This is helpful for East Asian summer rainfall prediction.
这对东亚夏季年际降水异常具有一定的预测意义。
No natural pollen can grow on account of inadequate summer rainfall.
因夏季雨水不足，自然花粉无法增多。
POP analysis of summer rainfall TBO of east China get two main modes.
东部夏季降水tbo的POP分析得到两个主要空间型。
East China summer rainfall TBO is closed with air circulation anomaly.
中国东部夏季降水tbo空间模态与大气环流异常关系密切。
Since earliness is not an issue, nor is summer rainfall, his only concern is clean fruit.
因为提早成熟和夏季雨水不是主要问题，所以他唯一关心的是果实的干净。
The correlation between summer rainfall over China and ENSO is as well different between HCP and LCP.
并仕，HCP和LCP时期中国夏季降水和ENSO的关系也有明显差异。
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。
Based on the last 40 year data, the distributive patterns of summer rainfall in the east of Chi-na are given.
分析了近40年来我国夏季降水的分布特征、形成原因及其变化规律。
The spring temperature of these two regions can explain 15% of the difference in summer rainfall in northern China.
这两个地区春季的温度能解释农牧交错带夏季降水方差的15 %左右。
The spring Arctic sea ice might provide a precursor for both Chinese summer rainfall and the summer monsoon mode P31.
春季北极海冰对于中国夏季降水变化和夏季风模态P 31均是先兆因子。
Since the summer rainfall abnormality has closely relationship with both the soil moisture and temperature abnormality.
初步揭示了前期土壤湿度与后期降水、气温异常间的准半年相关关系。
The rise of the worldwide temperature will increases the summer rainfall and the frequency of typhoon in the studied area.
全球气温上升将使本区夏季降水增多、台风频率增大。
Wang S W, Huang J B. 2006. The instability relationship between summer rainfall over North China and India[J]. Prog Nat Sci, 16(8):980-985.
王绍武， 黄建斌。 2006。中国华北与印度夏季降水遥相关的不稳定性[J]。自然科学进展，16（8）：980-985。
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。
Therefore, the spring sh circulation anomaly is one of important short-term climate predictors for summer rainfall over the Yangtze River Valley.
因此，春季南半球环流异常可以作为长江中下游夏季旱涝主要短期气候预测因子。
Deserts would start encroaching along Europe's southern borders. British agriculture would be increasingly difficult to sustain as summer rainfall dropped.
欧洲南部有将开始被沙漠侵袭，英国的农业将因为夏季降雨量的减少而日益艰难。
In the paper, the relationship between the summer rainfall in China and the intensity of the northern Pacific oscillation (NPO) in winter is analysed.
本文分析了冬季北太平洋涛动与我国夏季降水的关系。
The results are as follows:(1) The easterly intensity has a sustainable positive relationship with summer rainfall over North China from spring to summer.
结果表明：（1）从春季到夏季，东风强度与华北夏季降水具有显著而稳定的正相关关系。
Otherwise, the normat correlation exists between the corresponding SST in west sea area of NINO and the Kuroshio and the summer rainfall in southern Fujian.
另外，闽南地区后汛期降水量与同期NINO西海区和黑潮海区的海温成正相关关系。
The summer rainfall in China is influenced directly by the abnormal vertical motion, which is related closely to the abnormal heat sources in the atmosphere.
大气热源的异常是通过直接影响垂直运动场的异常，进而影响到我国的夏季降水的异常。
And we find that the precipitation was catastrophe in 1978. The water vapor of the Bengal Gulf and subtropical high was related to the Plateau summer rainfall.
北区年降水量变化较小。青藏高原降水量在1978年由少雨期转为多雨期，青藏高原夏季降水与孟加拉湾的水汽输送及副高的水汽输送关系密切。
The analysis of summer rainfall intensity in China is carried on for the purpose of practical application of climatic data to the natural resources development.
本文关于中国夏季日降水强度的分析，是以对国民经济服务为目的的。
The summer rainfall over NC was greater than normal when the EASM was strong, and while drought occurred along the middle and lower reaches of the Yangtze River.
当东亚夏季风强时，华北夏季降水偏多，同时长江中下游少雨；
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。
When the effect of sea surface temperature as a predictor tends to be weakened at present, AAO can be used as an important predictor for summer rainfall prediction in China.
在当前海温预报因子作用减弱的情况下，AAO有可能成为中国夏季降水预测的一个重要预报因子。
Therefore, the influence of AAO on summer rainfall in China is related to the decadal background. After 1976, the influence of AAO tended to intensify and extended more northward.
这说明AAO对中国夏季降水的影响与年代际背景有关，1976年之后，AAO对中国夏季降水的影响增强，影响范围更加偏北。
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。
Chen Dongdong, Dai Yongjiu. 2009a. Characteristics and analysis of typical anomalous summer rainfall patterns in Northwest China over the last 50 years[J]. Chinese J Atmos Sci, 33(6):1247-1258.
陈冬冬，戴永久。 2009a。 近五十年中国西北地区夏季降水场变化特征及影响因素分析[J]。大气科学，33（6）：1247-1258。
The results of the analysis indicate that:1)North China has more summer rainfall during strong East Asian summer monsoon years but less summer rainfall during weak East Asian summer monsoon years.
结果表明：（1）通常在强东亚夏季风年华北夏季降水偏多，在弱东亚夏季风年华北夏季降水偏少。
Summer rains constitute around 80% of the country’s annual rainfall.
夏季降雨量占年均降雨量的80%。
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