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中太平洋西部赤道附近地处低纬,属热带海洋区域,温度高,蒸发量大,是地球大气中水分和热量的主要源地之一。由于热带天气的变化,对推动和调整全球大气环流具有很大的作用和影响,而热通量变化是被看作海洋-大气间的反馈过程中重要的一个过程。海气界面热量交换是剖析海气相互作用机制的一个重要环节。就海气界面热量交换而言,许多作者已经作了大量研究。但对中太平洋西部海区来说,研究尚少。本文,拟就中太平洋西部赤道附近产生的天气与海气热交换关系进行初步分析。
Near the equator in the western Pacific Ocean is located in the low latitude, which belongs to tropical marine areas. It is one of the main sources of water and heat in the earth’s atmosphere due to its high temperature and large evaporation. Due to the change of the tropical climate, it has a great effect on the promotion and adjustment of the global atmospheric circulation. The change of heat flux is regarded as an important process in the ocean-atmosphere feedback. The exchange of heat in the air-sea interface is an important part of analyzing the mechanism of air-sea interaction. In terms of heat exchange at the air-sea interface, many authors have done a great deal of research. However, there are few studies on the western Pacific Ocean. This article intends to conduct a preliminary analysis of the relationship between the weather and the sea-air heat exchange generated in the equatorial Pacific in the western Pacific.