?troposphere

troposphere發(fā)音

英：[?tr?p?usf??]　　美：[?trop??sf?r, ?trɑp?-]

英：　　美：

troposphere中文意思翻譯

n.對流層

troposphere詞形變化

形容詞: tropospheric |

troposphere常見(jiàn)例句

1 、Right now, the balloon's rising through the troposphere which is the lower level of the atmosphere where most of our weather happens and up near the top of that layer, that's where the jet stream runs, about 10 kilometres up.─── 現在 氣球正在穿過(guò)對流層 它是大氣層的最低層 大多數天氣現象都發(fā)生在那里 在對流層的頂部 約十千米的高空 就是急流活動(dòng)的地方

2 、Nonlinear planetary wave reflection in the troposphere───在對流層非線(xiàn)性行星波的反射曹學(xué)柱譯

3 、Chlorofluorocarbons and hydrochloroflorocarbons are oxidated in the stratosphere and troposphere respectively.───兩類(lèi)物質(zhì)分別在同溫層和對流層氧化降解。

4 、NF3 has a relatively short atmospheric lifetime (740 years) and dissociates more readily than C2F6 and CF4.HF ultimately diffuses down to the troposphere where it is removed by wet deposition.───NF3具有相對短的大氣壽命（740年），比C2F6和CF4.更容易分解。hf最終**到大氣中，在大氣中它通過(guò)濕沉積被除去。

5 、The Windows-based software, AREPS3.0, is applied to compute path loss versus range in the troposphere, using atmospheric information from shipboard weather prediction station.───使用AREPS3.0軟件計算不同距離上的路徑損耗，大氣信息取自艦載氣象站；

6 、The main impact system is cold trough on 500hPa, low eddy shear line on 700hPa, lower troposphere jet in the southwest and surface occluded front.───其主要影響系統是500hPa冷槽、700hPa低渦切變線(xiàn)、西南低空急流以及地面"錮囚鋒"。

7 、The dualDIAL with (289, 313: 277. 1. 299. 1nm) wavelengths or (268. 4, 289: 277. 1, 299. 1nm) wavelengths can be used for ozone measurement in the region, where aerosol loading is high or distribution inhomogeneous in the troposphere.───利用（289，313；277.1，299.1nm）或（268.4，289；277.1，299.1nm）4波長(cháng)進(jìn)行雙差分吸收可以用于對流層大氣氣溶膠含量豐富或分布不均勻地區臭氧的測量。

8 、Next comes the tropopause, which is the upper boundary of the troposphere.───其上是對流層頂，它是對流層的上部邊界。

9 、SOME CHARACTERISTICS OF GENERAL CIRCULATION IN LOWER TROPOSPHERE OF SOUTHERN HEMISPHERE───南半球對流層中部大氣環(huán)流的若干特點(diǎn)

10 、Signatures of stratosphere to troposphere transport near deep convective events in the southern subtropics───副熱帶南部深對流事件附近平流層輸送到對流層的信號

11 、Impact of monsoon circulations on the upper troposphere and lower stratosphere───季風(fēng)環(huán)流對對流層上部和平流層下部的影響

12 、HF ultimately diffuses down to the troposphere where it is removed by wet deposition.───HF最終**到大氣中，在大氣中它通過(guò)濕沉積被除去。

13 、The Doppler wind lidar developed by ourselves is used to measure the troposphere wind field in Hefei and the experimental datum are processed using two different methods.───利用自行研制的一臺多普勒測風(fēng)激光雷達對合肥地區對流層風(fēng)場(chǎng)進(jìn)行測量，并用兩種方法處理了實(shí)驗數據。

14 、Late-spring increase of trans-Pacific pollution transport in the upper troposphere───在對流層上部橫過(guò)太平洋污染傳輸的晚春增加

15 、Persistence of a Kelvin-Helmholtz instability complex in the upper troposphere───上部對流層開(kāi)爾溫-赫爾姆霍次不穩定聯(lián)合體的維持

16 、the atmospheric layer between the troposphere and the mesosphere───位于對流層之上中間層之下的范圍的大氣

17 、The analysis of 43-year NCEP-NCAR reanalysis data and the station observations reveals the correlation between troposphere temperature variations and the weakening of the Indian summer monsoon circulation.───對43aNCEP/NCAR再分析資料和臺站實(shí)際觀(guān)測資料的分析,揭示了對流層溫度變化和印度夏季風(fēng)環(huán)流減弱之間的聯(lián)系。

