从工业革命以来全球有了一个较长期的增暖，全球地面平均气温也具有一种年代际变化，在这种长期趋势以及年代际变化的叠加影响之下，表现出来的全球气温在某些年份增暖相对停滞（hiatus）或者增暖相对较快（accelerated warming）。通过分析三次全球年代际变暖加速与停滞时期的增暖趋势，我们发现增暖趋势与其时间段内的温室气体排放量有很高的相关性。分析了在三次变暖加速停滞时期的东亚冬季风指数的变化，发现三次停滞时期东亚冬季风指数都有明显的下降趋势。通过全球年代际变暖加速和停滞时期的大气与海洋环流变化分析，在变暖停滞的时期，全球海洋表面温度下降，在变暖加速时期，全球大部分海洋的表面温度上升。而这种年代际变化主要是由于副热带—热带经圈环流导致。这一过程，主要起作用的是海洋环流的差异。例如：赤道信风在拉马德雷太平洋十年涛动背景下的（PDO）加强，造成的太平洋表面海洋在赤道附近与西大西洋的增暖，以及在与之相对的东太平洋的变冷，因此造成的水平运动导致为了构成一个完整的循环产生垂直方向的运动，即海洋热量的深层运动，也就是全球的热量的一个重新分布。

Global average air temperature have a longtime warming trend from industrial revolution, and global average air temperature have shown a decadal variability. Under the change of longtime warming trend and the decadal variability, the global air temperature in some periods were decadal accelerated warming, and in other periods they were warming hiatus. We analyses the warming trend in accelerated warming decades and hiatus decades, we find relativity between in global warming gas and warming trend in that period. Analyzing the ocean circulation difference during warming’s decadal accelerated warming and hiatus period, we find that SST reduced in hiatus and increased in accelerated warming decades. Along the research, we find the reason is subtropical tropical meridional cells. For example, under the background of the PDO, the tropical trend wind strengthen, causing the warming sea surface temperature in tropical regions and west of Atlantic ocean. And the cool in east Atlantic ocean. For a full recycle of the ocean circulation, the ocean cause a horizontal trend lead to the warming of the deeper sea.