Spatial and temporal variation characteristics of ocean waves in the South China Sea during the boreal winter

ZHU Geli LIN Wantao ZHAO Sen CAO Yanhua

ZHUGeli, LINWantao, ZHAOSen, CAOYanhua. 南海冬季海浪的时空变率特征[J]. 海洋学报英文版, 2015, 34(1): 23-28. doi: 10.1007/s13131-015-0592-0
引用本文: ZHUGeli, LINWantao, ZHAOSen, CAOYanhua. 南海冬季海浪的时空变率特征[J]. 海洋学报英文版, 2015, 34(1): 23-28. doi: 10.1007/s13131-015-0592-0
ZHU Geli, LIN Wantao, ZHAO Sen, CAO Yanhua. Spatial and temporal variation characteristics of ocean waves in the South China Sea during the boreal winter[J]. Acta Oceanologica Sinica, 2015, 34(1): 23-28. doi: 10.1007/s13131-015-0592-0
Citation: ZHU Geli, LIN Wantao, ZHAO Sen, CAO Yanhua. Spatial and temporal variation characteristics of ocean waves in the South China Sea during the boreal winter[J]. Acta Oceanologica Sinica, 2015, 34(1): 23-28. doi: 10.1007/s13131-015-0592-0

南海冬季海浪的时空变率特征

doi: 10.1007/s13131-015-0592-0
基金项目: The National Basic Research Program (973 Program) of China under contract No. 2011CB403501.

Spatial and temporal variation characteristics of ocean waves in the South China Sea during the boreal winter

  • 摘要: 本文利用欧洲中尺度天气预报中心提供的高分辨率再分析数据集ERA-Interim 资料, 分析了1979/80-2011/12 冬季南海海浪的时空变率特征. 结果表明: 南海冬季有效波高的主导模态存在显著的年代际和年际变化特征(上世纪90 年代中期), 空间模态呈海盆一致模, 异常中心位于吕宋海峡西侧. 在年代际尺度上, 有效波高从负位相转变为正位相主要受太平洋十年涛动(PdO)对东亚冬季风的调制作用影响;年代际尺度上, 波高变率与前秋和同期的 ENSO有很显著的负相关. 为了更好地探究南海海浪与ENSO 的物理机制, 我们进一步对环流场做了相应分析, 证明了 ENSO 通过南海冬季风和对流层底层的太平洋-东亚遥相关影响南海海浪. 在 El Niño(La Niña)年, 西太平洋被菲律宾海的异常反气旋(气旋)覆盖, 削弱(增强)了东亚冬季风从而导致南海海浪异常偏低(偏高).
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出版历程
  • 收稿日期:  2014-04-09
  • 修回日期:  2014-07-04

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