对流层

• In troposcatter transmission it turns out that m is of the order of magnitude of 100 to 1000
  在对流层散射通讯中已证明m在100到1000的数量级。
• During the sand - dust storm , the high pv spreads evidently downward from the upper troposphere
  沙尘暴期间，对流层高层大值位涡下传现象十分明显。
• Above the troposphere is the stratosphere , followed by the ionosphere and capped by the exosphere
  在对流层上是平流层，接着是电离层，最上层是外逸层。
• Insignificant in troposphere , dissociated in stratosphere photolysis and reaction with o
  在对流层中不易被分解，但在平流层中会被光线分解和跟o产生化学作用
• Insignificant in troposphere , dissociated in stratosphere ( photolysis and reaction with o )
  在对流层中不易被分解，但在平流层中会被光线分解和跟o产生化学作用
• Can knowledge of the state of the stratosphere be used to improve statistical forecasts of the troposphere
  平流层的状态的认识能被用来改进对流层的统计学预报吗？
• As the rise of the height , how does the temperature of troposphere and stratosphere flow change respectively
  随高度的上升，对流层和平流层的气温分别是怎样变化的？
• The ve > tical structure of such a circulation is found to be quasi - barotropic in northern spring and winter seasons
  与此相对应，在整个对流层，该环流在春/冬季呈相当正压结构。
• Temperature decreases with elevation through the troposphere at a rate , normally , of about 0 . 6 for 100 m
  在对流层，气温随高度减小，其递减率通常为每上升100米下降0 . 6左右。
• Some relation is found between the transition dates of 70hpa and the subtropical high in west pacific
  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。