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热带海洋对大气的显热和潜热供应的计算,越来越受到人们的注意,这是因为它不仅对热带环境本身,而且对全球大气环流的状态和变化计算都有直接关系。70年代进行的气团变性实验(AMTEX),主要是研究这个问题。在热通量计算方法方面,目前还存在一些问题,我们知道,大气中热量的输送,是由大气中微尺度的湍流运动和小尺度的积云对流完成的,显然,应用湍流通量法计算为
The calculation of the sensible and latent heat supplies to the atmosphere in the tropical oceans is drawing more and more attention because it is directly related not only to the tropical environment itself but also to the state and changes in the global atmospheric circulation. The air mass degeneration experiment (AMTEX) conducted in the 1970s mainly studied this issue. In terms of heat flux calculation methods, there are still some problems. We know that the transport of heat in the atmosphere is carried out by the micro-scale turbulence in the atmosphere and the small-scale cumulus convection. Obviously, the application of the turbulent flux method for