湖北农业科学 ›› 2018, Vol. 57 ›› Issue (13): 28-33.doi: 10.14088/j.cnki.issn0439-8114.2018.13.007

• 资源·环境 • 上一篇    下一篇

2011—2012年冬季西南地区干旱的时空分布特征及其动力成因诊断

周莉1, 蔡荣辉1, 兰明才1, 邓朝平1, 文萍1, 张舰齐2, 刘立军3   

  1. 1.湖南省气象台,长沙 410118;
    2.国防科技大学气象海洋学院,长沙 410118;
    3.空军参谋部气象局,北京 100032
  • 收稿日期:2018-01-16 出版日期:2018-07-10 发布日期:2019-12-23
  • 通讯作者: 兰明才(1984-),男,工程师,硕士,主要从事天气预报预测及短时临近预报预警技术研究,(电子信箱)372917798@qq.com。
  • 作者简介:周 莉(1989-),女,江苏扬州人,工程师,硕士,主要从事天气气候诊断研究工作,(电话)15116385600(电子信箱)442601285@qq.com;
  • 基金资助:
    湖南省气象台2018年湖南省气象局预报员专项(XQKJ18C011; XQKJ18C009)

Temporal and Spatial Distribution Characteristics of Drought in Southwest China During 2011—2012 and Its Diagnostic Analysis of Dynamic Causes

ZHOU Li1, CAI Rong-hui1, LAN Ming-cai1, DENG Cao-ping1, WEN ping1, ZHANG Jian-qi2, LIU Li-jun3   

  1. 1.Meteorological Observatory of Hunan Province,Changsha 410118,China;
    2.National University of Defense and Technology,Changsha 410118,China;
    3.Meteorologic Bureau of Air Force Staff,Beijing 100032,China
  • Received:2018-01-16 Online:2018-07-10 Published:2019-12-23

摘要: 利用NCEP/NCAR分析逐月逐日气象资料、全国基准站降水资料以及向外长波辐射(OLR,outgoing longwave radiation)资料,采用气候诊断方法,着重从环流特征、西太平洋副高及东亚冬季风特征、冷空气及湿度条件等方面,对2011—2012年冬季西南地区干旱的成因进行初步的动力诊断。结果表明,西伯利亚高压较常年同期明显偏强,东亚冬季风偏强的特征使得冷空气位置比较偏北偏东,能影响西南西北部的冷空气较常年偏弱,不利于冬季西南西部地区降水发生。同时,西太洋副热带高压较常年异常偏强,脊线位置偏北,不利于将孟加拉湾等地的暖湿气流输送到云贵高原;此外,孟加拉以及云南省一带的OLR偏高,表明由于对流活动受到抑制,使得天气持续晴朗少雨。

关键词: 西南地区, 干旱, 大气环流异常, 时空分布特征, 动力成因

Abstract: Analysis of monthly and daily meteorological data, the national benchmark station precipitation data and outgoing longwave radiation using NCEP/NCAR(OLR, outgoing longwave radiation), the climate diagnosis method, mainly from the aspects of circulation features, the West Pacific subtropical high and the East Asian Winter Monsoon characteristics, cold air and humidity conditions, analyze the causes of the preliminary diagnosis 2011 to 2012 winter drought in southwest China. The results show that the Siberia high pressure is obviously stronger than that of the same period of the year, and the strong feature of the East Asian Winter Monsoon makes the cold air position more northerly and easterly, and the cold air which influences the southwest and northwest is weaker than that of the whole year. It is not conducive to precipitation in Southwest China in winter. At the same time, the Western Pacific subtropical high was stronger than normal, the location of the North ridge line, is not conducive to the delivery of warm air to the bay of Bengal to the Yunnan Guizhou Plateau; in addition, Bangladesh Yunnan province area to show high OLR, inhibited due to convection, the weather continued fine little rain.

Key words: Southwest China, drought, atmospheric circulation anomaly, temporal and spatial distribution characteristics, dynamic cause of formation

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