大气中各种天气现象和物理过程发生的主要能源,均来自太阳辐射,而进入地球大气的太阳辐射却只有一小部分(约19％)被大气直接吸收,大部分(约51％)为地球表面特别是占地表约71％的海洋吸收,然后再以各种形式加热大气,推动大气运动,形成各种天气和气候。 西北太平洋辐射平衡的时空分布特征的研究,是西北太平洋辐射平衡、热量平衡及海 All kinds of weather phenomena in the atmosphere and the main energy sources in physical processes come from solar radiation, while only a small part (about 19%) of the solar radiation entering the earth’s atmosphere is directly absorbed by the atmosphere and the majority (about 51%) is Earth The surface absorbs, in particular, about 71% of the ocean’s surface and then heats the atmosphere in various forms to promote atmospheric movement and create a variety of weather and climate. The research on the spatio-temporal distribution of the radiation balance in the Northwest Pacific is the balance of the radiation and heat balance in the Northwest Pacific and the sea