troposphere

英音[ ˈtrɒpəsfɪə(r) ] 美音[ ˈtroʊpəsfɪr ]
对流层
常用释义
n. 对流层

扩展信息

对流层
对字的解释---在线新华字典 ... 对流〖 convection〗 对流层troposphere〗 对路〖 satisfytheneed〗 ...
对流圈
对流圈troposphere) 大气圈底部对流运动最显著,集中了整个大气质量的 3/4 和几乎全部水汽。对流层之上 的平流层、中 …
对流层顶
喷射气流是处於地球大气对流层顶Troposphere)的一条宽度不大的快速气流,通常出现於来自北极的冷气团与南方暖气团的 …
对零
农业词汇英语翻译(O-T) ... tropism 向性 troposphere 对零 true forget menot 勿忘草 ...
对流层选项卡
对流层选项卡Troposphere)中选取Niell(2005)等对流层模型, 然后敲击回车确认即可。 1 2 3 4 基线解算-构造基线解 …
中对流层
我的问题是,像下图中对流层Troposphere)之上有一层很厚的区域,温度没有随著高度而升高或降低,让我无从判断这个区 …

例句

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。

The troposphere is the human home. We live directly in the bottom of the troposphere, and all weather phenomenon takes place on story here.

对流层是人类的家园。我们直接生活在对流层的底部,一切天气现象均发生在此层。

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。

The line between the troposphere and the rest of the blue-colored atmosphere is called the tropopause.

对流层与蓝色大气中的其余部分之间的分界线,称为对流层顶(tropopause)。

From the outside in the sun for a nuclear reaction zone, the troposphere the sun, the sun's atmosphere.

由里向外分别为太阳核反应区、太阳对流层、太阳大气层。

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。

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 OH radical initiated degradation of ethane was possibly one of the main sources of H2O2, MHP and EHP in the troposphere.

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。

其余的臭氧在离对流层顶部至50公里高度的同温层里。

Can the dynamical impact of the stratosphere on the troposphere be described by large-scale adjustment to the stratospheric PV distribution?

对平流层PV分布的大尺度调整能描述平流层对对流层的动力学影响吗?。

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 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。

Latent heat release accompanying deep convection is critical in offsetting longwave radiative cooling in the middle and upper troposphere.

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。

STE may affect climate by altering the vertical distributions of greenhouse gases in the upper troposphere and low stratosphere.

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。

The enhancement of moisture flux convergence in lower layers of troposphere is a favorable condition for rainfall in Northeast China.

对流层低层水汽通量辐合加强,是东北地区降水的重要水汽条件;

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。

during the sand - dust storm , the high pv spreads evidently downward from the upper troposphere.

沙尘暴期间,对流层高层大值位涡下传现象十分明显。

这就使得较冷的平流层向下释放较少的长波辐射,从而冷却了对流层。

Troposphere the lowest level in the atmosphere, close to the Earth's surface, the thickness of approximately 10-20 kilometres.

对流层在大气层的最低层,紧靠地球表面,其厚度大约为10至20千米。

Space transitions into the orange-colored troposphere, the lowest portion of Earth's atmosphere.

空间过渡到橙色的对流层(troposphere)——地球上大气层的最低部分。

N, respectively. Thus, the zonal mean wind was weakened in the upper troposphere and the stratosphere over the region about 60?

N附近对流层中、上层为辐散,从而引起纬向平均西风在60?。

Rossby Wave Breaking in the Southern Hemisphere Wintertime Upper Troposphere.

冬季南半球对流层上层罗斯贝波爆发。

此外,模式也真实再现了对流层高层的行星季风。

Water Vapor Feedback in the Tropical Upper Troposphere: Model Results and Observations.

热带对流层高层水气反馈:模式结果和观测。

严格地评审了对流层中的异性反应与过程的作用。

The troposphere is a rich soup of oxygen rich air. It is unstable, chaotic, and unpredictable. but life depends upon it.

对流层氧气含量高。它并不稳定,混乱无序,无法预测。然而,生命却依赖它。

In summertime this dipolar pattern weakens to great extent and limits in the bound of troposphere.

而夏季这种形态明显减弱,并只限于对流层中。

There is strong evidence that vigorous narrow current is observed in the upper troposphere and stratosphere.

有重要的证据表明,在对流层上部和平流层有狭窄强劲的气流存在。

冬季和春季到对流层上层基本无水汽。