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Synoptic Aspects of the Catastrophic Flood Formation in the Northeast of Australia during Extreme La Nina 2010-2011

机译:2010-2011年极端拉尼娜期间澳大利亚东北部特大洪水形成的天气方面

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摘要

A synoptic mechanism of the formation of atmospheric circulation anomalies over the tropics of the Indian and Pacific oceans observed during the La Nifia 2010-2011 culmination is considered using the daily data of the NCEP/NCAR reanalysis. It was established that the most destructive flood during the whole modern history of Australia was caused by the unprecedented activity of the tropical cyclogenesis in the circulation system of the Australian summer monsoon. The tropical cyclones affected in turn the monsoon regions of Australia both from the Indian Ocean through the system of the equatorial zone of westerlies and from the Pacific Ocean through the system of the eastern trade wind. The Pacific trade wind during the Australian flood was maximally developed and the South Pacific high was shifted considerably from the coast of Peru and Chile to the center of the ocean. It is demonstrated that the maximum values of negative SST anomalies were observed not in the east of the Pacific Ocean as in the case of the "canonical" La Nina but they were shifted significantly to the west to the line of the date change. All this enables to refer the extreme La Nina 2010-2011 to La Nina of Modoki type.
机译:使用NCEP / NCAR再分析的每日数据考虑了在拉尼菲亚2010-2011年高潮期间观测到的印度洋和太平洋热带大气环流异常形成的天气机制。可以确定的是,整个澳大利亚近代史上最具破坏力的洪水是由澳大利亚夏季风环流系统中热带气旋作用的空前活动引起的。热带气旋又从印度洋通过西风赤道带系统影响了澳大利亚的季风区,并通过东部信风系统从太平洋影响了澳大利亚的季风区。澳大利亚洪水期间的太平洋贸易风得到了最大程度的发展,南太平洋的高压从秘鲁和智利的海岸转移到了海洋的中心。事实证明,在太平洋东部没有观测到负的海表温度异常的最大值,就象“经典的”拉尼娜的情况那样,但是它们明显向西移动到了日期变化线。所有这些使极端的La Nina 2010-2011可以指代Modoki类型的La Nina。

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  • 来源
    《Russian meteorology and hydrology》 |2012年第2期|p.90-97|共8页
  • 作者单位

    Lomonosov Moscow State University, GSP-1, Leninskie Gory, Moscow, 119991 Russia;

    Lomonosov Moscow State University, GSP-1, Leninskie Gory, Moscow, 119991 Russia;

    Lomonosov Moscow State University, GSP-1, Leninskie Gory, Moscow, 119991 Russia;

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