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南极涛动
释义
南极涛动
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理学
大气活动中心
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Southern Oscillation
南极涛动
东南太平洋与印度洋及印度尼西亚地区的海平面气压升降呈反相变化。20世纪20年代,英国气象学家G.沃克(Gilbert Walker,1868~1958)在研究印度季风雨的预报时发现,东南太平洋与印度洋及印度尼西亚地区台站观测的海平面气压升降呈反相变化,命名为南方涛动。
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