查询词典 Hadley

The intensity index of Hadley circulation is defined and calculated by using the 3 levels wind data in 4 key regions for the southern/northern hemisphere and the global.

利用3层4个关键区的风定义并计算了1948年l月－2004年12月的全球纬向平均的南／北半球和全球Hadley环流逐月强度指数。

In this research, the index for Hadley circulation intensity is defined as the maximum positive value of the zonal mean streamfunction occurring within the latitudinal zone of 0°~30°N, and index for NPO as normalized sea level pressure difference between the region (20°N, 180°~160°W) and the region (60°N, 180°~160°W).

本文选取0°~30°N区域里最大质量流函数来描述北半球Hadley环流强度随时间的演变，利用(20°N， 180°~160°W)和(60°N， 180°~160°W)区域平均的标准化海平面气压差代表NPO强度。

Then the Hadley circulation in the Eastern Hemisphere is weakened and that in the Western Hemisphere is enhanced, followed with the moment of momentum taken by its ascending branch increased in the Western Hemisphere while weakened in the Eastern Hemisphere. The PNA pattern is enhanced and the Pacific-East Asian teleconnection is weakened. As a result, the atmospheric circulation's response to the ENSO events in the Eastern Hemisphere is weakened and that in the Western Hemisphere is enhanced.

o事件使Walker环流减弱及其上升支东移的现象更明显，Hadley环流在东半球减弱而在西半球增强，由其上升支带至中纬的角动量在东半球减少，西半球增多，造成影响西半球大气环流的PNA型遥相关增强，影响东半球的太平洋-东亚型遥相关减弱，进而使得ENSO对东半球大气环流的影响减弱而对西半球大气环流的影响则有所增强。

In the same period, the meridional circulation is a typical Hadley cell in the Pacific trade wind area fig.

在信风区、低纬度则存在着典型的Hadley环流，高层有夏季太平洋中部副热带西风急流，下部有东北信风，东风随高度减弱。

Land-sea heating, monsoon circulation, eastern Pacific trade wind and the slow seasonal shift of NE Pacific SST form winter to summer bihemispherically- all in joint action give rise to the enhancement of the Walker circulation that will travel east-and northward (west-and southward); the intensification of the maintained eastern Pacific Hadley circulation and north America-Alatantic Walker circulation zonally is responsible dominantly for the zonal/meridional movement of the WPSH in the winter-to-summer (or summer-to-winter) shift and its combination with the north American subtropical high.

海陆加热、季风环流、东太平洋信风以及东北太平洋海表温度由冬向夏关于赤道南北季节转换的迟缓性等综合作用导致的纬向Walker环流的加强东移和北抬、持续的东太平洋Hadley环流和北美—大西洋纬向Walker环流的加强是西太平洋副高由冬向夏产生东西、南北移动及其与北美副高合并的主要原因。

Hadley was a tall, shambling man with thinning red hair.

Hadley身材高大，头发是红色的却很稀少，走起路来摇摇晃晃。

It seems to be completed throngh the influence of the marine anomaly heat transfer from Equatorial Eastern Pacific on the Hadley circulation and the westerlies in No...

同时指出，这种影响可能是通过赤道东太平洋海洋对大气的异常加热、对北半球冬季Hadley环流和中纬度西风环流型的影响来实现的。

In the third chapter, using the methods of nonlinear feedback functions and Lyapunov functions and combining analytical with numerical methods, the nonlinear feedback methods are introduced and the synchronizations of chaos in Hadley system of aerographs and LFRBM system of physics are realized. Some of nonlinear feedback functions are constructed.

第三章在介绍非线性反馈方法原理的基础上，应用非线性控制的基本思想及Lyapunov函数方法，将解析法与数值法相结合，分别对气象学中著名的Hadley环流和物理学中的LFRBM系统进行研究，找到了一类非线性反馈函数，实现了混沌自同步，并利用Mathematica软件进行仿真实验，数值结果说明了该方法的有效性。

The weather of Yunnan-Guizhou Plateau is greatly impacted by the emergence of the Ferrel cell, which is resulted from the lifting effect of Tibetan Plateau and the southward anomaly of the Hadley cell.

青藏高原的抬升作用与Hadley环流偏南导致Ferrel环流的生成、加强对云贵高原的天气有重大的影响。

The main characteristic of the meridional cell averaged over 110~ 140°E is as follows: The monsoon cell in East Asia replaces Ferrel cell in January and Hadley cell in July in the Northern Hemisphere. In addition, its decadal change is very obvious.

2110～140°E的平均经圈环流主要特点是：1月东亚季风环流圈代替了北半球的Ferrel环流圈，7月东亚季风环流圈代替了北半球的Hadley环流圈，而且其10年际变化也比较明显。

It goes back to what I told you...

现在回到我告诉过你的。。。

With a supporter in Mr Charest and an admirer in Mr Dumont, Mr Harper may be encouraged to call an election himself.

由于在沙雷那边有个支持者，杜蒙那边有个崇拜者，鼓励哈珀为自己举行一次选举。