• In the troposphere, the air at higher altitudes is in general cooler than the air below it.

    对流层中,海拔地区空气通常低海拔地区的空气

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  • Troposphere delay error could be accurately determined using WVR.

    使用WVR精确测定对流层时延误差

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  • This means that the stratosphere and troposphere are close related.

    意味着平流层对流层之间紧密相关的。

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

    必须通过对流层顶的输送来建立平衡

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

    其上对流层顶,对流层上部边界

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  • The mission will also observe clouds and aerosol particles in the troposphere.

    此次任务观测对流层中的云和气溶胶粒子

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

    此外,模式真实再现了对流层高层行星季风

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  • When they re-enter the troposphere, they are rapidly washed out of the atmosphere by rain and snow.

    重新回到对流层时,它们很快大气中形成雨雪所洗刷殆尽。

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  • The pollutants such as nuclear explosions, in the stratosphere than in the troposphere lot more.

    核爆炸产生污染物平流层对流层很多。

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  • Because of the above reasons stratospheric more easily than the troposphere by chemical pollution.

    由于上述原因平流层对流层容易化学污染影响

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  • Above the troposphere is the stratosphere, followed by the ionosphere and capped by the exosphere.

    对流层平流层接着是电离层上层是外逸层。

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  • Methane as an important green house gas, its concentration in the global troposphere is increasing.

    甲烷作为重要温室气体大气中的浓度正在增加。

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  • 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焦点问题。

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  • Deep oranges and yellows appear in the troposphere, which extends from the Earth’s surface to 620 km high.

    大气层呈现出厚重的颜色各种黄色这些颜色地球表面延伸620千米高空。

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  • The orange layer is known as the troposphere, where all of the weather and clouds are generated and contained.

    橘黄色一层称为“对流层”,那里所有气候状况云层形成和演变的地方。

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  • Weather as we know it also takes place in the troposphere, with the rising and falling of air through convection.

    天气我们所知道发生对流层地方,在上升下降通过空气对流

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  • 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

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  • 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高度增加不断地减小的。

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  • The dynamic response to the heating imbalance is such as to converge heat into the upper troposphere of the desert regions.

    加热不平衡动力学响应结果导致沙漠地带对流层上部辐合。

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  • 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气溶胶粒子平流层碰并要大于对流层中的碰并率。

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  • The pressure at the top of the troposphere is only 10% of that at sea level and above this layer the pressure continues to drop.

    对流层顶部压力只有10%,在海平面以上一层压力继续下降

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  • However because of the refraction effect in the troposphere there is refractive error in the parameters measured in positioning system.

    由于对流层中的折射效应定位系统目标的仰角、距离等参量存在一定的折射误差

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  • At the beginning of the 20th century, Nikola Tesla proposed using huge coils to transmit electricity through the troposphere to power homes.

    20世纪,尼古拉·特斯拉提出利用巨型线圈通过大气对流层输送千家万户。

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  • The seasonal reversal of wind field from the upper troposphere to the stratosphere is as pronounced as in the middle and lower troposphere.

    东亚对流层上部平流层中下部季节变化,对流层中下部一样显著

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  • Tropospherethe atmosphere which is closet to the earth. Its depth ranges from about 10 miles over the equator to about 5miles over the poles.

    对流层——接近地表大气层距赤道深度超过10英里两极超过5英里。

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  • Atmosphere Refraction, Troposphere Delay, Ionosphere Delay, Local Atmosphere Mode, Atmosphere Predictive Mode, Corrective Grid of Electron Content.

    大气折射对流层延迟电离层延迟,局部大气模式,大气预报模式,电子含量格网改正

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  • In the convectively heating region latent heat release causes a heating peak in the upper troposphere and a moisture sink in the lower troposphere.

    对流加热,大量的潜热释放形成深厚的热源水汽,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;

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  • In the convectively heating region latent heat release causes a heating peak in the upper troposphere and a moisture sink in the lower troposphere.

    对流加热,大量的潜热释放形成深厚的热源水汽,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;

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