troposphere

美 ['tr?p?sf??(r)] 　英 ['tr?p?sf??(r)]

• n.對流層（大氣的最低層，在地球表面和 6 至 10 公里上空之間）
• 網絡對流圈；對流層頂；對零

英漢雙解

英漢解釋

n.

1. 【氣】對流層

英英解釋

n.	1. the lowest and most dense layer of the atmosphere, extending 10 to 20 km (6 to 12 mi), in which temperature decreases with rising altitude and most weather occurs

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.

在對流層的頂部壓力，只有10%，在海平面以上這一層的壓力繼續(xù)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.

對流層是人類的家園。我們直接生活在對流層的底部，一切天氣現(xiàn)象均發(fā)生在此層。

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世紀初，尼古拉·特斯拉就提出利用巨型線圈，通過大氣對流層將電輸送到千家萬戶。

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

對流層與藍色大氣中的其余部分之間的分界線，稱為對流層頂（tropopause）。

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

由里向外分別為太陽核反應區(qū)、太陽對流層、太陽大氣層。

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

橘黃色的那一層被稱為“對流層”，那里是所有的氣候狀況和云層形成和演變的地方。

The stratosphere begins about 12 kilometres up, above the troposphere where weather systems like the monsoon develop.

平流層大約從距離地面12公里開始，天氣系統(tǒng)例如季風通常在對流層上發(fā)生。

As a rule, the temperature in the troposphere decreases steadily with increasing altitude until the tropopause is reached.

通常對流層溫度直到對流層頂都是隨高度增加而不斷地減小的。

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

OH自由基引發(fā)的乙烷降解反應可能是對流層大氣H2O2，MHP及EHP的重要來源之一。

The rest is in the stratosphere, from the top of the troposphere to an altitude of 50 kilometers.

其余的臭氧在離對流層頂部至50公里高度的同溫層里。

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

對平流層PV分布的大尺度調整能描述平流層對對流層的動力學影響嗎？。

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

當重新回到對流層時，它們將很快被大氣中形成的雨雪所洗刷殆盡。

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

必須通過對流層頂的熱輸送來建立平衡。

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

長波輻射造成的對流層中、上層大氣的冷卻則主要由深對流潛熱釋放來補償。

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

STE可以影響溫室氣體在上對流層和下平流層中的垂直分布，進而影響氣候。

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

對流層低層水汽通量輻合加強，是東北地區(qū)降水的重要水汽條件；

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

在對流層上是平流層，接著是電離層，最上層是外逸層。

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

沙塵暴期間，對流層高層大值位渦下傳現(xiàn)象十分明顯。

the resulting colder stratosphere emits less long-wave radiation downward, thus cooling the troposphere.

這就使得較冷的平流層向下釋放較少的長波輻射，從而冷卻了對流層。

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

對流層在大氣層的最低層，緊靠地球表面，其厚度大約為10至20千米。

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

空間過渡到橙色的對流層（troposphere）——地球上大氣層的最低部分。

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

N附近對流層中、上層為輻散，從而引起緯向平均西風在60？。

Rossby Wave Breaking in the Southern Hemisphere Wintertime Upper Troposphere.

冬季南半球對流層上層羅斯貝波爆發(fā)。

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

此外，模式也真實再現(xiàn)了對流層高層的行星季風。

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

熱帶對流層高層水氣反饋：模式結果和觀測。

The role of heterogeneous reactions and procedure in the troposphere are assessed strictly.

嚴格地評審了對流層中的異性反應與過程的作用。

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

對流層氧氣含量高。它并不穩(wěn)定，混亂無序，無法預測。然而，生命卻依賴它。

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

而夏季這種形態(tài)明顯減弱，并只限于對流層中。

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

有重要的證據(jù)表明，在對流層上部和平流層有狹窄強勁的氣流存在。

Winter and spring to the upper troposphere, almost no water vapor.

冬季和春季到對流層上層基本無水汽。

HF ultimately diffuses down to the troposphere where it is removed by wet deposition.

HF最終擴散到大氣中，在大氣中它通過濕沉積被除去。

In the ENSO cold phase, because the Siberian ridge in upper troposphere strengthens, the Siberian high strengthens in lower troposphere.

冷事件時，上對流層的東亞主槽會減弱并往西南偏移，西伯利亞脊以及阿拉斯加脊都會增強。

Hopflied troposphere model and accurate troposphere model in radio wave refraction error modify in troposphere are gived.

給出了對流層電波折射誤差修正應用中的霍普菲爾德大氣模型和精確大氣模型。

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

對這一加熱不平衡的動力學響應結果導致熱在這沙漠地帶的對流層上部輻合。

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

由于上述原因平流層比對流層更容易被化學污染影響。

Above the troposphere, some 30 miles (48 kilometers) above the Earth's surface, is the stratosphere.

在對流層之上，離地大約30英里（48公里）的地方，是平流層（同溫層）。

About 10 percent of ozone is in the troposphere, from the Earth's surface upward 10 kilometers to 16 kilometers.

約10%的臭氧是在離地球表面上空10至16公里的對流層中。

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

如核爆炸產生的污染物，在平流層中比對流層中多很多。

A Simulation Study of Stratosphere-Troposphere Exchange due to Cut-off-low over Eastern Asia

東亞地區(qū)一次切斷低壓引起的平流層、對流層交換數(shù)值模擬研究

Persistence of a Kelvin-Helmholtz instability complex in the upper troposphere

上部對流層開爾溫-赫爾姆霍次不穩(wěn)定聯(lián)合體的維持