2) rainfall in South China
华南降水
1.
Results show that,positive(negative) surface temperature anomalies over middle and lower reaches of Yellow River,and negative(positive) anomalies in South China,indicates more(less) rainfall in South China and.
结果表明:当黄河中下游及其附近地区地表气温偏高(低),华南偏低(高),则华南降水偏多(少),而江黄流域降水偏少(多)。
3) continual torrential rain in South China
华南持续强降雨
1.
Anomalous features of Asian summer monsoon and their influence on the continual torrential rain in South China in early summer of 2005 are analyzed.
利用国家气象中心1957-2006年基本观测站点逐日降水量资料,NCEP/NCAR所提供的2005年5-7月逐日OLR资料、日平均再分析资料及其相应的多年平均资料,采用诊断分析方法讨论了2005年初夏华南持续强降雨雨情、亚洲季风异常特征及其对华南持续强降雨的影向。
5) precipitation in rainy season in South China
华南汛期降水
6) pre flood season rainfall in Southern China
华南前汛期降水
1.
By using the data of latitude of Antarctic sea ice (1973～1989) as well as cyclone numbers (1972～1981) over the Southern Hemisphere, the influence of the changes of Antartctic sea ice on the pre flood season rainfall in Southern China has been analyzed.
利用１９７３～１９８９年南极海冰北界资料和１９７２～１９８１年南半球气旋资料，分析南极海冰变异对华南前汛期降水的影响。
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