1) China precipitation
中国降水
1.
By using the daily precipitation data of 490 stations in China from 1960 to 2000, the characters of climate and anomaly for intraseasonal oscillation (MJO) of China precipitation are studied in this paper.
本文用1960～2000年中国490站逐日降水资料,研究了中国降水季内振荡(即MJO)的气候及其异常特征。
2) precipitation in china
中国降水
1.
Study on Correlations between Decadal Variability of Tropical and North Pacific SSTA and That of Precipitation in China;
热带及北太平洋SSTA与中国降水年代际变化的相互关系及其机制研究
3) summer precipitation in China
中国夏季降水
1.
The relation between the interannual variation of the east Asian summer monsoon (EASM) and the summer precipitation in China is investigated in terms of the east Asian summer monsoon intensity index.
以海陆气压差定义的夏季风强度指数为依据，讨论了东亚夏季风年际异常与中国夏季降水的关系。
4) autumn rainfall in China
中国秋季降水
1.
Based on the 1950—1999 data of Hadley Center monthly global SST,NCEP/NCAR reanalysis and rainfall over 160 stations in China,investigation is undertaken for the difference in autumn rainfall in China between years of Indian Ocean Dipole(IOD) only and IOD and ENSO concurrence,so as to study effects of ENSO on the relationship between IOD and autumn precipitation in China.
利用1950—1999年Hadley中心全球海温资料、NCEP/NCAR再分析资料和中国气象局整编的160站降水资料,通过讨论印度洋偶极子(IOD)独立发生时及IOD与ENSO联合发生时中国秋季降水的差异,研究了ENSO对IOD与中国秋季降水关系的影响。
5) summer rainfall in China
中国夏季降水
1.
Relationship between index of land-sea thermal difference and summer rainfall in China;
东亚海陆热力差指数与中国夏季降水的关系
2.
Based on 1950～1999 monthly global SST from Hadley Center,NCAR/NCEP reanalysis data and rainfall over 160 stations in China,investigation is conducted into the difference of summer rainfall in China between the years with IOD happening independently and those with IOD happening along with ENSO so as to study the effects of ENSO on the relationship between IOD and China precipitation in summer.
利用1950～1999年Hadley中心海温资料、NCEP/NCAR再分析资料和中国160站降水资料,通过讨论印度洋偶极子(IOD)独立发生时及IOD与ENSO联合发生时中国夏季降水的差异,研究了ENSO对IOD与中国夏季降水关系的影响。
3.
The effects of spring Eurasian snow cover on Northern Hemispheric atmospheric circulation and summer rainfall in China have been explored using the latest version of general circulation model (GCM) CAM3.
1版本模式,研究了欧亚大陆春季积雪异常对北半球大气环流和中国夏季降水的影响。
6) Spring and summer precipitation in China
中国春夏季降水
补充资料：冰雹(见降水)
冰雹(见降水)
hail
bingbQo冰雹(hail)见降水。
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