maximum rainfall中文是什么意思

發(fā)音:

中文翻譯
造句

最大降雨量

maximum n. (pl. maximums, -ma ) 極點，最 ...
rainfall 下雨，雨量。
area of maximum rainfall 最大降雨面積
maximum daily storm rainfall 日最大暴雨量
maximum hourly rainfall 最大小時降雨量
maximum possible rainfall 最大可能降水量最大可能降水量; 最大可能降雨量
maximum rainfall intensity 最大降雨強(qiáng)度
maximum rolling rainfall 最高滾存降雨量
abundant rainfall 過量降雨
amount of rainfall 雨水量
ample rainfall 充沛降水; 義沛降水
annual rainfall 年降水量; 年降雨量; 年雨量
antecedent rainfall 前期降雨; 前期影響雨量
areal rainfall 面雨量
artificial rainfall 人工降雨; 人造雨
available rainfall 有效雨量
average rainfall 平均降雨量; 平均雨量
continuous rainfall 連續(xù)降雨
convection rainfall 對流降雨
convectional rainfall 對流雨
convective rainfall 對流性降雨
crystal rainfall 水晶之雨
cumulative rainfall 累積雨量
daily rainfall 日雨量
discharge of rainfall 降雨流量

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例句與用法

The maximum rainfall events in all prefectures in ningixa occurred in the relative warm and stable clouds , d )
寧夏各地逐時降水的極大值均產(chǎn)生于較暖的云團(tuán)或云系中。
When the rainfall reaches 1 mm , the reading from the raingauge with the maximum rainfall in each region will be summarized in the bulletin
當(dāng)雨量達(dá)到一毫米時，每小時天氣報告便會提供各區(qū)過去一小時內(nèi)錄得的最高雨量。
And a scaling lognomial model of rainfall intensity is introduced to represent the affection of temporal scale of duration in annual maximum rainfall intensity distributions
另外，本文提出了暴雨強(qiáng)度的對數(shù)正態(tài)分布模型來表征年最大暴雨強(qiáng)度分布中歷時的尺度影響。
Potential instability existed near 0 in the warm area and between - 10 and 0 in the cold area . the occurrence of potential instability was corresponding with maximum rainfall and maximum vapor content
C附近，冷區(qū)位勢不穩(wěn)定分布在一10一ooc ，位勢不穩(wěn)定出現(xiàn)的時間與地面強(qiáng)降水、水汽最大累積區(qū)出現(xiàn)的時間一致。
The scaling hypotheses is applied to the relationship of annual maximum rainfall intensity and duration . the rainfall intensity - duration - frequency form is proved based on the temporal scaling property of rainfall
由年最大平均暴雨強(qiáng)度隨歷時變化的標(biāo)度性質(zhì)推導(dǎo)出暴雨公式的形式，找到了暴雨公式的理論根基? ?暴雨在時間上分配具有自相似性的結(jié)果。
Heavy rainfall occurred in the warm area , and maximum rainfall lay in the windward slope where the width of raindrop size distribution was b roadened and sometimes it was bimodal spectrum . the shape of rain band in cold area was zonal , and the area of rain band was small
暖區(qū)有明顯的強(qiáng)降水中心，雨強(qiáng)極大值出現(xiàn)在山區(qū)迎風(fēng)坡，降水雨滴譜譜寬較大，有時滴譜呈雙峰型分布；冷區(qū)降水區(qū)常呈帶狀分布，雨區(qū)范圍大，雨滴譜較窄，雨滴譜為單峰型。

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