近50 a华北平原日照时数的时空特征及其影响因素
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浙江省科技厅重点农业项目(2011C22082)


Temporal and spatial variations of sunshine duration and its influence factors in the north China plain in recent 50 years
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    摘要:

    利用1961—2010年华北平原50个站日照、降水、云量、风速和视程障碍日数等资料,采用线性倾向率、聚类分析和突变检测等方法,研究了华北平原年、季、月日照时数的时空特征及其成因。结果表明,华北平原年、季、月日照时数空间分布均呈北多南少的分布形式,春季最多,其次为夏、秋与冬季。近50a华北平原年日照时数普遍显著减少,区域平均减幅为93.4 h/10a,为同期全国平均(-45.9 h/10a)的两倍多,明显的年代际转折发生在1980s中后期。年日照时数异常偏多和偏少分别出现在1965年和2003年。四季日照时数也都明显减少,没有一个季节、一个测站的日照时数有明显的正趋势变化,夏季减幅最大也最明显,其次依次是冬、秋和春季。近30a年及夏、秋两季日照时数减幅增大,而冬、春两季减幅略缩小。大气透明度下降和平均风速减小是造成华北平原日照减少的主要原因,此外,在不同地区云量的作用也不尽相同。

    Abstract:

    Based on the data such as sunshine duration, rainfall, cloudiness, mean wind speed, and day numbers of vision obstruction of 50 stations in the north China plain during 1961—2010 with modern statistical diagnostic methods such as linear trend analysis, cluster analysis, and abrupt detection, the temporal/spatial features and cause of yearly, seasonal, and monthly sunshine duration in the north China plain were investigated in this paper. The results showed that the spatial distribution of yearly, seasonal, and monthly sunshine duration in the north of the north China plain was more than that in the south of the plain. The yearly sunshine duration was 1910.6-2982.9 h, and the maximum was in spring, and next in summer, autumn, and winter. The yearly sunshine duration in the north China plain in the recent 50 a was obviously reduced(93.4 h/10a), the reduction was over 2 times more than that of the national average(-45.9 h/10a) at the same period. The significant decadal change was in the middle/late 1980s. The yearly sunshine duration was extremely excessive in 1965,and extremely deficient in 2003. Meanwhile the seasonal sunshine duration was also obviously declined, but it did not show an obviously positive trend in a single season at a single station. The maximum reduction was in summer, and next in winter, autumn, and spring. The reduction rate of the seasonal sunshine duration in summer and autumn in recent 30 a was found to increase, but it reduced slightly in winter and spring. The reduction of the sunshine duration in the north China plain might be ascribed to the decline of the atmospheric transparency and the reduction of the mean wind speed. Moreover the effect of the cloudiness in different regions was different.

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陈红梅,张立波,娄伟平.近50 a华北平原日照时数的时空特征及其影响因素.气象科学,2012,32(5):573-579 CHEN Hongmei, ZHANG Libo, LOU Weiping. Temporal and spatial variations of sunshine duration and its influence factors in the north China plain in recent 50 years. Journal of the Meteorological Sciences,2012,32(5):573-579

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  • 收稿日期:2011-09-04
  • 最后修改日期:2012-03-03
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  • 在线发布日期: 2012-10-24
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