18 、Guided propagation of naturally occurring infrasound in the troposphere and stratosphere───在對流層和平流層自然出現次聲速的導向傳播

19 、Analysis of Altimeter Wet Troposphere Range Correction -───中國海洋與湖沼學(xué)報：英文版 - 紀永剛,張杰,姬光榮

20 、In the downstream of Qinghai-Xizang Plateau, convergence of high level of troposphere restrains cyclone development in the east of China continent.───在青藏高原主體下游,高層輻合,抑制了我國大陸東部的氣旋發(fā)展。

21 、INFLUENCE OF ATMOSPHERIC TIDE ON CORRECTION OF TROPOSPHERE DELAY───大氣潮給對流層延遲影響的探討

22 、Significant enhancements of nitrogen oxides, black carbon, and ozone in the North Atlantic lower free troposphere resulting from North American boreal wildfires───在北大西洋較低的自由大氣中來(lái)自北美北部的野外火災的氮氧化物、黑碳和臭氧的重要增強

23 、a high-speed high-altitude airstream blowing from west to east near the top of the troposphere; has important effects of the formation of weather fronts.───一種高速、高海拔的風(fēng)流，通常在對流層的最高處從西向東刮；對鋒面的形成有重要影響。

24 、Raman lidar observations of aged Siberian and Canadian forest fire smoke in the free troposphere over Germany in 2003: Microphysical particle characterization───在2003年德國上空自由對流層中的西伯利亞和加拿大長(cháng)期的森林火煙霧的Raman激光雷達觀(guān)測:微物理粒子特征

25 、Therefore, it is not the advection process, but the vertical heating profile, which causes the atmospheric response in the lower troposphere out of phase with that in the upper troposphere.───因而闡明，不是由于平流作用，而是由于加熱垂直梯度方向的改變，在加熱中心下方產(chǎn)生正渦度強迫，中心上方產(chǎn)生負渦度強迫。

26 、Two wind maxima with jet-stream characteristics often occur, one above the other, in the lower troposphere by the south side of therainstorm area over South China in summer.───華南暴雨區南側對流層中下層常常同時(shí)存在兩個(gè)大風(fēng)層且各具急流的特征。

27 、The vertical vorticity transition is not favorable to the strengthening of plateau vortex in the middle and low troposphere levels.───垂直渦度輸送不利于對流層中低層低渦加強。

28 、Significant enhancements of nitrogen oxides, black carbon, and ozone in North Atlantic Lower free troposphere resulting from North American boreal wildfires───北美北方野外火災導致的北大西洋自由大氣下部的氮氧化物、黑碳和臭氧的重要增加

29 、In this region there exists a vorticity accumulation in the lower half of the troposphere and a sink in the upper troposphere.───在對流層下層有一個(gè)渦度的積累,對流層上層有渦度的虧損。

30 、H2O absorption is predominant in the troposphere, particularly the lower troposphere.───H2O吸收在對流層，特別在對流層下部起著(zhù)主要作用。

31 、In the smog chamber, black light was used to simulate the sun light in troposphere and metyl nitrate to produce OH radical by photo decompose.───在煙霧箱中,對流層太陽(yáng)光用黑光燈模擬。OH自由基用亞硝酸甲脂光解產(chǎn)生。

32 、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(guò)程的作用。

33 、Fishman, J., Watson, C.E., Logan J.C. and Logan, J.A., 1990.Distribution of troposphere ozone determined from satellite data.Journal of Geophysical Research 95, 3599-3617.───何宜達，2004，高屏地區臭氧事件日光化學(xué)模式解析及氣象條件之探討，國立中山大學(xué)環(huán)境工程研究所，博士論文。

34 、in the upper troposphere, ozone is created much more efficiently and is destroyed less easily than at ground level───在上對流層中，與地面附近相比，臭氧能更有效地生成，而且更難分解。

35 、Over the Bay of Bengal, summertime latent heat release associated with deep convection exceeds longwave radiative cooling, resulting in intense heating in almost the whole troposphere.───夏季孟加拉灣地區的深對流凝結潛熱釋放遠大于長(cháng)波輻的冷卻作用，因而整個(gè)對流層幾乎都保持較強的非絕熱加熱。

