单位时间或某一时段的降水量。
...降水强度 雨季划分 典型旱涝年 新疆博州地区 [gap=1484]Keywords】: spatial-temporal distribution of precipitation,precipitation intensity,determination of the rainy season,typical drought or flood year,Bole region in ...
基于574个网页-相关网页
... energy intensity能源强度;能源密集度 rainfall intensity降雨强度;降水强度;暴雨强度 current intensity电流强度 ...
基于118个网页-相关网页
... the index of precipitation intensity 降水强度指数 distribution ratio of precipitation intensity 降水强度分配比 intensity of precipitation 降水强度 ; 降雨强度 ...
基于22个网页-相关网页
...：降水落到地面后，未经蒸发、渗透、流失而在水平面上 积聚的水层深度(mm)（固态降水指融化后的厚度） 降水强度(rain intensity) ： 单位时间内的降水量 降水绝对变率：Ri-R，又称降水距平，―+‖:偏多，―-‖偏少，反映 降水的年际变化。
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日降水强度 SDII
降水强度频率曲线 Rainfall intensity frequency curve
降水强度指数 the index of precipitation intensity
降水强度与频数 precipitation intensity and frequency
年平均降水强度 mean annual precipitation intensity
降水强度分配比 distribution ratio of precipitation intensity
地面降水强度 surface rainfall intensity ; Surface precipitation intensity
降水强度类属矩阵 rainfall intensity category matrix
Through altering the main programming of the weather model in the integrated dust model system and displaying the main programming of both water vapor and convection parameterized schemes, we calculated and provided the data about precipitation intensity.
本文通过修改“集成沙尘模式系统”的天气模式主程序、显式水汽方案和对流参数化方案主程序,来计算并提供降水强度数据。
参考来源 - 沙尘模式中湿沉降过程的参数化及模拟试验ResultsThe trend of summer precipitation intensity in Anhui province was strenthened and extreme precipitation events growed in number,Huaibei district most significant. The mean date of the Meiyu onset was June 16 and the end of Meiyu period was July 10.
结果结果表明:夏季降水强度增强趋势明显,极端降水事件增多,以淮北显著;夏季淮北准2年和准8年周期振荡较明显,沿江江南准16年周期较明显;全省平均入梅日期6月16日,出梅为7月10日,梅雨量年际变幅大。
参考来源 - 安徽省夏季降水变化及其对旱涝的影响研究·2,447,543篇论文数据，部分数据来源于NoteExpress
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.
而当云体温度低并且含水量很少时，微粒并不能增加云体的厚度和降水强度。
In contrast, aerosols did not increase the thickness or precipitation intensity of clouds which had cold bases and no ice.
还以实际降水数据检验了降水强度的指数分布，在此基础上求出了模型的解。
Then based on the exponential distribution of precipitation the model was solved to give the equivalent precipitation of each level in the landscape.
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