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北太平洋局地海洋-大气相互作用的主模态
  • 期刊名称：中国海洋大学学报(自然科学版)
  • 时间：0
  • 页码：10-14
  • 分类：P732.6[天文地球—海洋科学]
  • 作者机构：[1]中国海洋大学物理海洋实验室,海洋-大气相互作用实验室,山东青岛266003
  • 相关基金：国家自然科学基金项目（40830106,40921004）;国家重点基础发展计划项目（2007CB411803,2010CB428904）资助 致谢：感谢得克萨斯A＆M大学张平老师提供的模式数据,感谢中国科学院海洋研究所王法明研究员对此工作的指导.
  • 相关项目：北太平洋中纬度海洋-大气耦合系统近50年演变特征与机制
作者： 郭建民|刘秦玉|
关键词： 北太平洋, 海洋-大气耦合模式, 主模态, 海表温度异常, the North Pacific, coupled ocean-atmosphere model, dominate mode, sea surface temperature anomalies
中文摘要：

本文分析美国国家大气研究中心（NCAR）的CCM3-ML耦合模式100a积分模拟结果，依据对该模式结果中SSTA与海面风异常的最大协方差分析，证实的确存在北太平洋局地大气影响海洋和海洋“反馈”大气的主模态；指出通过局地海洋一大气的相互作用，冬季马蹄型海温异常可以持续到夏季，冬季大气对马蹄形暖海温异常可能的响应为高压异常，春夏季对马蹄形暖海温异常可能的响应为低压异常。

英文摘要：

By using NCAR CCM3-ML coupled model result （one hundred year）, based on Maximum Co- variance Analysis between the monthly sea surface temperature anomaly （SSTA） and the sea surface wind anomaly, the dominate modes of local atmosphere influences ocean and ocean feedbacks on atmosphere in North Pacific are confirmed to exist;It is indicated that horseshoe SSTA pattern in winter can persist to summer through local atmosphere-ocean interaction. The atmosphere response to the horseshoe SSTA is warm/high in winter and warm/surface low in spring and summer in North Pacific.

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