Seasonal variations of air-sea heat fluxes and sea surface temperature in the northwestern Pacific marginal seas

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• 作者：Na Liu (1) (4)
  Dexing Wu (2)
  Xiaopei Lin (2)
  Qingjia Meng (3) (4)
  
• 关键词：heat flux ; seasonal variations ; Kuroshio ; heat content
• 刊名：Acta Oceanologica Sinica
• 出版年：2014
• 出版时间：March 2014
• 年：2014
• 卷：33
• 期：3
• 页码：101-110
• 全文大小：790 KB
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• 作者单位：Na Liu (1) (4)
  Dexing Wu (2)
  Xiaopei Lin (2)
  Qingjia Meng (3) (4)
  
  1. Key Laboratory of Research on Marine Hazards Forecasting, National Marine Environmental Forecasting Center, State Oceanic Administration, Beijing, 100081, China
  4. LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China
  2. Physical Oceanography Laboratory, Ocean University of China, Qingdao, 266100, China
  3. State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing, 100012, China
  
• ISSN：1869-1099

文摘

Using a net surface heat flux (Q net) product obtained from the objectively analyzed air-sea fluxes (OAFlux) project and the international satellite cloud climatology project (ISCCP), and temperature from the simple ocean data assimilation (SODA), the seasonal variations of the air-sea heat fluxes in the northwestern Pacific marginal seas (NPMS) and their roles in sea surface temperature (SST) seasonality are studied. The seasonal variations of Q net, which is generally determined by the seasonal cycle of latent heat flux (LH), are in response to the advection-induced changes of SST over the Kuroshio and its extension. Two dynamic regimes are identified in the NPMS: one is the area along the Kuroshio and its extension, and the other is the area outside the Kuroshio. The oceanic thermal advection dominates the variations of SST and hence the sea-air humidity plays a primary role and explains the maximum heat losing along the Kuroshio. The heat transported by the Kuroshio leads to a longer period of heat losing over the Kuroshio and its Extension. Positive anomaly of heat content corresponds with the maximum heat loss along the Kuroshio. The oceanic advection controls the variations of heat content and hence the surface heat flux. This study will help us understand the mechanism controlling variations of the coupled ocean-atmosphere system in the NPMS. In the Kuroshio region, the ocean current controls the ocean temperature along the main stream of the Kuroshio, and at the same time, forces the air-sea fluxes.