英语释义

• the region of discontinuity between the troposphere and the stratosphere

片语

extratropical tropopause温带对流层顶

tropopause oscillation对流层顶振蕩

double tropopause双重对流层顶

tropopause e对流层顶

multiple tropopause复对流层顶

muluple tropopause复对流层顶

tropopause chart[气象]

tropopause ozone对流层顶臭氧

TROPO Tropopause对流层顶

英汉例句

• the downward transport of ozone due to tropopause folding can reach middle part of troposphere, which has the most influence on the ozone in the upper troposphere.

  对流层顶折叠使高空臭氧向下输送，这种向下的输送可以到达对流层中部，对上对流层的臭氧影响最大。

• the frenqu-ency distribution of compound tropopause in summer and winter and inter-diurnal variation of various categories of tropopause over beijing.

  阐述了冬夏复合对流层顶的频率分布情况以及北京、汉口等站对流层顶的日际变动。

• there are three main eof modes of tropopause height field: the first eof mode is consistently higher (lower) than normal;

  对流层顶高度场有三种主要的模态：第一种为全区一致的偏高（偏低）型；

• the spatial-temporal distribution feature of tropopause pressure field over the tibetan plateau and adjacent areas from 1948 to 2004 is analyzed using the method of empirical orthogonal function(eof).

  利用经验正交函数分解（eof）方法，对1948～2004年青藏高原及东亚邻近区域对流层顶气压场的时空演变结构进行了分析。

• the largest differences are near the ground and in tropopause region, particularly over the land with complicated topography.

  最大偏差主要发生在近地面大气层、对流层顶附近和地形复杂的陆地区域。

• there are close relations between the losses of total ozone in spring and summer and the uplift of the second tropopause height in summer over the qinghai-xizang plateau in recent 30 years.

  近30年春、夏季高原臭氧总量亏损与夏季高原第二对流层顶高度的抬升存在着密切关系。

• diagnostic study of jet streaks: kinematic signatures and relationship to coherent tropopause disturbances.

  急流爆发的诊断研究：动能特征及其雨对流层顶连续扰动的关系。

• analysis of the observational data, the toms total ozone, and ncep circulation, shows that the atmospheric ozone amount experienced a high-low-high variation with low-high-low tropopause altitude.

  分析大气监测资料、toms臭氧总量资料和ncep大气环流资料表明，大气臭氧总量随着对流层顶的低一高一低变化呈高一低一高的变化过程。

• the results show that the h2o mixing ratio decreases with height in upper troposphere quickly reaches a minimum near the tropopause and the bottom of stratosphere; and then it increases .

  结果表明：高原上空h2o混合比在对流层上层随高度迅速减少，在对流层顶和平流层底达到极小值，平流层里水汽混合比随高度增加。

• 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 results show that when the two kinds of tropopause are used, the mass and ozone fluxes cross tropopause in tropical latitudes are tst flux areas, and convers to the stt flux in the sub\|tropics.

  结果表明，采用这两种定义下的对流层顶时，穿越对流层顶的质量和臭氧通量都表现出在热带纬度带为tst通量， 到了副热带则转换为stt通量。

• the whole tropical tropopause has been warmed up from cold period to warm period.

  从偏冷期到偏暖期，整个热带对流层顶显着变暖。

• the equatorial heat budget at tropopause is quasi-equilibrium state, the strongest zone of the abrupt change character of q is above some sea marching with some land.

  ②赤道附近对流层顶的热量收支处于相对的準平衡态，而加热率突变性最强的区域位于海陆交界的洋面上空；

• strong westerlies, at times, have been observed near the tropopause over recife, brasil, approximately 9o from the equator.

  强大的西风气流有时曾在离赤道大约9个纬度的巴西recife上空的对流层顶附近观测到过。

• the tropopause folding, which means that high pv spreads downward from the upper troposphere or stratosphere, helps the releasing of potential instability energy and the development of rainstorm.

  对流层高层或平流层低层高位涡的下传有利于位势不稳定能量的释放，使得暴雨增幅。

• double tropopause frequency is high in winter, while the first tropopause (ft) (also called polar tropopause) is rarely seen in summer, in which there is only the second tropopause.

  到了夏季，第一对流层顶 （极地对流层顶）较少见， 基本只有第二对流层顶。

• the relationship between arctic tropopause height and surface air temperature is discussed by using the aerological sounding and surface data during 1977-1990 in beijing area.

  利用北京地区1977—1990年的高空、地面资料，讨论了极地对流层顶与地面温度的关系。

• from annual change of the tropopause height, it was negatively related to lower stratospheric temperature and positively associated with the troposphere temperature, and there was seasonal difference.

  从平均对流层顶高度的年变化看来，对流层顶高度与平流层低层温度呈负相关，与对流层温度呈正相关，且存在季节差异。