廣東地區(qū)后汛期降水集中度和集中期特征
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Characteristics of Precipitation Concentration Degree and Precipitation Concentration Period during Second Rainy Season in Guangdong
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    摘要:

    利用廣東省23個臺站1961—2006年后汛期(7—9月)逐候的降水資料,計算了降水集中度和集中期,并討論了其時空分布特征和變化規(guī)律。結(jié)果表明,降水集中度和集中期能夠表征降水量在時空場上的變化,降水集中度和集中期EOF的第1特征向量表現(xiàn)出一致的上升趨勢,呈現(xiàn)東北—西南向分布,第2特征向量變化特征呈東西向反向分布。廣東地區(qū)后汛期降水集中度呈逐年微弱下降趨勢,并在年代際和年季尺度上存在不同的周期變化。廣東地區(qū)降水集中度分布不均,在廣東中部多水年的集中度大于少水年,多水年集中期要小于少水年。環(huán)流場的分析表明,集中度的高值年,1000 hPa、500 hPa上我國北方均易受高壓控制,存在高度場的正距平中心,同時高壓易于南伸,與南方暖濕空氣交匯,容易導(dǎo)致強降水。

    Abstract:

    By use of the pentad precipitation data from 23 stations in Guangdong Province during the second rainy season (July to September) from 1961 to 2006, the characteristics of the spatialtemporal distribution and variation of precipitation are analyzed in terms of the Precipitation Concentration Degree (PCD) and Precipitation Concentration Period (PCP). The results show that PCD and PCP can reflect well the spatialtemporal distribution of the precipitation. There was a weak descending trend and various periodic variations at interannual and decade scales in PCD in Guangdong Province during the second rainy season. The spatial distribution of PCD shows the characteristic of decreasing from north to south successively. PCD had a uneven distribution, more concentrative over the central part of Guangdong in rainy years than dry years. PCPs in rainy years were smaller than those in dry years. By the empirical orthogonal function (EOF) method, the first eigenvector of PCD shows the characteristic of identical increasing trend over the province, with the contours being northeastsouthwest oriented, but the second eigenvector is opposite from the east to the west. The circulation field analysis shows that in the high PCD years, the northern China was often controlled by high pressure systems at 1000 hPa and 500 hPa high fields, and there was usually a positive anomaly center in the height field, while the high pressure often extended southward, which converged with the warm and wet air, leading to strong precipitation.

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張金玲,王冀,鄒菊香,韓照宇.廣東地區(qū)后汛期降水集中度和集中期特征[J].氣象科技,2011,39(4):401~407

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  • 收稿日期:2010-04-02
  • 定稿日期:2010-11-09
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