北极冰异常对亚洲夏季风影响的数值模拟
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摘要: 本文利用菱形截断15波的9层全球大气环流谱模式研究了北极关键区域海冰面积异常对亚洲夏季风环流、降雨量及我国夏季天气气候的影响,结果表明,格陵兰海-巴伦支海极冰偏多,导致亚洲夏季风环流特别是东亚季风环流的增强、我国东南部降水偏多;东西伯利亚海-波弗特海极冰偏多,导致东亚夏季风环流减弱、我国东南部降水偏少,而印度半岛季风增强;该区极冰偏少引起相反的效应。文中对上述效应的可能动力学机制也进行了讨论。因此,北极冰是引起亚洲夏季风年际气候异常的重要原因之一。
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Rasmusaon E M and T H Carpenter.The relation between eastern equatorial Pacific sea surface temperatures and rainfall over India and Sri Lanka.Mon,Wea.Rev,,1983,111,517-528 Krishnamurti T N and N Surgi,Observational aspects of summer monsoon.Monsoon Meteorology,Oxford Univ.Press,1987,3-25 Keshavamurty R N.Response of the atmosphere to sea-surface temperature anomalies over the equatorial Pacific and the teleconnections of the Southern Oscillation.J.Atmos.Sci,,1982,38,1241-1269 Shukla J.Interannual variability of the monsoons,Monsoon,1987,399-463 Gadgil S.Recent advances in monsoon research with particular reference to the Indian monsoon.Aust.Meteor.Mag,,1988,36.193-204 -
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