1) subtropical summer monsoon trough
副热带夏季风槽
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) tropical summer monsoon
热带夏季风
1.
Basing on the NCEP/NCAR 850 hPa averaged wind field in summer and the SST data of GISST from 1950 to 2002,the result that there is some nonlinear relationship between the tropical summer monsoon and ENSO is obtained by using the nonlinear canonical correlation analysis.
采用1950—2002年NCEP/NCAR53 a夏季平均的850 hPa低空风场和GISST海温资料,通过非线性典型相关分析(Nonlinear Canonical Correlation Analysis;NLCCA),得到热带夏季风对ENSO的响应存在一定的非线性。
补充资料:副热带
亚热带。
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