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1)  subtropical high-pressure belt
副热带高压区
2)  subtropical anticyclone
副热带高压
1.
The progress in the dynamical study of the formation and variation of the subtropical anticyclone during the past decade is reviewed.
首先回顾了近年来关于副热带高压形成和变异研究的若干动力学进展,阐明夏季副热带"四叶型"LOS-ECOD加热分布型的内涵。
2.
This study investigates the influences of the minus-SSTA over the northern Pacific Ocean in the mid-latitudes in Summer of 1993 on the subtropical anticyclone by using the T42L9 global circulation spectral model developed by the IAP/CAS.
利用中国科学院大气物理研究所的T42L9全球大气环流模式,研究了1993年夏季北太平洋中纬度海温异常对西太平洋副热带高压的影响。
3)  subtropical high
副热带高压
1.
Comparison and analysis of the cold high approaching to sea and subtropical high;
入海冷高压与副热带高压对比分析
2.
Characteristic timescales and temporal-spatial changes of the subtropical high over the northern pacific in summer;
夏季北太平洋副热带高压年际变化的特征时间尺度及其时空演变
3.
Statistic relation between sea ice in the Bohai Sea and North Yellow Sea of China and the subtropical high in the Pacific Ocean
渤海、北黄海冰情与太平洋副热带高压的统计关系
4)  subtropical high pressure
副热带高压
1.
Connection between the short period evolution structure and vertical motion of the subtropical high pressure in July 1998;
1998年7月副热带高压短期结构演变特征与垂直运动的关系
2.
Analyzing 14 ENSO incidents occurring during the period of 47 years, we have reached a conclusion that abnormal warming up of water in the east Pacific Ocean near the equator corresponds with that the subtropical high pressure of the west Pacific Oceauis continuously at high side and its location is at south side in the early summer.
对近47年以来出现的14次ENSO事件分析,发现1991年~1997年厄尔尼诺赤道增暖首先出现位置和增暖开始的时间,与一般认为的“上半年发生的厄尔尼诺,海温正距平具有自东向西传播的特征,而下半年发生的厄尔尼诺,海温正距平具有自西向东传播的特征”不一致;并分析赤道东太平洋海温异常增暖对应初夏西太平洋副热带高压持续偏强、位置偏南,与我省夏季降雨多、夏旱轻有较好的一致性。
5)  subtropical high belt
副热带高压带
6)  Subtropical anticyclone over SCS
南海副热带高压
补充资料:副热带
亚热带。
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