汛期降水量,precipitation amount in flood period
1)precipitation amount in flood period汛期降水量
英文短句/例句
1.The Comparative Analysis of Precipitation Variations during the First and Second Flood Season in Chaozhou by Wavelet Analysis潮州市前、后汛期降水量的多时间尺度特征对比
2.Variations of the Spring Rain Season Onset Time in Fujian Province and its Relationship with the Subsequent Precipitation福建春季开汛时间变化特征及其与后期降水量关系
3.It might be a useful index for rainfall forecast in China.这是每年汛期降水预报的一个指标.
4.Typhoon Activity Effect on Precipitation over North China During Flood Season;台风活动对华北汛期降水影响的研究
5.Precipitation Test by WRF Model in Jiaozuo Flood Season in WRF模式对焦作汛期降水的检验
6.Changes of Flood-Season Severe Precipitation over South China in 2071-210021世纪末华南汛期强降水变化分析
7.Anomalies of the Northeast China Floods Season Precipitation and the Relations with SSTA;东北地区汛期降水异常及其与海温异常的关系
8.Analysis on the characteristic of the precipitation and the affection of the drought-flood risk in the high water season in Guiyang;贵阳市汛期降水特点及对旱涝灾情影响的分析
9.The Analysis of Circulation Background and Prediction Research of Precipitation in Rainy Season in Jiangxi Province in 江西省汛期降水环流背景分析及预测研究
10.Characteristics of Extreme Precipitation Events and Their Circulations in Guizhou贵州主汛期极端降水事件及其环流特征分析
11.The Circulation Features and Spatial-Temporal Characteristic Of Meiyu Distributions In Zhejiang In Recent 50 Years近50年浙江梅汛期降水分布的时空及环流特征
12.Probability distribution of precipitation extremes during raining seasons in South China华南地区汛期极端降水的概率分布特征
13.SVD ANALYSIS BETWEEN THE ANNUALLY FIRST RAINING PERIOD PRECIPITATION IN THE SOUTH OF CHINA AND THE SST OVER OFFSHORE WATERS IN CHINA华南前汛期降水与我国近海海温的SVD分析
14.Temporal and Spatial Variations of Extreme Precipitation Events of Flood Season over Sichuan Basin in Last 50 Years近50年四川盆地汛期极端降水事件的时空演变
15.Climate Characteristics of Precipitation and Phenomenon of Drought-flood Abrupt Alternation during Main Flood Season in Huaihe River Basin淮河流域主汛期降水气候特征及“旱涝急转”现象
16.ANALYSIS OF PRECIPITATION IN THE ANNUALLY FIRST RAINY PERIOD AND GENERAL CIRCULATION IN THE SOUTH OF CHINA华南前汛期降水异常及其环流特征分析
17.Analysis and Study on Hydrological Time Series Similarity Search水文时间序列相似性查询的分析与研究——以漯河站、何口站汛期降雨量相似性查询为例
18.Multiple-time-scale Variability Analyses of Rainfall during Rainy Season over North China and Study on It"s Evolution of Large-scale Precipitation Conditions华北汛期降水的多尺度变化及其大尺度降水条件的演变研究
相关短句/例句
Precipitation during the flood period from June to August主汛期降水量
3)floods season precipitation汛期降水
1.The results showed that there is a high correlation betweenfloods season precipitation in Zhejiang and SSTA.根据1951年1月～1999年12月浙江省23站汛期降水的资料,寻求海温因子对浙江省汛期降水的影响,结果表明:热带海洋海温异常与浙江省汛期降水异常有较好的对应关系。
2.In the study of the mechanism of the precipitation anomalies, the discovery is then chiefly to study the effect of SSTA on rainfall in floods season in TPNES, concluding that there is a high correlation between thefloods season precipitation in.本文在对中国西北地区降水气候特征及其与北方气旋相关关系的分析基础之上，重点对青藏高原东北侧汛期降水异常以及其同期和前期的影响因子进行了分析研究，并侧重寻求前期SSTA对青藏高原东北侧降水的影响，结果发现澳大利亚东侧SSTA及分布型与高原东北侧汛期降水异常有较好的对应关系。
4)rainy season precipitation汛期降水
1.(2) The general interdecadal variations period of therainy season precipitation is 20-25a in the past 58 years.结果表明:近58a来柳州市汛期降水主要呈波动性变化,线性趋势变化不明显,但前汛期降水总体呈上升趋势,降水量约增加87mm;后汛期降水量总体呈下降趋势,约减少了89mm。
5)second rainy season后汛期降水
1.in this paper, the inter-annual variational characterization of preacipitation of 1951～1990 during the annuallysecond rainy season in south Guangxi and low-latitude circulation system is studied.本文用近４０年（１９５～１９９０年）降水资料，统计出广西南部后汛期降水的年际变化特征，并初步分析了低纬度环流系统对广西南部后汛期降水年际变化的影响。
6)typhoon season precipitation台汛期降水
1.Thetyphoon season precipitation of Aug.嘉兴8～9月台汛期降水与台风影响关系密切,台风影响多,降水正常到偏多,台风影响少,降水正常到偏少。
2.Moving average method and wavelet translation method have been used to analyze flood season precipitation,which including Meiyu season precipitation andtyphoon season precipitation,in JiaXing from 1954 to .对1954至嘉兴汛期降水,包括梅汛期和台汛期降水做滑动平均和小波分析,发现嘉兴汛期梅汛期降水,在降水偏多的50年代和80~90年代都存在着3~4 a周期变化,而台汛期降水存在5 a和9~10 a的周期振荡。
延伸阅读
降水量降水量amount of precipitationJ iangshuiliang降水工(一nt of preciPitation)一定时段内从天空降落到地面上的液态或固态水，未经蒸发、渗透、流失而在地面上积聚的水层深度。单位为毫米，气象观测中取一位小数。有时也称为雨量。降水量一般用雨量筒测定，所以降水量中可能包含少量的露、霜和淞等。在自然资源研究中，常用的降水量有年、季、月、旬和生育期的降水量。中国全国平均年降水量为63()毫米，自沿海向内地、自东南向西北递减。东南沿海的广东、广西东部、福建、江西和浙江大部以及台湾等地区年降水量为15仪】~2(XX)毫米;长江中下游地区为1以X)~1召】〕毫米;淮河、秦岭一带和辽东半岛年降水量为8(X)、1仪五)毫米;黄河下游、渭河、海河流域以及东北大兴安岭以东大部分地区为5《】)~750毫米;黄河上、中游及东北大兴安岭以西地区为2(X)~中以)毫米;西北内陆地区年降水量为100~2(X)毫米;新疆塔里木盆地、吐鲁番盆地和柴达木盆地不足50毫米，盆地中心不足20毫米。中国降水量季节分配不匀。春季降水，长江流域中下游占全年so%~45%，新疆占30%~35%，大部分地区小于20%;夏季降水，长江中下游、华南和新疆部分地区占全年50%以下，全国其他地区都大于50%;秋季降水，西南地区占全年25%，其他地区不足20%;冬季降水，长江中下游、华南大部、新疆地区占全年10%~巧%，其他地区都在10%以下。降水不匀易形成旱涝灾害。下页附图为中国年降水量分布图。(霍治国)
