tropopause

The characteristics of temporal and spatial variation of Tropopause over China and its controlling factors

我国对流层顶的时空分布特征及其影响因子

The differences of tropical tropopause temperature between these two periods are intrinsically related to the anomalous variations of air temperature and the geopotential height in the troposphere .

热带对流层顶气温在两个不同时期的差别与大气气温以及位势高度的异常变化有较好的关系。

Polar tropopause temperature structure has different trend in two hemisphere ;

南北半球的极地对流层顶温度结构在不同的季节有不同的变化趋势；

The Relationship Between Arctic Tropopause Height and Surface Air Temperature in Beijing Area

北京地区极地对流层顶与地面要素之间的关系

Climatic characteristics of the first tropopause height over Liaoning province

辽宁地区第一对流层顶高度变化特征分析

Change The variation of spatial-temporal distribution of the global tropopause ozone

大气对流层顶的臭氧时空分布变化

Statistics of the global tropopause temperature change

全球对流层顶温度场演变的气候学特征分析

Nonlinear evolution of a gravity wave propagating from the tropopause

对流层上传重力波的非线性演化

Convective impact on temperatures observed near the tropical tropopause .

对流对热带对流层顶附近观测到的温度的作用。

Change Trend and Analysis of Abrupt Change for the First Tropopause Height over Xinjiang in 1960 - 1999

新疆1960-1999年第一对流层顶高度变化及其突变分析

As soon as the tropopause is reached , temperature stops decreasing with height .

一达到对流层，温度就停止随高度上升。

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著变暖。

The Seasonal Variation of Total Ozon and Its Relationship with the Tropopause

臭氧层季节变化与对流层顶的关系

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。

Climatic characteristics of tropopause over Shenyang

沈阳地区对流层顶气候特征分析

Variation of the Tropopause Height and Its Influence on Ozone Variation in Upper Troposphere / Lower Stratosphere over Beijing

北京地区对流层顶变化及其对上对流层/下平流层区域臭氧变化的影响

Characteristics of Tropopause Over Wuhan and Haikou

武汉与海口地区对流层顶的变化特征

Conversion between potential and kinetic energy in the upper troposphere and the lower stratosphere and energy transports across the tropopause

对流圈上层与平流圈下层动能位能的转换及其间的能量交换输送

The dominant periodicities as detected in the index of either pressure or temperature at tropopause are the 11 year and 3-5 years .

气压指数和气温指数都显示出准11年及准3-5年的主要周期，二者的变化趋势基本上是一致的。

Using the 44 years ( 1958 & 2001 ) NCEP data and ozone mixing ratio data , calculating the global ozone distribution at tropopause .

利用1958~2001年的臭氧垂直分布和NCEP资料，计算出全球对流层顶的气候场，并对其空间分布、季节、年际和年代际演变进行了分析。

In the low-latitude and equator regions , the global tropopause ozone distribution is similar to the temperature distribution to some extent .

极地各季节对流层顶的臭氧分布和高度场特征相似，低纬则与温度场分布较一致；

Both the global mean tropopause pressure and temperature have been decreasing since 1979 , indicating that our tropopause has been moving higher and higher .

夏季全球平均的对流层顶气压和气温在分析时段内均呈下降趋势，表明对流层顶高度有所上升。

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。

The height , temperature and frequency of the first tropopause demonstrated obviously seasonal feature . The height had the lowest value in January and the highest value in July .

第一对流层顶的高度、温度以及出现频率都表现出明显的季节变化特征，其中高度在1月最低，7月最高；

The tropical tropopause temperature decreases in both cold and warm periods , which possibly relates to the increase of the tropical SST in the following falls .

在偏冷期和偏暖期热带对流层顶气温一致下降，引起后期秋季热带地区海温持续升高。

On a theorem in hydrodynamics with some meteorological applications ( deduction of the rate of change of lapse rate and conditions for the substantiality of tropopause )

流体力学的一个定理及在气象学上的应用（大气温度直降率的变化及对流顶同质点造成的条件）

When the SST changes are considered in the doubled CO2 experiment , the stratospheric water vapor is significantly increased with a much higher , but warmer , tropopause .

二氧化碳浓度加倍和海温增加的综合效果，会导致一个更高更暖的对流层顶，同时平流层的水汽也会显著增加。

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。

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。

It doesn 't hurt that the tropopause resides far above the weather that can damage conventional aircraft or , more critically for Solara , block out the sun .

对流层顶下的天气会损坏普通飞行器，对Solara来说更关键的还在于，它会遮蔽太阳，因此在远高于这种天气的对流层顶飞行Solara就不易损坏。