文中指出垂直风切变及其变化与温度平流的存在是紧密相关的。
It is pointed out that vertical wind shear and its change are closely correlated with the temperature advection.
冰雹落区与高低空温度平流和总温度平流的分布有着较好的对应关系。
The hail area was correlated well to the distribution of temperature advection.
多普勒速度场、回波顶高、垂直液态含水量、对应的上升气流以及温度平流对这次降水具有预报指示意义。
The vortex in Doppler velocity field, Echo tops, Vertical integrated liquid, lift stream and cold advection are significant in this rainfall case.
结果表明，高空急流区温度平流分布的不均匀性，会在急流附近等温线密集区边缘激发出空气垂直运动和湍流，引起飞机颠簸。
The results show that the inhomogeneous distribution of temperature advection in upper jet stream trigger vertical currents in the marginal area of upper jet stream and cause airplane turbulence.
重要的是要记住，极端温度与平流基本无关，因为它们主要是在相当静止的空气中形成的。
It is important to bear in mind that the extreme temperatures are largely independent of advection, for they develop mostly in rather stagnant air.
向平流层喷洒硫酸盐颗粒，可以通过反射阳光达到降低地球温度的作用。
Injecting sulphate particles into the stratosphere, for instance, would cool the Earth by reflecting more sunlight into space.
不过，其他时候这温度似乎只预示了一个更潮湿的平流层。
At other times, though, they have seemed to predict a wetter stratosphere.
也可能像前人建议的，当对流层温度升高，长期起来会形成一个湿度更大、温度更高、高度更低的平流层。
Or it may be, as others have suggested in the past, that the long-term trend, as the troposphere warms up, will be to a wetter, more warming lower stratosphere, too.
Solomon博士倾向于前者，理由是平流层和海洋表面温度两者关系的改变方式。
Dr Solomon suspects the former, because of the way the relationship between the stratosphere and the sea-surface temperature has changed.
1996年，Haigh指出，平流层的温度影响了喷流的一段，而喷流是横跨欧洲自西向东的一条高海拔气流通道。
Back in 1996, Haigh showed that the temperature of the stratosphere influences the passage of the jet stream, the high-altitude river of air passing from west to east across Europe.
温室气体增加和可能的臭氧恢复将是影响21世纪平流层温度变化的两个主要因素。
Increasing greenhouse gases and likely ozone recovery will be the two most important factors influencing changes in stratospheric temperatures in the 21st century.
水平温度梯度的平流对锋生（消）的影响都很小。
The horizontal advection term contribute little to the frontogenesis and frontolysis.
这与近几年来，平流层内臭氧减少，温度降低，对流层高度抬升有关。
These are related with the decreasing of stratospheric ozone and temperature, as well as the rising of the troposphere in recent years.
大气湍流平流作用对不同模式的大气温度有一定的影响。
The turbulence advection has a certain extent impact on the temperature of different modes.
平流层温度趋势能被归因于臭氧减少吗？
Can stratospheric temperature trends be attributed to ozone depletion?
对我国1980 ~ 2007年120个观测站的探空资料进行处理后，分别计算得出对流层顶高度、对流层温度和平流层低层温度。
Based on sounding data of 120 meteorological observation stations in China from 1980 to 2007, the height of tropopause, tropospheric temperature and temperature at low stratosphere were calculated.
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。
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.
EESC的年代际变化与臭氧变化趋势相似，臭氧的年际变化与平流层温度关系密切。
Decadal changes in EESC are similar to those of the ozone hole, and interannual variations of ozone are closely related with stratospheric temperature.
EESC的年代际变化与臭氧变化趋势相似，臭氧的年际变化与平流层温度关系密切。
Decadal changes in EESC are similar to those of the ozone hole, and interannual variations of ozone are closely related with stratospheric temperature.
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