Based on summer precipitation data, by using trend analysis, wavelet transform methods, the changes of summer rainfall in North China and in India were analyzed.
利用华北和印度夏季降水资料，采用趋势分析、小波变换等方法，对两地区夏季风降水进行了对比分析。
It is forecasted that less than normal rainfall is expected in near future in North China and Huang-Huai Plain.
据预测，今后一段时期，华北、黄淮地区降水仍比常年同期偏少，主要江河来水总体将继续偏枯。
This pattern of SSTA distribution is related to summer rainfall anomaly of North China by means of the tropical convection activity and general circulation in the middle and high latitude. iv.
这种海温异常分布型可通过夏季热带对流活动和中高纬大气环流与华北夏季降水异常产生联系。
There was consanguineous relationship between summer rainfall anomaly in North China and continual circulation anomaly from spring to summer .
华北夏季降水异常与从春到夏的持续环流异常密切相关。
The effect of different rainfall years and different water and nitrogen management ways on winter wheat and summer maize was studied in northern part of north China Plain.
在华北平原北部研究了不同降水年型、不同水氮管理措施对冬小麦和夏玉米产量和氮素平衡的影响。
The results indicate that there is better relationship between the departure accumulation of the index STPNA (PNA teleconnection pattern of the North Pacific SST) and flood season rainfall in china.
结果表明：STPNA（海温的太平洋北美遥相关型）指数距平累积和与江淮流域夏季降水有密切的相关，与全国雨带的类型也有较好的联系。
In this paper, two wet springs and two dry springs of North China have been chosen to study the effect of large-scale persistent rainfall anomalies on the land surface processes in semi-arid regions.
本文以华北地区春季两个多雨年和两个少雨年为例，研究半干旱地区大范围持续性降雨对地面物理过程的影响。
The influence of sea surface temperature sustained heating in the North Pacific on flood season rainfall in China is discussed by the departure accumulation of the sea surface temperature.
用海温距平累积和讨论了北太平洋海温异常持续加热对夏季中国降水和大气环流的影响。
These EASM modes affect Chinese summer rainfall variation, particularly in north and northeast China.
这些夏季风模态均对中国降水变化产生影响，特别是在华北和东北地区。
When the AAO in boreal spring was stronger before 1976, there was more rainfall in the south of the Yangtze River and north China and less rainfall in the Yangtze-Huaihe River valley.
在春季AAO偏强的情况下，1976年之前，长江以南地区和华北地区降水偏多，江淮流域降水偏少；
This basin is located in north China continental arid and semi-arid climate zones . Low rainfall and strong evaporation, weak ecological environment in general.
该盆地地处我国北温带大陆性干旱-半干旱气候区，总体上降雨稀少、蒸发强烈，生态环境脆弱。
Therefore the monsoonal rainfall was suppressed in North China and enhanced in South China.
长江流域和华南地区则相反，季风降水降水加强。
Therefore the monsoonal rainfall was suppressed in North China and enhanced in South China.
长江流域和华南地区则相反，季风降水降水加强。
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