Based on the meteorological data from 21 stations in 1962-2009, and by using detrended fluctuation analysis, spline interpolation, and least square fitting, this paper analyzed the spatiotemporal variations of surface moisture index, precipitation, and air temperature in different sub-regions of north Tians- han Mountains, Xinjiang of Northwest China in 1962-2009. During the past 48 years, the tem- poral pattern of the moisture index showed a weak Hurst' s effect, i. e. , the moisture index ex- hibited relatively weak persistence and relatively strong randomness through the time. There was a significant seasonal difference among the sub-regions. In desert oasis sub-region, the annual precipitation had an overall increase, but the moisture index varied spatially. The sub-regions that experienced significant drying also experienced significant warming, and the sub-regions with the most significant drying were the Ili Valley, followed by the west mountainous area and the eastern edge of Junggar basin. The ground surface drying-wetting also varied seasonally, with a trend of becoming drier in winter and autumn, followed by in spring, and wetter in summer.
分 类 号:P468.023[天文地球—大气科学及气象学]
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