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Seasonal variability of turbulent heat fluxes in the tropical Atlantic Ocean based on WHOI flux product
作者姓名:JIANG Hu  WANG Hui  WU Dexing
作者单位:JIANG Hua1,WANG Hui1,WU Dexing21.Institute of Climate System,Chinese Academy of Meteorological Sciences,Beijing 100081,China 2.Institute of Physical Oceanography,Ocean University of China,Qingdao 266003,China
基金项目:国家自然科学基金 , 国家高技术研究发展计划(863计划)
摘    要:The mean seasonal variability of turbulent heat fluxes in the tropical Atlantic Ocean is examined using the Woods Hole Oceanographic Institution(WHOI) flux product.The most turbulent heat fluxes occur during winter seasons in the two hemispheres,whose centers are located at 10°~20°N and 5°~15°S respectively.In climatological ITCZ,the turbulent heat fluxes are the greatest from June to August,and in equatorial cold tongue the turbulent heat fluxes are the greatest from March to May.Seasonal variability of sensible heat flux is smaller than that of latent heat flux and mainly is dominated by the variations of air-sea temperature difference.In the region with larger climatological mean wind speed(air-sea humidity difference),the variations of air-sea humidity difference(wind speed) dominate the variability of latent heat flux.The characteristics of turbulent heat flux yielded from theory analysis and WHOI dataset is consistent in physics which turns out that WHOI's flux data are pretty reliable in the tropical Atlantic Ocean.

关 键 词:季节性变异  湍流  海洋科学  热带气候
收稿时间:1/5/2007 12:00:00 AM
修稿时间:2007-01-052007-05-18

Seasonal variability of turbulent heat fluxes in the tropical Atlantic Ocean based on WHOI flux product
JIANG Hu,WANG Hui,WU Dexing.Seasonal variability of turbulent heat fluxes in the tropical Atlantic Ocean based on WHOI flux product[J].Acta Oceanologica Sinica,2007,26(5):1-11.
Authors:JIANG Hu  WANG Hui and WU Dexing
Institution:1.Institute of Climate System, Chinese Academy of Meteorological Sciences, Beijing 100081, China2.Institute of Physical Oceanography, Ocean University of China, Qingdao 266003, China
Abstract:The mean seasonal variability of turbulent heat fluxes in the tropical Atlantic Ocean is examined using the Woods Hole Oceanographic Institution (WHOI) flux product. The most turbulent heat fluxes occur during winter seasons in the two hemispheres, whose centers are located at 10°~20°N and 5°~15°S respectively. In climatological ITCZ, the turbulent heat fluxes are the greatest from June to August, and in equatorial cold tongue the turbulent heat fluxes are the greatest from March to May. Seasonal variability of sensible heat flux is smaller than that of latent heat flux and mainly is dominated by the variations of air-sea temperature difference. In the region with larger climatological mean wind speed (air-sea humidity difference), the variations of air-sea humidity difference (wind speed) dominate the variability of latent heat flux. The characteristics of turbulent heat flux yielded from theory analysis and WHOI dataset is consistent in physics which turns out that WHOI's flux data are pretty reliable in the tropical Atlantic Ocean.
Keywords:turbulent heat fluxes  seasonal variation  tropical Atlantic
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