潜热释放时,水蒸气变成液态、固态水。所以潜热释放哪里有降水。所以你主要看地方有很多湿对流……赤道附近的ITCZ然后是情理之中。我相信所有的潜热释放高空应该意味着更多的热量移向极在高层大气中分支的全球环流会感动对流干燥。因此提高流通效率,也许有长期影响的允许减少水平风力大小相比,干燥的世界(不稳定产生的减少意味着较弱的上升气流和更好的运输向极意味着更小的温度\压力失衡,因此风力小于一个没有水分的世界)。我不知道文献…谷歌学术搜索帮助虽然你遇到很多气候模型参数化的文章使用大多数术语。[全球大气循环)的性质(http://eaps4.mit.edu/research/Lorenz/Nature_of_the_Global_Circulation_1969.pdf)应该相当坚定,洛伦兹是相当大的我相信。谈到如何潜热在热带地区提高了上升气流风在ITCZ 17页小一点。 The paper seems to suggest it would increase the global circulation strength by increasing those velocities. [Response of the Hadley Circulation to Convective Forcing in the ITCZ](http://journals.ametsoc.org/doi/abs/10.1175/1520-0469(1989)046%3C2957:ROTHCT%3E2.0.CO%3B2) looks like it might have potential too. My most successful search term set seemed to be ["global circulation" "latent heat" -simulation -co2](https://www.google.nl/search?q="global+circulation"+"latent+heat"+-simulation+-co2) though it still wasn't amazing. But probably some other good articles to find if you thumb through them. I'm certainly not a top expert in the field, but hope these thoughts and links add at least a little potential help or a starting point for you.