36 、In the event of passenger cruise stage of the jet, mostly because of the troposphere has convection beyond phenomenon.───同樣地，滑翔機一般會(huì )在上升暖氣流上滑翔，這股氣流從對流層上升到達平流層就會(huì )停止。

37 、The overall diabatic heating is positive in the whole troposphere in summer, with the most intense heating located in the boundary layer.───夏季高原地區總非絕熱加熱是正值，且最大加熱率出現在邊界層內。

38 、In the development of the vortex, there exist three branches of air flows in the upper and lower troposphere, which are compared with those in the heavy rain region onthe east side of Rocky Mountains.───在渦發(fā)展時(shí)期,對流層高低層存在“三支氣流”,并將其與美國落基山東側暴雨區內的“三支氣流”作了比較.

39 、Mean radiative energy balance and vertical mass fluxes in the equatorial upper troposphere and lower stratosphere───在赤道對流層上部和平流層下部平均輻射能量平衡和鉛直質(zhì)量通量

40 、Florida thunderstorms: A faucet of reactive nitrogen to the upper troposphere───佛羅里達雷暴:到上部對流層的活性氮入口

41 、Raman Lidar Measured Temperature Profiles in the Mid- and Upper Troposphere───Raman激光雷達探測對流層中上部大氣溫度分布

42 、troposphere layer───對流層

43 、Modeling of ozone reactions on aircraft-related soot in the upper troposphere and lower stratosphere───對流層上部和平流層低部臭氧在飛機-有關(guān)的煤灰反應的模擬

44 、At the same time, troposphere delay is one of he main influence factors.───其中,對流層延遲是影響高程方向精度的主要因素之一。

45 、Keywords Atmospheric chemistry Stratosphere Troposphere Instrumental measurement Platform Ozone Nitrogen oxides;───關(guān)鍵詞大氣化學(xué);平流層;對流層;儀器測量;平臺;臭氧;氮氧化物;

46 、circulation pattern at the upper troposphere───對流層上部環(huán)流形勢

47 、Any time metal breaks the upper troposphere, it can acquire a temporary radioactive charge.─── 任何時(shí)候只要金屬在對流層上部發(fā)生破損 就會(huì )暫時(shí)帶上放射性電荷

48 、In the lower troposphere, the forced anticyclone appears on the eastern side of the heating region;───從而反氣旋式高壓位于熱源中心層以上（下）的高（低）層的西（東）側；

49 、the atmospheric layer between the troposphere and the mesosphere.───位于對流層之上中間層之下的范圍的大氣。

50 、In the natural air of the troposphere a suitable amount of ozone is beneficial to clean air.───在對流層大氣中,適量臭氧對清潔大氣是有益的。

51 、87. 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(zhù)是電離層，最上層是外逸層。

52 、In the southwestern part of the WNP, the interannual variation in TCs number is attributed to the convergence of zonal wind in low troposphere;───分析結果表明:在WNP的西南區域,低層緯向風(fēng)的緯向輻合對TC生成數量的年際變化起著(zhù)重要的動(dòng)力作用;

53 、For the warm-type, clouds also extended into the prefrontal area because of more humid and warmer southerlies as well as stronger convergence and upward motion in the lower troposphere.───兩類(lèi)鋒面之云區均主要分布在鋒上與鋒后，唯暖型上滑鋒鋒前仍有些許云量，此應與鋒前近地層南風(fēng)分量帶來(lái)較暖濕空氣，且鋒前有較大之低層輻合與較大之上升運動(dòng)有關(guān)。

54 、Column-integrated aerosol optical properties in the free troposphere: case study-Sierra Nevada, Spain───在自由對流層里柱狀-綜合氣溶膠光學(xué)特性:西班牙、內華達山脈個(gè)例研究

55 、Intraseasonal variations of water vapor and cirrus clouds in the tropical upper troposphere───在熱帶上部對流層水汽和卷云的季內變化

56 、The refraction of the neutral atmosphere including the troposphere and stratosphere, is one of the major error sources for GPS positioning.───中性大氣包括對流層和平流層，它們對GPS信號造成的延遲影響是GPS**的一個(gè)主要誤差源。

