大气垂直结构

上对流层/下平流层大气垂直结构研究进展平流层和中层大气环流

Recent Advances in the Study of Atmospheric Vertical Structures in Upper Troposphere and Lower Stratosphere

论文接着研究了用SVD和EOF技术对传统的一维变分（1DVAR）反演做出改进的方法，基本做法是利用SVD剔除观测中的无效信息，利用EOF技术描写大气参数垂直结构特征。

Secondly , we modify the traditional one-dimensional variational ( 1DVAR ) retrieval method by the SVD and EOF technique . The basic method is that utilize the SVD to get rid of the ineffective information and use the EOF to extract the vertical structure of the atmospheric parameters .

大气的垂直结构与遥相关型

The vertical structure of atmosphere and its teleconnection

然后，对海洋大气的垂直结构作了分层描述，从而对海面有效辐射一般表达式进行具体运算，并且求得简化分析式。

And then , the vertical structures of marine atmosphere are described , and simplified formulae for analysis are obtained .

并利用NCEP资料计算了Brunt-Vaisala频率，分析大气温度场垂直结构和静力稳定度，进一步分析了重力波活动频率与Brewer-Dobson环流的关系。

The Brunt-Vaisala Frequency also was also calculated by the NCEP data to analyze the vertical structure of the atmosphere temperature and the static stability , as well as the relationship between the gravity wave frequency and the Brewer-Dobson circulation .

海洋加热尺度对热带大气垂直环流圈结构的影响

Influence of the ocean heating scale on the structure of the vertical circulation cell in the tropical atmosphere

使用一枚携带chaff的火箭观测到的垂直速度数据，研究中层大气垂直速度扰动细微结构。

Vertical velocity data observed from a chaff rocket measurement are used to study the small scale structure of the vertical velocity fluctuations .

论热带大气垂直环流圈的结构和海洋加热尺度间的关系

On relationship between the structure of vertical circulation and the ocean heating scale in the tropics

试验结果表明，不同的坐标系对大气垂直速度大小计算存在着差异，特别是当分辨率提高时，不同垂直坐标系对大气垂直结构的刻画的差别更加明显。

The simulation results showed that the calculation of vertical velocity is sensitive to vertical coordinates . It is especially more evident when the resolution increased .