对流层

Evaluation results show that the turbulence in convection zone is capable of generating enough wave energy to supply coronal energy lose due to convection and radiation.

利用理论结果的计算表明，对流层的湍动对流完全有可能激发足够的波能去补充日冕中等离子体对流和辐射造成的能量损失。

In the first part, turbulent motion in convection zone as source to generate Alfven waves is studied following Lighthill-Stein theory, in which the turbulent source was described by nonlinear terms in MHD equations.

第一个方面主要地研究了加热日冕的Alfven波源。我们采用Lighthill-Stein理论分析了对流层中的湍流运动对扭转Alfven波的激发作用。

The decennary increment of AOD averaged from all stations was 0.05. As to mean values, the maximum was in Sichuan Basin of 0.649, and the second maximum in South-Xinjiang Basin of 0.411, while the minimum was in Qinhai-Tibet plateau of 0.125. As to seasonal mean, AOD in spring had the highest value, and then in summer, while the minimum was in winter.

对本文方法反演的50多个台站1961～1990年的0.75μm对流层AOD数据进行统计分析，结果表明：我国AOD分布受地形影响显著，存在四川盆地、南疆盆地高值区和青藏高原低值区，1961～1990年平均AOD四川盆地为0.649，南疆盆地为0.411，青藏高原为0.125.1961～1990年，四川盆地光学厚度增加最显著，平均每十年增加0.16；南疆盆地光学厚度增长相对缓慢，平均每十年增加0.03；青藏高原为光学厚度增加最缓慢的地区，平均每十年增加0.01；全国平均AOD每十年增加0.05。

This is because the top of the troposphere is normally very cold, causing ascending water vapour to freeze into ice crystals that drift and fall, rather than continuing up into the stratosphere.

这是因为对流层的顶端通常极其寒冷，上升的水蒸汽凝结成飘落而下的冰晶，而没有继续上升进入平流层。

In most part of east China, the biogenic VOC emission played an enhancive role in the ozone production. The induced increases of the surface ozone concentration ranged from 0ppbv to 5ppbv for most regions, and in some places, however, the increase could be more than 30ppbv.

VOC生态源对于对流层O〓的产生一般起不同程度的促进作用，其所导致的近地面O〓浓度的增加幅度大部分地区在0～5ppbv之间，但局部地区可达30ppbv以上。

A final has an accuracy of 5cm for the precise ephemeris and 0.1~0.2ns for the clock information.

本文研究了利用随机游走过程模拟对流层延迟残差随机变化的方法。

Newell, et al ., found 10 huge filamentary structures that are the preferable pathways of water vapor movement in the troposphere (the lower 10-20 km of the atmosphere) with flow rates of about 165 million kilograms of water per second.

纽维尔，等人，发现10个巨大的丝状结构，是最好的途径，水汽运动在对流层（下10-20公里的大气层）与流率约1.65亿公斤水每秒。

The strong westerly jet in the upper troposphere is linked to the Mongolia cyclone and frontogenesis at low level which can cause strong wind and further provides the dynamic factor for the increased DWF in Beijing.

春季对流层高层的东亚西风急流增强能使低空的蒙古气旋加强和锋生，从而引起地面大风，为沙尘天气频次的增加提供动力条件。

Data comparison shows a significant correlation between the TOR and surface ozone data collected at the GAW Lin 誥 n regional background station in the Yangtze Delta region, suggesting that the observational data have regional representativeness.

结果表明，长江三角洲地区对流层 O3柱含量的季节变化与该地区的临安区域大气本底站的地面 O3季节变化有着显著的相关关系，临安站的观测数据具有区域代表性。

Year global analysis of characteristics of tropopause distribution and variation.

40年全球对流层顶分布和变化特征分析。

As she looked at Warrington's manly face, and dark, melancholy eyes, she had settled in her mind that he must have been the victim of an unhappy attachment.

每逢看到沃林顿那刚毅的脸，那乌黑、忧郁的眼睛，她便会相信，他一定作过不幸的爱情的受害者。

Maybe they'll disappear into a pothole.

也许他们将在壶穴里消失