57 、troposphere absorption───大氣吸收

58 、A new gale center is generated near the lower troposphere of westerly belt system when it has partly invaded into the egion of typhoon.───發(fā)現在侵入臺風(fēng)后的西風(fēng)帶系統附近的低層產(chǎn)生一新的大風(fēng)中心,在該中心的下風(fēng)處的低層輻合區產(chǎn)生暴雨。

59 、But in the stratosphere, ozone concentration sharp rise, the moisture content is extremely small, there will not be a cloud phenomenon, stratospheric than troposphere to dry much.───但是中在平流層，臭氧濃度急劇上升，水汽含量也極為的少，所以不會(huì )出現云雨現象，平流層比對流層要干燥得多。

60 、INFLUENCE OF COLD ADVECTION IN MID-AND-UPPER TROPOSPHERE ON SQUALL LINE OCCURRENCE───中上層冷平流對颮線(xiàn)發(fā)生的影響

61 、The troposphere is around 10 kilometres thick.─── 對流層的厚度大概為十千米

62 、English: 87.Above the troposphere is the stratosphere, followed by the ionosphere and capped by the exosphere.───中文: 在對流層上是平流層，接著(zhù)是電離層，最上層是外逸層。

63 、However, under certain conditions, will also appear in the troposphere with a high degree of temperature increase and rising phenomenon, called "inversion phenomenon.───但在一定條件下，對流層中也會(huì )出現氣溫隨高度增加而上升的現象，稱(chēng)之為“逆溫現象”。

64 、By using the relationship between troposphere delay and water vapor, the GPS water vapor retrieval method can be built to get precipitation water vapor(PWV) and slant-path water vapor (SWV).───利用對流層延遲與水汽之間的關(guān)系，可以建立地基GPS水汽反演方法以獲取大氣可降水汽總量PWV和斜路徑水汽含量SWV，并通過(guò)層析算法得到三維水汽分布。

65 、7.a high-speed high-altitude airstream blowing from west to east near the top of the troposphere;───一種高速、高海拔的風(fēng)流，通常在對流層的最高處從西向東刮；

66 、upper troposphere and lower stratosphere───上對流層-下平流層

67 、THE DECADAL VARIATIONS OF CLIMATE IN TROPOSPHERE OF SOUTHERN HEMISPHERE AND ITS RELATION WITH SOLAR ACTIVITIES───南半球對流層氣候年代際變化及其與太陽(yáng)活動(dòng)的聯(lián)系

68 、Why do we say troposphere and human are in most close relations ?───為什么說(shuō),對流層與人類(lèi)的關(guān)系最為密切?

69 、English: 87. Above the troposphere is the stratosphere, followed by the ionosphere and capped by the exosphere.───中文:在對流層上是平流層，接著(zhù)是電離層，最上層是外逸層。

70 、There are favourable conditions in height and temperature fields for the vortex forming over the Plateau if the water vapor increases in the middle and upper troposphere over the west of India and Arabian Sea.───印度西部 -阿拉伯海上空對流層中上部水汽增加 ,可使高原上出現有利于低渦形成的高度場(chǎng)、溫度場(chǎng)條件 ;

71 、A SYNOPTIC ANALYSIS OF THE EVOLUTION OF GENERAL CIRCULATION IN THE UPPER TROPOSPHERE OF THE NORTHERN HEMISPHERE DURING THE PERIOD OF EARLY SUMMER, 1958───1958年初夏北半球對流層上部大氣環(huán)流演變的分析

72 、Ozone variability in the midlatitude upper troposphere and lower stratosphere diagnosed from a monthly SAGE II climatology relative to the tropopause───從每月SAGE II關(guān)于對流層頂的氣候學(xué)診斷的中緯度上部對流層下部平流層的臭氧變率

73 、ANALYSIS FOR A CASE OF OZONE DOWNWARD TRANSPORT FROM STRATOSPHERE TO TROPOSPHERE AS OBSERVED OVER XINING, CHINA───一次對流層異常臭氧次峰的觀(guān)測研究及其動(dòng)力輸送過(guò)程的分析

74 、Regional and global trace gas distributions and inferred transports in the upper troposphere and lower stratosphere───對流層上部和平流層下部局部的和全球的示蹤氣體的分布及其推斷的輸送

