2011年1月貴州凍雨天氣成因分析
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公益性行業(氣象)科研專項資助項目(GYHY201206004)資助


Analysis of Freezing Rainfall in 2011 Winter in Guizhou
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    摘要:

    利用2011年1月NCEP1°×1°6 h再分析資料和貴州省氣象局提供的84個地面氣象站1970—2011年冬季(12月至次年2月)資料對貴州省2011年1月持續的低溫凍雨天氣進行了氣候統計和診斷分析。此次凍雨天氣范圍廣,強度大,34個站氣溫達到40年來歷史同期最低值。此次過程中的亞歐大陸環流異常的主要表現是烏拉爾山阻塞高壓階段性活躍,在里海槽前西南氣流的持續補充下兩次崩潰三次重建,在脊前形成深厚低壓中心,導致頻繁有冷空氣南下影響貴州地區。

    Abstract:

    The NCEP/NCAR reanalysis data (1°×1°,6 h) in January 2011 and the observation data in winter from 1970 to 2011 provided by Guizhou Meteorological Service are used to investigate the climatic characteristics of freezing disaster occurred in January 2011 and its causes by climate statistics and climate diagnostic methods. More than 34 stations reached the lowest temperature in the past 40 years during the freezing rain event. There were active blocking anticyclones near the Ural Mountains persistently, which were more active than the normal. They were broken down twice and rebuilt thrice, with the wet southwesterly flow brought by the strong Caspian Sea trough, supplying the warm air constantly. There was a strong and steady high existed in the front of the Urals blocking high and the frequent activities of trough, bringing cold air to the western China, which resulted in the freezing disaster in Guizhou region.

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李麗麗,肖天貴,黃金全,冷宇.2011年1月貴州凍雨天氣成因分析[J].氣象科技,2013,41(6):1116~1121

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  • 收稿日期:2012-08-08
  • 定稿日期:2012-12-11
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  • 在線發布日期: 2013-12-27
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