在中国东部，平均降水强度极值出现的范围趋于扩大。
In eastern China, much above normal mean intensity of precipitation tends to increase.
中国东部的雨量较多，年平均降水量为250—400毫米。
The eastern part of China has more rainfall, with an annual average of 250-400 mm.
因此，该模式可以应用于中国东部夏季降水的模拟研究。
So, the model can be applied to the study of summer rain in Eastern China.
利用一个具有门限的非线性随机动力气候模式对中国东部江淮流域的降水进行了分析。
This paper applies a non linear stochastic dynamic model with threshold to analyze the rainfall in the Yangtze and Huaihe river basins of east China.
中国东部降水同样存在数百年的趋势变化，且存在明显的区域差异，特别是华北与江南的低频变化趋势几乎相反。
Precipitation showed the inter-centennial tendency having obvious spatial difference, especially in North China and south of the Yangze River, is opposite to the low frequency change trend.
它使得中国东部地区降水减少，由此造成的降水减少占末次盛冰期降水减少的25%—50%。
The impact on precipitation in the east coastal region of China was most significant, accounting for 25%-50% of the total precipitation reduction during the LGM.
气溶胶使得冬季和夏季中国东部大部分地区的降水减少。
The aerosol leads to a reduction of precipitation in eastern China both in winter and summer.
该模式可应用于中国东部夏季风降水的研究。
Therefore we consider that the model can be applied to the study of summer precipitation simulation over Eastern China.
这些都说明东中国海及邻近海的热力状态可能是影响我国东部夏季降水的重要因子之一。
Consequently, it is suggested that the thermal state of the East China seas and their adjacent seas maybe one of the important factors affecting the summer precipitation in East China.
这些都说明东中国海及邻近海的热力状态可能是影响我国东部夏季降水的重要因子之一。
Consequently, it is suggested that the thermal state of the East China seas and their adjacent seas maybe one of the important factors affecting the summer precipitation in East China.
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