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Lying in the North Hemispheric Subtropical High, the middle reaches of the Yangtze, as a key passage of the East Asian monsoon, is climatologically characterized by the energy exchange between the trade wind and westerlies as well as water-vapor convergence of the Southeast and Southwest monsoons.

长江中游地处北半球副热带,是东亚季风的必经之地。副热带附近东风与西风之间的能量交换和东南季风与西南季风的水汽辐合造就了该区环境的过渡带特征,使它灵敏地响应气候的变化。

Based on observation data, numerical simulation and theory of ocean circulation, it is discovered that there is a branch of eastward countercurrent, in addition to the traditional Subtropical Countercurrent in Subtropical Gyre of North Pacific.

依据观测资料,运用数值模式和理论分析,发现了气候平均意义下北太平洋副热带环流中除了传统的副热带逆流外,还存在一支向东的逆流。

Humification proxy has better recorded the subtropical high activities of the Western Pacific Ocean for long period. For shorter period , the humification proxy is less sensitive.

腐殖化度代用指标能很好地记录较长时间西太平洋副热带高压的变化,而对西太平洋副热带高压数十年到百年的频繁波动,则记录不明显。

According to long-term climatology typhoon translation direction is northwestward of South of 30°N, northward around 30°N and northeastward of North of 30°N. In the aspect of interannual variance, typhoon translation direction will be more northward when the subtropical ridge weakens during strong cold years and will be more westward when the subtropical ridge enhances during strong warm years.

并且不论是长期气候平均或年际变化,主要皆会受到太平洋副热带高压环流的影响,即太平洋副热带高压较强且向西延伸时,台风会呈较偏东西向的移动。

Based on the analysis of Sea Surface Height Anomaly from satellite observation, it is proved that the oscillation with period of 70~210 days is dominating in two branches of the eastward countercurrent in Subtropical North Pacific: Subtropical Countercurrent and Hawaiian Lee Countercurrent.

根据对卫星观测的海平面高度资料的分析,进一步证实了在北太平洋副热带两支向东的流(副热带逆流和夏威夷背风逆流)所在的区域内,海平面高度的70~210天周期振荡是主要的低频变化。

Through analysis of the 1999/2000 background field of winter circumfluence, we find that the changes of West Pacific subtropic high and polar vortex are important factors that affect the changes of winter climates characters of our countrys and decay or melt of sea ice in the Bohai Sea .

通过对1999/2000年冬季环流背景资料的分析,发现西太平洋副热带高压和极涡的变化是影响我国冬季天气气候特征变化和渤海海冰生消的重要因素,而副热带高压和极涡等大气活动中心的变化又与赤道东太平洋的厄尔尼诺现象及拉尼娜现象有关。

In the free atmosphere, the location of the zonally averaged ridge of SA deviates completely from this descent arm; in the planetary boundary layer, although the locations of the descent and the ridgeline of subtropical anticyclone coincide with each other due to firictiona, the decent is compensated by horizontal divergence and does not contribute to mass built-up related to the formation of SA.

1研究气候尺度副热带高压尤其是西太副高与垂直运动的关系,发现无论是在自由大气中还是在边界层内,Hadely环流的下沉支都不贡献于副热带高压的形成。

Based upon a systematic review on the study of subtropical anticyclone, in this study, the mechanism linking the formation of subtropical anticyclone in boreal summer to zonally asymmetric diabatic heating is investigated via data diagnosis, theoretical study, and numerical experiment. The complete form of the tendency equation for vertical vorticity development, the NCEP/NCAR reanalysis data, and the IAP/LASG GOALS climate model are employed for the study.

本文在回顾有关北半球副热带高压研究的基础上,基于全型垂直涡度倾向方程,利用NCEP/NCAR月平均资料和IAP/LASG GOALS气候模式,从资料诊断、理论研究及数值试验三方面研究了纬向非对称非绝热加热对北半球夏季副热带高压形态变异影响的物理机制。

Based on T213 numerical forecast products, the abrupt city flood caused by heavy rain in Kunming, Yunnan province on June 24, 2006 is analyzed. The results indicate that the event has a close relation with the southward movement of upper shear line and the peripherad southwest warm and wet airflow.

2006年6月24日云南昆明发生了当年最为严重的一次城市洪涝,利用T213数值预报产品资料对这次突发性洪涝灾害的气象成因进行了诊断分析,结果表明此次强降水与高空切变线南压及西太平洋副热带高压外围西南暖湿气流有关,高空切变线南压有利于引导北方冷空气南下入侵,而西太平洋副热带高压外围西南暖湿气流为此次洪涝灾害的爆发提供了丰富的水汽。

It is found that the variations of the subtropical high of Western Pacific and the westerlies over East Asia are the essential elements to determine the beginning and the end of Mai-yii.

分析指出,西太平洋副热带高压和东亚上空西风气流的变化,是决定入梅和出梅的重要因素,其中东经110°到125°之间的副热带高压脊线的变化更重要。

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