南北两半球大气的相互作用和季风的本质分析  

Interaction of Atmosphere in the North and South Hemisphere and the Essence of the Monsoon

作　　者：李智明[1] 

机构地区：[1]海南师范大学地理与环境科学学院,海南海口571158

出　　处：《时代农机》2017年第2期173-174,共2页Times Agricultural Machinery

摘　　要：根据相关的研究资料显示:大气环流的季节性变化以及越赤道气流即两半球的相互作用。而行星热对于流环流是作为热带季风到来的"主要推动力之一",而由于地球表面各种特性之间的差异化,在很大程度上致使于准定常行星波作为第二推动力。如果针对于推动整个大气质量以及跨维圈传输的效率水平上来分析,总体上两个推动力的功效比率占位2:1。而第二推动力也在整个亚欧季风区与第一推动力进行融合,这样在很大程度上使热带季风气候在全球的亚欧地区最为明显。According to the relevant research data,it is shown that the seasonal variation of atmospheric circulation and the interaction between the two hemispheres.The planetary heat is the ＂main driving force＂ for the arrival of the tropical monsoon,and the difference between the various characteristics of the Earth＇s surface,to a large extent,causes the quasi-stationary planetary wave as the second driving force.If it analyzes from the overall level of efficiency and the efficiency of the transmission of the cross-dimensional circle,the efficiency ratio of the two driving forces is 2：1.And the second driving force is also in the entire Asia-Europe monsoon region with the first driving force to integrate,to a large extent the tropical monsoon climate becomes most obvious in Asia-Europe region in the world.

关 键 词：南北半球 大气作用 季风本质 推动力 

分 类 号：F301[经济管理—产业经济]