In the troposphere, the air at higher altitudes is in general cooler than the air below it.
在对流层中，高海拔地区的空气通常比低海拔地区的空气冷。
The mission will also observe clouds and aerosol particles in the troposphere.
此次任务还将观测对流层中的云和气溶胶粒子。
When they re-enter the troposphere, they are rapidly washed out of the atmosphere by rain and snow.
当重新回到对流层时，它们将很快被大气中形成的雨雪所洗刷殆尽。
The orange layer is known as the troposphere, where all of the weather and clouds are generated and contained.
橘黄色的那一层被称为“对流层”，那里是所有的气候状况和云层形成和演变的地方。
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。
Besides, the planetary monsoon in the upper 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。
In the natural air of the troposphere a suitable amount of ozone is beneficial to clean air.
在对流层大气中，适量臭氧对清洁大气是有益的。
We also use this new index to study the influence of QBO on areas in the tropical troposphere.
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。
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。
Methane as an important green house gas, its concentration in the global troposphere is increasing.
甲烷作为重要的温室气体，它在大气中的浓度正在增加。
At the same time troposphere delay is also the focus of GPS meteorology and numerical weather forecasting.
同时对流层延迟也是GPS气象学、数值天气预报所关心的焦点问题。
The stratosphere begins about 12 kilometres up, above the troposphere where weather systems like the monsoon develop.
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。
As a rule, the temperature in the troposphere decreases steadily with increasing altitude until the tropopause is reached.
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。
The dynamic response to the heating imbalance is such as to converge heat into the upper troposphere of the desert regions.
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 results show that there is larger coagulation rate of the aerosol particles in the stratosphere than in the troposphere.
结果表明，对于重力占优的气溶胶粒子，平流层中碰并率要大于对流层中的碰并率。
Atmospheric duct is one of the hot-topics and difficult problems in the propagation of electromagnetic waves in troposphere.
大气波导的影响是对流层电磁波传播研究的热点和难点问题之一。
The intensity of vorticity variability was closely related with the conditional symmetric instability in the middle-low troposphere.
而涡度变率强度与中低空的条件对称不稳定密切相关。
At the beginning of the 20th century, Nikola Tesla proposed using huge coils to transmit electricity through the troposphere to power homes.
早在20世纪初，尼古拉·特斯拉就提出利用巨型线圈，通过大气对流层将电输送到千家万户。
However because of the refraction effect in the troposphere there is refractive error in the parameters measured in positioning system.
但由于对流层中的折射效应，定位系统所测目标的仰角、距离等参量均存在一定的折射误差。
These are related with the decreasing of stratospheric ozone and temperature, as well as the rising of the troposphere in recent years.
这与近几年来，平流层内臭氧减少，温度降低，对流层高度抬升有关。
The seasonal reversal of wind field from the upper troposphere to the stratosphere is as pronounced as in the middle and lower troposphere.
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 dry PV field in the lower troposphere shows that the coupling of the dense PV isoline zone and the wind shear was formed in the storm area.
对流层低层干位涡场特征表现为，风暴区形成干位涡等值线密集区和风场切变的耦合。
Based on the regional acid deposition model (RADM), a high resolution model (EM3) for species exchange within the troposphere (TL) is designed.
在区域酸沉积模式(RADM)基础上，设计了一个高分辨对流层(TL)物质交换模式(EM3)。
Several usual models for troposphere delay and ionosphere delay are discussed and their influences to different time transfer methods are analyzed.
本文讨论了几种常用的对流层延迟和电离层延迟模型，分析了它们对各种时间比对方法的影响。
In the convectively heating region latent heat release causes a heating peak in the upper troposphere and a moisture sink in the lower troposphere.
在对流加热区，大量的潜热释放形成深厚的热源和水汽汇，热源峰值出现在上部对流层，水汽汇峰值出现在下部对流层；
Over the past decade this stormy effect seems to have been pronounced, with the coldest parts of the tropical troposphere getting about a degree colder.
过去十年里这种暴风雨的影响似乎非常明显，热带上空的对流层中最寒冷的部分温度又下降了约1度。
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.
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 downward transport of ozone due to tropopause folding can reach middle part of troposphere, which has the most influence on the ozone in the upper troposphere.
对流层顶折叠使高空臭氧向下输送，这种向下的输送可以到达对流层中部，对上对流层的臭氧影响最大。
The downward transport of ozone due to tropopause folding can reach middle part of troposphere, which has the most influence on the ozone in the upper troposphere.
对流层顶折叠使高空臭氧向下输送，这种向下的输送可以到达对流层中部，对上对流层的臭氧影响最大。
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