1) the East Asian tropical and subtropical monsoons
东亚热带-副热带季风
1.
The progress is reviewed briefly of research on the East Asian tropical and subtropical monsoons by Chinese meteorologists,which involves the features of Asian tropical monsoon onset with its mechanisms,and the index design,associated circulation systems,low frequency oscillations,interannual and interdecadal variations of the East Asian monsoon.
简要回顾了近年来国内在东亚热带-副热带季风方面的研究进展。
2) East Asian subtropical monsoon
东亚副热带季风
1.
Using the monthly mean reanalysis datasets from the NCAR/NCEP,relationships of the interannual variation between an eastern Asia[CD*2]Pacific dipole(APD) mode and the East Asian subtropical monsoon are studied.
利用美国NCEP/NCAR的月平均再分析资料,研究东亚太平洋地区地面气压的耦合模态与东亚副热带季风异常的关系,结果表明:在亚洲大陆和北半球太平洋之间气压场的偶极子模态主要反映了东亚地区东西向气压梯度的异常。
4) East Asian subtropical summer monsoon
东亚副热带夏季风
1.
With 1958 - 1997 NCEP/NCAR reanalysis data and 1961 - 1995 summer (JJA) rainfall and temperature records of 160 stations in China, a new East Asian subtropical summer monsoon circulation index is defined, in which the barotropic and baroclinic components of the circulation are included.
采用大气环流正、斜压分解方法,从东亚副热带夏季风为正、斜压混合型季风观点出发,定义并计算了1958-1997年东亚副热带夏季风环流指数。
5) East Asian subtropical monsoon index
东亚副热带季风指数
6) East-Asian tropical and subtropical summer monsoon
东亚热带季风-副热带季风
补充资料：热带季风气候
又称“热带冬干气候”。分布在纬度5°～10°到15°～20°的内陆到大陆西岸一带。全年气温较高，最冷月平均气温一般在18°c以上。全年降水1500毫米左右，迎风地区达2000～3000毫米以上。有旱季和雨季之分，冬季降水稀少，夏季降水丰沛。主要出现在亚洲的印度半岛、中南半岛、菲律宾群岛以及中国台湾岛南部、海南岛等地。
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