75 、Chlorine and bromine atom ratios in the springtime Arctic troposphere as determined from measurements of halogenated volatile organic compounds───從鹵化揮發(fā)性有機化合物測量確定的春季北極對流層中的氯氣和溴原子比率

76 、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)。

77 、For decades it was thought that all our weather happened in just one layer of the atmosphere, the troposphere, but scientists have discovered that the layer above, the stratosphere, is also fundamental to our weather.─── 幾十年來(lái)我們都認為天氣現象只發(fā)生在 大氣層中的一層 也就是對流層中 但是科學(xué)家們發(fā)現對流層上方的 平流層也對天氣起到重要作用

78 、The purpose of DGPS is to reduce the effect of GPS satellite orbit errors, clock errors, and the atmospheric delays from ionosphere and troposphere.───其目的在減低GPS衛星軌道及時(shí)間誤差,及大氣層中電離層和對流層延遲效應之影響。

79 、For example, a non-geostrophic vortex in wind field on the 375 mb level can result in a high with the warm center in the troposphere and the cold center in the stratosphere.───例如375毫巴上單純非地轉風(fēng)的流場(chǎng)的反氣旋渦旋,適應后可建立起對流層暖性、平流層是冷性的高壓系統。

80 、a high-speed high-altitude airstream blowing from west to east near the top of the troposphere; has important effects of the formation of weather fronts───一種高速、高海拔的風(fēng)流，通常在對流層的最高處從西向東刮；對鋒面的形成有重要影響

81 、Mid-upper troposphere───對流層中上層

82 、4) AIRS can significant increase the retrieval accuracy introposphere middle ? up level and tropopause, in the troposphere lower, especially near thesurface, the accuracy is not ideal enough;───4)AIRS反演的大氣溫度在對流層頂和中上層具有較高的精度,在對流層低層,尤其是近地面反演精度不夠理想;

83 、The region of discontinuity between the troposphere and the stratosphere.───位于對流層和平流層之間的界限。

84 、The Relationship Between the Intraseasonal Oscillations in the Northern Hemisphere During the Boreal Winter in the Stratosphere and Troposphere───冬季北半球平流層季節內振蕩與對流層季節內振蕩的關(guān)系

大氣層大氣上分為哪幾層這幾層是按什么順序來(lái)說(shuō)明的

按熱力學(xué)垂直分布對大氣分層（熱分層），可以分為以下幾層：

一，對流層(Troposphere)：對流層是大氣的最低層，其厚度隨緯度和季節而變化。在赤道附近為17-18km；在中緯度地區為l0-12km，高緯度為8-9km。夏季較厚，冬季較薄。在對流層中，因受地表的影響不同，又可分為三層。在0.6~1.5km以下叫擾動(dòng)層（或者叫摩擦層）；2m以下叫貼地層；擾動(dòng)層以上稱(chēng)自由大氣．這里平均溫度在17~-52℃．

二，平流層(Stratosphere)：從對流頂層(tropopause)到約55km的大氣層為平流層,這里氣流呈水平運動(dòng)，25km以下溫度隨高度變化較小，氣溫趨于穩定，所以又稱(chēng)同溫層；25km以上，溫度隨高度升高而升高。 在高約10~60km范圍內，有厚約20km的臭氧層，因臭氧具有吸收紫外線(xiàn)的能力，故使這里的平流層溫度升高。這里平均溫度在－3℃．

三，中間層(Mesosphere)：從平流頂層(stratopause)到距地面85km高度稱(chēng)為中間層。這一層空氣更為稀薄，溫度隨高度增加而降低。這里也是電離層的底部，流星，極光都誕生在這里．這里平均溫度在-93℃．

四，熱層：從中間頂層(mesopauce)到約600km稱(chēng)為熱層。頂部溫度可達1000k°（太陽(yáng)大年可達2000k°）．電離層的中上部都在這里．這里平均溫度在1727℃．

五，逃逸層(Exosphere)：600km以上叫逃逸層又稱(chēng)外大氣層．它的邊界可達6400km．溫度可達數千k°,這里有極光，流星．

大氣層大氣上分為哪幾層這幾層是按什么順序來(lái)說(shuō)明的

依次分別是對流層、平流層還有臭氧層。如果對你有幫助，就給個(gè)好評唄，謝謝。