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中文摘要: 本文根据1986年2月8—14日中国“向阳红14号”考察船以及其它的船泊水文气象观测资料,计算了西太平洋热带海面(140—160°E、18°S—14°N)的能量收支各分量。计算结果表明,这个期间内该海面所获得的热量净收入的大小与赤道辐合带低值系统的增强或减弱有关;海面向大气输送的热量主要是以潜热通量输送方式进行的;考察海域内相当部分海面,供给大气能量大于它从大气接收的能量,其中最明显的地区出现在西太平洋热带地区(10°N附近),而不是在赤道地区。
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Abstract:The marine meteorological data collected with the vessel "Xiangyanghong No. 14, China" and other ships have been used in this study to evaluate net radiation, latent and sensible heat exchanges, and the net heat gain by the sea surface. It is shown that the measure of the net heat gain by the sea surface is related to the increase and reduction of the Equatorical Convergence Zone. Meanwhile, the heat fluxes transfer from sea surface to atmosphere would be by means of the latent heat.This study has also emphasized that the supporting atmosphere energy from sea surface may take place on the tropical zone of the West Pacific (by 10 °N) rather than on the equatorical zone during this investigation, February 8-14, 1986.
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引用文本：
李月洪,李维亮,1987.热带西太平洋海面的热量收支——中美西太平洋海-气合作考察观测事实之三[J].气象,13(7):19-22.
,1987.A survey of heat budget on the West Tropical Pacific[J].Meteor Mon,13(7):19-22.
李月洪,李维亮,1987.热带西太平洋海面的热量收支——中美西太平洋海-气合作考察观测事实之三[J].气象,13(7):19-22.
,1987.A survey of heat budget on the West Tropical Pacific[J].Meteor Mon,13(7):19-22.