1) onset of South China Sea monsoon
南海季风建立
3) South China Sea monsoon
南海季风
1.
The effect characteristics of cross-equatorial current on South China Sea monsoon onset and drought/flood in east China have also been analyzed.
应用NCEP/NCAR全球再分析资料和NOAA卫星接收的HIRS-Tb12等资料,研究了东半球夏季越赤道气流的气候学特征、越赤道气流对南海季风爆发的影响、越赤道气流与海温场的联系、以及对华东地区旱涝的影响。
2.
The progressive analysis shows that the transfers in different stages of the Indian monsoon and the south China sea monsoon are also different, which is also the same as the varying of vapour transferring pe.
进一步分析结果表明，在印度季风和南海季风不同的位相阶段，孟加拉湾地区和南海地区的经向水汽输送也是各不相同的，这也和各月经向水汽输送变化基本一致。
3.
Relationships among sunspot, eruption of South China Sea monsoon and tropical storm activity are studied preliminarily by using the statistics during the period between 1949 and 1998.
利用 1 949— 1 998年的资料 ,以统计分析的方法 ,对太阳黑子及南海季风爆发、热带风暴活动的相互关系进行了初步探讨。
4) SCS monsoon
南海季风
1.
Temporal and spatial variations of the weekly mean SST in the South China Sea(SCS) during the SCS monsoon onset period and impact factors have been analyzed by using the weekly mean SST data and daily NCEP/NCAR reanalyzed surface heat fluxes and 10-m wind from 1982 to 2001.
结果表明,南海季风爆发前,SST急剧升高,季风爆发后,SST的变化呈现比较明显的空间差异,南海北部SST继续上升,而南部SST持续下降。
5) South China Sea summer monsoon
南海夏季风
1.
Role of snow depth in spring of Tibetan Plateau in onset of South China Sea summer monsoon;
青藏高原春季积雪在南海夏季风爆发过程中的作用
2.
The regional durative rainstorm during pre-rainy season over South China is defined and its climatic distribution features before and after the onset of South China Sea summer monsoon are studied using daily rainfall data of 175 stations in Guangdong and Guangxi provinces.
对南海夏季风爆发前后区域持续性暴雨的气候分布特征的分析发现,季风爆发前持续性暴雨频数从60年代至今呈现出正态分布的年代际变化特征,而季风爆发后的区域持续性暴雨频数变化则几乎相反;广东省前汛期区域持续性暴雨降水明显比广西强。
3.
The impacts of spring tropical Indian Ocean Sea Surface Temperature(SST) anomalies on the strength of South China Sea summer monsoon(SCSSM) are investigated by analyzing 50 a Reynolds monthly mean SST data and NCEP/NCAR atmospheric reanalysis data.
利用50年的Reynolds月平均海表温度资料和NCEP/NCAR全球大气再分析资料,分析了热带印度洋春季海温异常对南海夏季风强度变化的影响。
6) SCS Summer Monsoon
南海夏季风
1.
Characteristics of the water vapor transporting path in strong and weak SCS summer monsoon years
强弱南海夏季风年水汽输送路径特征分析
2.
The Rossby-wave chain triggered by the convection over BOB might be a main factor for the onset of SCS summer monsoon.
利用RegCM2模式进行数值试验 ,得到中南半岛对流对北半球副高带断裂、进而对孟加拉湾对流建立具有重要影响 ,而孟加拉湾对流建立后激发的Rossby波列又是南海夏季风建立的主要因子之一。
3.
The results show that the warmer SST in the SCS in winter and spring can make a good condition for formation of monsoon circulation in high and low levels, which promote the SCS summer monsoon onset.
使用s-p区域气候模式,通过两组海温异常下的数值试验和2个理想试验来初步探讨南海与中南半岛局地海陆热力对比对南海夏季风爆发的影响。
补充资料：季风(见季风气候)
季风(见季风气候)
j!feng候季风见季风气
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