由于风场以及绿洲-荒漠水热条件差异程度不同，绿洲不同站点平流出现的时间及强度不同。
Due to the discrepancy of wind field and the water vapor and heat conditions in oasis and desert, the occurrence time and intensity of advection was different at each site in oasis.
从平均对流层顶高度的年变化看来，对流层顶高度与平流层低层温度呈负相关，与对流层温度呈正相关，且存在季节差异。
From annual change of the tropopause height, it was negatively related to lower stratospheric temperature and positively associated with the troposphere temperature, and there was seasonal difference.
应用推荐