平流层和对流层环流的相互作用及其与季风建立的关系很值得进一步研究。
The interactions between stratospheric and the tropospheric circulations and their relation to the onset of monsoons need further investigation.
近年来，科学家们对关于平流层平均风可能对对流层环流具有的影响产生了进一步的兴趣。
Recently there has been some renewed interest in the influence that the stratospheric mean wind may have on the tropospheric circulation.
一些学者已通过平流层和对流层耦合机制的研究探索极涡变化对低层环流的作用。
The mechanisms coupling the stratosphere and troposphere have been studied by some scientists for understanding the effect of the polar vortex change on the lower circulation.
对流层中低层的暖脊和地面均压场的维持是此次大雾形成的良好环流背景。
The warm high ridge at the middle and low troposphere and the lower pressure of the ground all provide the good circulation background of this heavy fog.
这种环流中心与云团的相对位置关系和对流层上部的环境流场密切相关。
The position of the circulation center relative to a deep convective cloud cluster is associated with the upper tropospheric environmental flow.
气旋性环流和气旋性涡度在对流层中层的700毫巴附近最强。
The strongest cyclonic circulation and vorticity are at about 700 mb.
这些机制可以大致说明一些爆发性增温期间平流层和对流层大气环流出现异常以及随后又恢复到正常冬季环流的过程。
These mechanisms can largely explain occurring of abnormal circulation in the stratosphere and troposphere during stratospheric sudden warming and returning then to normal regime.
中平流层环流转型与对流层重要系统(极涡、西太平洋副热带高压)存在一定关系。
The relation between the transition dates in middle stratosphere and the important systems in troposphere such as polar vortex and the subtropical high in West Pacific.
青藏高原东北侧地区夏季各月降水量同对流层、平流层前期环流特征之间存在明显的统计相关。
There exists distinct statistical relationship between precipitation of each summer month and prophase atmosphere general circulation introposphere and low stratosphere.
分析大气监测资料、TOMS臭氧总量资料和NCEP大气环流资料表明，大气臭氧总量随着对流层顶的低一高一低变化呈高一低一高的变化过程。
Analysis of the observational data, the TOMS total ozone, and NCEP circulation, shows that the atmospheric ozone amount experienced a high-low-high variation with low-high-low tropopause altitude.
分析大气监测资料、TOMS臭氧总量资料和NCEP大气环流资料表明，大气臭氧总量随着对流层顶的低一高一低变化呈高一低一高的变化过程。
Analysis of the observational data, the TOMS total ozone, and NCEP circulation, shows that the atmospheric ozone amount experienced a high-low-high variation with low-high-low tropopause altitude.
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