在风的作用下，地表上部空气的强制对流和表土层中的水分蒸发大大增强，对冻土层的热状况产生重要的影响。
Under the action of wind, forced convection of air above ground and water evaporation of top soil layer will be greatly enhanced.
这是由于全球变暖中对流层静力稳定度的增强，与IOD模态相关的纬向风异常减弱。
The zonal wind anomalies associated IOD are found to weaken, likely due to increased static stability of the troposphere from global warming.
应用推荐