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With western Pacific subtropical high as the focus through diagnosis and simulation addressed are the following problems: a the change in northern hemisphere subtropical high and possible mechanisms during seasonal shift; b the index and circulation variation of east Asian monsoon; c Tropical air/sea-the monsoon interaction on an interannual scale, with the results given below.

以西太平洋副热带高压为核心,采用诊断和数值模拟方法讨论了如下问题:1、季节转换过程中的北半球副高变动及其可能机制;2、东亚季风指数与东亚季风环流变化;3、热带海气及其与东亚季风年际相互作用关系;研究表明

4For the typical great flood years of the Yangtze River basin,the ISO anticyclone and cyclone system are continue making and move westward and northward to the eastern China and the coastwise western Pacific by the change of ISO during May and August.

4对典型的长江流域特大洪涝年,伴随着ISO的变化,夏季5~8月,在西太平洋副热带地区和热带赤道附近不断有ISO气旋环流系统生成,并向西、向北移动到我国东部及沿海地区。

Weather patterns are now under the control of Earth's large circulation systems: the belt of subtropical highs near 30° north latitude; the easterly trade winds that occupy the zone south of the highs; and the region of cloudiness that marks the Intertropical Convergence Zone, about 5° north of the equator.

这一段的天气形势处于地球巨大的循环系统控制下:北纬30°附近受副热带高压带控制;向东的信风占据了南高压带;赤道以北大约5°的热带辐合区有较厚的云层。

Bring about air temperature of plain change area the reason of unusual change is very much, the sea expresses Pacific Ocean of equatorial middle east temperature is unusual on the high side the on the high side that can cause this area air temperature northing of high pressure of; South Asia and intertropical Pacific Ocean sea lifts lukewarmly on the west , through the influence subtropic circle system all can cause on the high side of air temperature of plain change area .

导致川渝地区气温异常变化的原因很多,赤道中东太平洋海表温度异常偏高会引起该地区气温的偏高;南亚高压北进以及热带西太平洋海温的升高,通过影响副热带环流系统均会造成川渝地区气温偏高。

Matmo formed as a tropical depression over the western North Pacific about 430 km northeast of Manila on 15 May and moved northeastwards along east periphery of the subtropical ridge .

麦德姆於五月十四日在马尼拉东北约360公里的北太平洋西部上形成为一热带低气压,初时沿著副热带高压脊之东面向东北移动。

Any of several rays of the family Mobulidae,inhabiting tropical and subtropical seas and having a large flattened body,winglike pectoral fin s,a whiplike tail,and two hornlike fin s that project forward from the head.

蝠鲼任一种蝠鲼科的鳐鱼,生活在热带或副热带海域,有大而扁平的身体和翼状的胸鳍,以及鞭状的尾,头的前部有两个角状的向前突出的鳍

Until the third stage, when subtropical high retreats completely from the SCS and the low pressure system over southern China moves southeastward and embeds itself in the low pressure zone over the northern SCS, strong tropical southwesterly flow brings in ample amount of moisture and causes moisture convergence over the southern SCS under the influences of the low pressure zone. Deep convections bloom due to sudden increase of low-level convective instability.

一直到第三个阶段,太平洋副热带高压完全退出南海,而华南低压中心移入南海北部的低压带,与强盛的热带西南气流结合,在南海南部形成强烈的西风与大量的水气集结,低层对流不稳定度快速增加,以致於产生旺盛的对流。

Our analyses show that for the zonally averaged data, in the tropics and subtropics most of zonal anomalies of basic atmospheric fields and quantities related to the energy cycle take on obviously opposite changes between warm and cold events, which does not happen in the middle- and high-latitude regions.

结果表明:对于纬向平均资料来说,冷、暖事件在热带和副热带地区的大气环流相关量的反相变化特征非常清晰,中高纬地区并不明显。

Any of several rays of the family Mobulidae, inhabiting tropical and subtropical seas and having a large flattened body, winglike pectoral fins, a whiplike tail, and two hornlike fins that project forward from the head.

蝠鲼任一种蝠鲼科的鳐鱼,生活在热带或副热带海域,有大而扁平的身体和翼状的胸鳍,以及鞭状的尾,头的前部有两个角状的向前突出的鳍

Anomalous extensive drought and megatherm weather from 1998 autumn to 1999 spring is diagnosed,and it is found that El Nino and La Nina events are the important climatic background resulting in anomlous climate in Guangxi.Exceptional weakness of cold air intruding into Guangxi,positive anomalies of the heigh field over the Qinghai-Xizang plateau,weakness of the Indochina trough,a sustained strong subtropical high,and less and weak tropical cyclones influence are main contributing factors to the long sustain...

对广西1998 年秋至1999 年春出现的大范围干旱伴高温的异常天气进行了诊断分析,发现厄尔尼诺与拉尼娜事件是导致广西气候异常的重要气候背景,入侵广西的冷空气异常偏弱,高原高度场偏高,印缅槽偏弱,副热带高压持续偏强,热带气旋影响偏少,强度偏弱,是导致广西1998年秋至1999年春罕见的长时间高温、少雨、异常干旱的主要原因。

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