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使用WVR能精确测定对流层时延误差。Troposphere delay error could be accurately determined using WVR.

此次任务还将观测对流层中的云和气溶胶粒子。The mission will also observe clouds and aerosol particles in the troposphere.

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闪电是常见的对流层大气火花放电现象。Lightning is a common phenomenon of spark discharge of the air in the troposphere.

HF最终扩散到大气中，在大气中它通过湿沉积被除去。HF ultimately diffuses down to the troposphere where it is removed by wet deposition.

同时本文还通过新指数研究了QBO对热带对流层地区的影响。We also use this new index to study the influence of QBO on areas in the tropical troposphere.

甲烷的光化学氧化可能是大气对流层有机过氧化物的重要来源。Photooxidation of CH4 probably was an important source of organic peroxides in the troposphere.

其余的臭氧在离对流层顶部至50公里高度的同温层里。The rest is in the stratosphere, from the top of the troposphere to an altitude of 50 kilometers.

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在对流层上是平流层，接着是电离层，最。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。Above the troposphere is the stratosphere, followed by the ionosphere and capped by the exosphere.

高空动量下传促使地面气旋发展，从而使中、低层大气变得非常干燥。The air momentum down from high levels developed the cyclone and cooled the air in middle and low troposphere.

这些变化引起了局地对流层中低层大气环流的调整，进一步影响干旱气候。Thus, the low-atmospheric circulation in troposphere is changed, and the climate change in arid areas is affected.

平流层大约从距离地面12公里开始，天气系统例如季风通常在对流层上发生。The stratosphere begins about 12 kilometres up, above the troposphere where weather systems like the monsoon develop.

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通常对流层温度直到对流层顶都是随高度增加而不断地减小的。As a rule, the temperature in the troposphere decreases steadily with increasing altitude until the tropopause is reached.

对这一加热不平衡的动力学响应结果导致热在这沙漠地带的对流层上部辐合。The dynamic response to the heating imbalance is such as to converge heat into the upper troposphere of the desert regions.

OH自由基引发的乙烷降解反应可能是对流层大气H2O2，MHP及EHP的重要来源之一。The OH radical initiated degradation of ethane was possibly one of the main sources of H2O2, MHP and EHP in the troposphere.

STE可以影响温室气体在上对流层和下平流层中的垂直分布，进而影响气候。STE may affect climate by altering the vertical distributions of greenhouse gases in the upper troposphere and low stratosphere.

夏季高原地区总非绝热加热是正值，且最大加热率出现在边界层内。The overall diabatic heating is positive in the whole troposphere in summer, with the most intense heating located in the boundary layer.

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长波辐射造成的对流层中、上层大气的冷却则主要由深对流潜热释放来补偿。Latent heat release accompanying deep convection is critical in offsetting longwave radiative cooling in the middle and upper troposphere.

水汽在对流层中上层的切变线附近辐合，大降水落区与切变线相一致。Water vapor converges near shear line of upper- middle troposphere and the region of torrential rain is identical with that of shear line.

东亚对流层中上部和平流层中下部风场的季节变化，与对流层中下部一样显著。The seasonal reversal of wind field from the upper troposphere to the stratosphere is as pronounced as in the middle and lower troposphere.