1) extra tropical western Pacific high
副热带西太平洋高压
1.
Evidence suggests that the increase (decrease) in intensity of Ehuocik blocking high in out of phase with the decrease (increase) in intensity of extra tropical western Pacific high in the western part is mostly responsible for the increase .
结果发现 ,鄂霍次克海附近阻塞高压加强 (减弱 )和副热带西太平洋高压西部强度减弱 (加强 )的反位相变化是造成长江中下游和东北大部分地区的降水增加 (减少 )的重要原
2) West Pacific subtropical high
西太平洋副热带高压
1.
A probe into the maintaining mechanism of one type of the double-ridges processes of West Pacific subtropical high;
一类西太平洋副热带高压双脊线过程维持机制初探
2.
Using OLR field to describe West Pacific subtropical high;
利用OLR场对西太平洋副热带高压的描述
3.
Analysis and Description of West Pacific Subtropical High Using TBB Data;
利用TBB资料对西太平洋副热带高压特征的分析和描述
3) subtropical high
西太平洋副热带高压
1.
An inverse correlation between the isotope time series of peat cellulose from Jinchuan and Hongyuan has been used for indicating the subtropical high activities of the Western Pacific Ocean.
文章以金川和红原两组泥炭纤维素Δδ1 3C时间序列值的反向变化来指示西太平洋副热带高压活动变化。
4) Western Pacific subtropical high
西太平洋副热带高压
1.
Interdecadal Change in Western Pacific Subtropical High and Climatic Effects;
西太平洋副热带高压的年代际变化及其气候影响
2.
Relationship between the Western Pacific Subtropical High and sea-surface temperature anomaly
西太平洋副热带高压与海表温度的关系
3.
Using the daily and monthly NCEP/NCAR reanalysis data,Outgoing Longwave Radiation(OLR) data,monthly precipitation of 160 stations in China and daily precipitation of 45 stations in South China,relationships among sustained torrential rain in South China,anomalous convection over the Bay of Bengal and evolution of the western Pacific Subtropical High in June 2005 are analyzed.
利用NCEP/NCAR再分析逐日及逐月资料、NOAA卫星观测的向外长波辐射(Outgoing Long-wave Radiation,OLR)资料、我国160站月降水资料及华南45站逐日降水资料,分析了2005年6月华南持续性致洪暴雨的发生与孟加拉湾对流异常活跃及西太平洋副热带高压演变的关系,并对华南6月有无持续性大范围暴雨年进行合成分析,结果表明华南持续性大范围暴雨发生的年份,孟加拉湾对流相对活跃,西太平洋副高强度偏强、位置偏西;反之亦然。
5) The westwest-extending ridge of west Pacific subtriopical high
西太平洋副热带高压西伸脊点
补充资料：热带
1.赤道两侧南回归线和北回归线之间的地带称"热带"，也叫"回归带"。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条