副热带

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。

Especially in Somalia jet stream region ove...

在南印度洋的副热带，全年都有副热带高压控制。

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。

The structure of atmosphere and the evolution of the subtropical jet and subtropical high during the period May 22-July 3, 1958, are studied by means of tropopause map.

本文利用1958年5月下旬至7月初北半球的对流层顶图，分析这段时期内大气的结构，以及副热带急流和副热带高压的变化，得到以下一些事实：(1)在初夏大气的三折结构也是很清楚的。

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。

The equatorward movement of a middle latitude trough-front system into the South China may give rise to the retreating eastward of the subtropical high ridge over the South China Sea.

1994年南海夏季风建立于5月第一候，利用MM5成功地模拟了这一过程，并通过敏感性试验，讨论了中纬度系统和中南半岛及其附近地区的积云对流对夏季风环流建立的影响，结果表明：（1）南下接近副热带一定强度的中纬度槽－锋系统的强迫，可引起南海地区副热带高压脊的减弱东撤。

But we don't care about Battlegrounds.

但我们并不在乎沙场中的显露。

Ah! don't mention it, the butcher's shop is a horror.

啊！不用提了。提到肉，真是糟透了。