1) typhoon rain
台风雨
1.
Flood in Daguangba river basin is caused by typhoon rain.
大广坝流域洪水由台风雨形成,台风登陆路径的不同造成台风期降雨中心位置分布的差异,另外流域上游的友谊水库对下游大广坝水库天然入流方式的改变,直接导致洪水预报方案的改变,即从全流域产汇流计算改为“上下库区间汇流计算和库区产汇流计算”。
2) typhoon storm
台风暴雨
1.
This paper analyses "Taili" typhoon storm flood above Shanxi Reservoir dam site of Feiyun River Vally,reservoir flood operation and flood control benefit.
对飞云江流域珊溪水库坝址以上“泰利”台风暴雨洪水及水库洪水调度和防洪效益进行了分析。
2.
9612 typhoon storm in the regenerated tropical mountain rainforest watershed at Hainan Island s Jianfengling were analyzed comparatively.
另一种是ｐＨ值、Ｋ和Ｓｉ元素，在暴雨期间，浓度随降雨强度的增强而减小，并在最大降雨强度时达到最低值；④台风暴雨能加速森林生态系统养分的丧失；⑤暴雨是热带地区普遍缺磷的一个重要原因；⑥在９６１２号台风暴雨过程中，养分的输入输出变化表现为Ｎ，Ｍｇ，Ｃａ和Ｋ的输入大于输出，Ｐ，Ａｌ，Ｓｉ为输出大于输入。
3) typhoon rainstorm
台风暴雨
1.
The blown-up theory and the construction forecast of the V-3θ chart are used to analyze and verify the typhoon rainstorm of the last flood season in South China.
运用溃变理论及V 3θ图结构预测法对华南后汛期台风暴雨进行预测及检验。
2.
It is found that moisture and strong ascending motion produced typhoon rainstorm directly and the rainstorm has a close relation to vorticity,divergence at 850hPa.
模拟结果表明:充沛的水汽和强烈的上升运动是造成台风暴雨的直接原因,降水与850hPa涡度场、散度场有较好的对应关系。
3.
no changing topographic height, double topographic height, half topographic height and erased topographic to simulate the typhoon rainstorm of “Bilis” landing (period.
采用MM5模式,以2000年10号(0010)台风“碧利斯”为个例,选取台风登陆前后时段,采用不同地形高度来模拟该时段台风暴雨过程。
4) typhoon torrential rain
台风暴雨
1.
At the same time, typhoon torrential rain is a kind ofimportant precipitation form in Middle and Eastern China.
台风暴雨是台风灾害的主要形式之一,同时也是我国中东部地区的一种重要降水类型。
5) typhoon heavy rainfall
台风暴雨
1.
By using conventional data,HLAFS grid point data and GMS 5 stationary satellite infrared cloud picture,the diagnosis and research on synoptic characteristics of typhoon heavy rainfall in the year of 2001 in China,a especially severe rainfall caused by tropical depression on 5th August in Shanghai and physical conditions of severe rainfall from typhoon Liulian (0103) are performed.
利用常规资料、HLAFS格点资料和GMS 5静止卫星红外云图 ,对 2 0 0 1年我国台风暴雨的天气气候特征、热带低压造成的“8 5”上海特大暴雨及 0 1 0 3号台风“榴莲”的强暴雨形成的物理条件进行了诊断分析研究 ,并探讨了动力学、热力学和大气层结稳定度等物理因子在这两次强暴雨过程中的主要作用。
2.
It is revealed that convectionalcloud cluster from South China Sea and Gulf Bengal keep infloodingcontinuously into the typhoon circulation, the convergence of the vapor at lowlever and the divergence of the vapor at high lever, and the strong risingmovement are the main reasons of the occurance of typhoon heavy rainfall.
本文首先对0312号台风“科罗旺”的形势场进行分析，发现南海、孟加拉湾一带对流云团不断流入台风环流，低层水汽辐合、高层水汽辐散和强烈的上升运动是产生台风暴雨的主要原因。
3.
It shows the causes of typhoon intensity weakening slowly, and the favorable environment of typhoon heavy rainfall generating.
利用风云2号可见光云图分析了台风的发展过程,揭示了此次台风强度减弱缓慢原因,以及台风暴雨产生的有利环境。
6) typhoon rainfall
台风暴雨
1.
In this poper, five cumulus parameterization schemes with the send-prognostic method are tcsted and their availability in the typhoon rainfall system is discussed.
本文使用半预报方法检验了五种积云参数化方案，并讨论了它们在台风暴雨中的适用性，结果表明：Arakawa－Schubrt方案能最好地描述台风暴雨过程Q1和Q2的垂直结构，该方案所要求的云功函数准平衡假设在台风暴雨过程中能够成立；而Kuo－type方案由于假设了加热和增温分别线性正比于Ts－T和qs一q不能很好地描绘实际Q1和Q2的垂直结构，但当改进云温的求取法后，参数化结果会得到较大改善。
2.
Numerical experiments show that the neutral typhoon track, typhoon rainfall distribution and intensity are obviously affected by the interactions of the factors including outer—region circulation,ambient subtropical high system, subsynoptic scale jet steam and topographic forcing.
研究了7805号登陆台风暴雨地形增幅效应问题。
补充资料：宿鸟远峡化台遇风雨
【诗文】：
孤鹤长松颠，独宿万岩雨。龙湫在石脚，引袂时一取。
惊风折乔木，飞焰猎窗户。半夜霹雳声，高斋有人语。
【注释】：
【出处】：
全唐诗：卷568-36
孤鹤长松颠，独宿万岩雨。龙湫在石脚，引袂时一取。
惊风折乔木，飞焰猎窗户。半夜霹雳声，高斋有人语。
【注释】：
【出处】：
全唐诗：卷568-36
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条