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汉语拼音：duì liú céng

地球大气的下 层。厚度约8—18千米，随纬度和季节的不同而变化。对流层内气温随高度的增加而下降，空气升降运动 显著，云、雨、雹、雷等主要天气现象都发生在这一层里。

• H 2 O absorption is predominant in the troposphere, particularly the lower troposphere.

  H2O吸收在对流层, 特别在对流层下部起着主要作用.

• The balance must be made up by heat transported through the troposphere.

  必须通过对流层顶的热输送来建立平衡.

• Meridional heat transfer by large - scale eddies is most significant in the upper troposphere of middle latitude.

  大尺度湍涡的子午线热输送在纬度对流层上层是最重要的.

• Next comes the tropopause, which is the upper boundary of the troposphere.

  其上是对流层顶, 它是对流层的上部边界.

• Characterization and evolution of tropospheric plumes from Lascar and Villarrica volcanoes, Chile.

  来自智利Lascar和 Villarrica火山对对流层烟羽状的特征和发展.

• Chlorofluorocarbons and hydrochloroflorocarbons are oxidated in the stratosphere and troposphere respectively.

  两类物质分别在同温层和对流层氧化降解.

• Impact of monsoon circulations on the upper troposphere and lower stratosphere.

  季风环流对对流层上部和平流层下部的影响.

• As soon as the tropopause is reached, temperature stops decreasing with height.

  一达到对流层, 温度就停止随高度上升.

• Why do we say troposphere and human are in most close relations?

  为什么说,对流层与人类的关系最为密切?

• Stratospheric influences on the tropospheric seasonal cycles of nitrous oxide and chlorofluorocarbons.

  氧化一氮和chlorofluoro碳的对流层季节周期对平流层影响.

• Besides, the planetary monsoon in the troposphere is also realistically reproduced.

  此外, 模式也真实再现了对流层高层的行星季风.

• Convective generation of cirrus near the tropopause.

  对流层顶附近的对流产生的云.

• Rain is created in the troposphere.

  降雨往往是在对流层发生的.

• The tropospheric lifetime for CH 3 Cl is sufficiently long.

  CH3Cl在对流层中的寿命足够长.

• 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.