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stationary front相关的网络例句

查询词典 stationary front

与 stationary front 相关的网络例句 [注:此内容来源于网络,仅供参考]

First, according to a phase matching condition of electromagnetic wave on the stationary boundary surface, we find the refelection and transimission angles in the front system with a static ionization front. Then using the transformations of wave vector and frequency we get the corresponding angles in the laboratory system in which the ionization front is moving at relativistic speed.

首先在波面参考系中根据电磁波在固定边界上的相位匹配条件,确定电磁波在静止电离波面上的反射角和透射角,并利用波矢和频率的相对论变换,导出了在实验室参考系中相应的反射角和透射角的表达式,最后对所得的结果作了进一步的讨论。

It is also shown that heating frontogenesis is unfavourable to the maintenance of horizontal stable layer in the quasi-stationary front

分析还表明,凝结加热的锋生作用不利于南岭静止锋水平稳定层的维持。

By using the observed data, ten canonical cases of Kunming quasi-stationary front during 1993-1995 in winter and spring seasons are studied.

利用常规探空资料,选取1993-1995年冬、春季节中10个昆明准静止锋典型个例作了合成计算,分析了昆明准静止锋的结构。

There is a monsoon surge to the south of the stationary front bringing moisture into the rainstorms.

中国淮河以南地区夏季最易受到洪水灾害的威胁,这种致洪暴雨一般出现在沿着河谷走向的静止锋上。

It was a typical South China quasi-stationary precipitation which was associated with the stationary front, low-level wind shear and low-level jet.

这是建立在静止锋、低空切变线和低空急流等系统基础上的一次典型的华南准静止锋降水。

The relationship of front and weather: They had the right conception of "front" and "air mass" as scientists, but some students were easily mixing the concept of cold front , warm front and stationary front.

锋面与天气的关系:对於锋面与气团的概念具有符合科学家的概念。但是对於冷锋、暖锋及滞留锋的天气状况,部分学童仍有混淆的情形。

Based on NCEP and other observational datasets, a severe heavy rainfall process occurred in the south of china during June 18-19,1998 was investigated. The first diagnostic analyses show that the strong rainfall are produced by vortex, shear line and upper and lower jets, stationary front. The condition of high energy, saturation, potential instability is propitious to the form and maintenance of this rainfall.

采用NCEP全球谱模式和常规观测资料对98年6月18~19日华南暴雨的影响系统及其可能机制进行了初步诊断分析,发现这次强降水过程是受低槽、低涡、切变线、高、低空急流和地面静止锋共同影响造成的,该地区维持高能、饱和、潜在不稳定的环境,有利于暴雨的产生。

Based on general ground observation data and NCEP data, the atmospheric circulation and the structure of Dian-Qian Quasi-stationary Front during Jan. 2001 are studied.

利用地面常规观测资料和NCEP/NCAR再分析资料,分析2001年1月的滇黔准静止锋在演变过程中的温湿结构和大气环流特征。

Based on general ground observation data and NCEP data,the atmospheric circulation and the structure of Dian-Qian Quasi-stationary Front during Jan.

利用地面常规观测资料和NCEP/NCAR再分析资料,分析2001年1月的滇黔准静止锋在演变过程中的温湿结构和大气环流特征。

The intensity is less and depth is higher comparing with ones of Yangtze River Basin in the Mei-Yu period and quasi-stationary front rainstorm in South China.

混合云团与东移的高空槽云系相遇并叠置的大到暴雨过程,镶嵌于回波中的对流单体是造成强降水的直接系统,其尺度只有10~20km。

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