• 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。

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  • Troposphere delay error could be accurately determined using WVR.

    使用WVR能精确测定对流层时延误差。

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  • 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。

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  • 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。

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  • 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。

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  • 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。

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  • 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。

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  • 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。

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

    甲烷作为重要的温室气体,它在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的焦点问题。

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  • Deep oranges and yellows appear in the troposphere, which extends from the Earth’s surface to 6–20 km high.

    大气层呈现出厚重的颜色和各种黄色,这些颜色从地球表面延伸到6至20千米的高空。

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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。

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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是随高度增加而不断地减小的。

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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.

    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。

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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,对于重力占优的气溶胶粒子,平流层中碰并率要大于对流层中的碰并率。

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  • 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。

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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.

    在对流层的顶部压力,只有10%,在海平面以上这一层的压力继续下降。

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

    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。

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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.

    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。

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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。

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  • Troposphere — the 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——接近地表的大气层。它的距赤道深度超过10英里距两极超过5英里。

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  • 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。

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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.

    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;

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  • 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。

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  • The image was made with data collected by the Measurements of Pollution in the Troposphere (MOPITT) instrument during the week of May 16 through May 23, 2010.

    这张图由在2010年5月16日- 23日对流污染测量仪所收集的数据而做出来的。

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  • Or it may be, as others have suggested in the past, that the long-term trend, as the troposphere warms up, will be to a wetter, more warming lower stratosphere, too.

    也可能像前人建议的,当对流层温度升高,长期起来会形成一个湿度更大、温度更高、高度更低的平流层。

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  • Or it may be, as others have suggested in the past, that the long-term trend, as the troposphere warms up, will be to a wetter, more warming lower stratosphere, too.

    也可能像前人建议的,当对流层温度升高,长期起来会形成一个湿度更大、温度更高、高度更低的平流层。

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