台湾海峡及邻近海域海面热量平衡分布特征  

Feature of heat budget at sea surface 0f Taiwan Strait and its adjacent waters

作　　者：陈义斌[1] 蔡淑惠[1] 

机构地区：[1]国家海洋局第三海洋研究所,厦门361005

出　　处：《台湾海峡》1990年第1期1-7,共7页Journal of Oceanography In Taiwan Strait

摘　　要：本文利用1961—1985年历次台湾海峡及邻近海域水文气象调查资料,计算分析了该海域海面吸收辐射、有效回辐射、蒸发耗热、海-气感热交换的时空分布,给出了该海域热量平衡年平均状况和季节变化特征。Based mainly on the hydrometeorogical data from the investigations in the period from 1961 to 1985,this paper computes and analyses the components of the sea surface heat budget in the Taiwan Strait and its adjacent areas. The annual mean features and seasonal and spatial variation of heat budget in this area are discussed. The results show that (1)due to the influences of the warm currents of the South China Sea Current and the Kuroshio, the heat transfer from the ocean to the atmosphere appears maximumly in the central zone of the Strait and waters to the east of the Taiwan Island where the contribution of the latent heat is most obvious ,and minimumly in the coastal waters of Fujian and Zhejiang; (2)the components of the heat budget show remarkable seasonal variations; (3)remarkable differences exist between the variations in the eastern and western waters of the Taiwan Island. Under greater effects of the warm currents,the eastern waters has greater heat dissipation than that in the western waters.

关 键 词：海面 热量 平衡分布 海域 台湾海峡 

分 类 号：P731.23[天文地球—海洋科学]