台风的

The climate characteristics of TCP were analyzed with variance analysis,trend coefficient and linear regression technique,followed by comparison with those of annal total rainfall in East China.Results show that the spatial distribution of TC rainfall is not uniform in East China with the...

结果表明：华东地区登陆台风降水量空间分布不均匀，福建东南沿海地区最大，具有向西北方向递减的趋势，这种趋势与地形等因素有关；TCP的年际变化明显，9 a和15 a周期显著；TCP年代际变化表现为20世纪50年代最多，70年代前开始减少，比华北地区台风降水减少出现的时间提早10 a；TCP与总降水两者的时间演变特点差异较大。

According to the data of tropical cyclone landfalling in China for 1949-2006, climatologically statistical parameters of typhoon season, including the first-landfall TC date, the last-landfall TC date and the duration of typhoon season were analyzed.

利用1949—2006年登陆中国的热带气旋资料，分析登陆 TC 台风季参数的气候特征，结论如下：1 登陆中国的初旋①以南海生成为主（占5成半），终旋以西太平洋为主（高达8成），近50多年来初、终旋源地分别呈现向东北、西北移动的趋势；2 广东初旋最早，广西、浙江终旋较早，广东台风季最长。

Besides the variables of Reisner scheme, they all produce the number contents of rain, snow and graupel, which are also reasonable with observations.

模拟的台风眼半径比原三显式方案更接近实况，模拟的水成物比质量和数浓度与以往实测的台风资料对比在合理的范围内。

In the last of this paper, a typhoon-resistance showhouse of low-rise buildings has been designed and constructed to prove and apply the results of researches obtained in this paper.

本文的最后，通过一抗台风试点房的设计和建造，对本文的研究成果进行了实际的检验和应用，同时对沿海地区的抗台风民房设计和建造起到了示范的作用。

Based on the analysis of potential vorticity and elements on isentropic surface about the typhoon 9608 and its heavy rain outside, the study is to show the PV structure and the interaction with midlatitude weather systems. It shows the feature of severe rainstorm dynamic and thermodynamic process. A picture about the process of heavy rain amplification is given.

通过对9608号台风低压及其外围暴雨位涡和等熵面上物理量场的分析，揭示了台风低压北上诱发暴雨过程的位涡场的结构及冷空气对暴雨增幅的作用，给出此次暴雨增幅过程的图像。

The eddy flow around waterspout of a tub and the cyclone in the bottom of a typhoon are convergent flow-in rotational flow .

水槽排水孔形成的旋涡和台风底层的气旋都是Coriolis力作用下的辐合流入层旋流，台风顶部是辐散流出层气旋。

Through the analysis, it is shown that the Matsa s extratropical transition and the re-intensification are due to the intrusion of cold air from the upper-level trough into the typhoon s circulation.

以一个在陆上长久维持并最终演变成温带气旋的登陆台风&麦莎&为研究对象，通过对其北上变性过程的分析发现，台风与中高纬西风槽的相互作用使得冷空气侵入是其变性加强的原因。

With conditions of approximately actual beckground wind field in typhoons and a barotropic nondivergent model in a cylindlical coodinate, the Problem of instability of the Perturbation in tyPhoons is discussed.

在与实际台风风场近似一致的环境流场条件下，应用柱坐标中的正压无辐散模式，讨论了台风中扰动的稳定性问题。

Dr. Wu Chun-chieh is the professor of atmospheric science in National Taiwan University. Dr Wu grew up in the southeast coast of Taiwan, where the majority of direct typhoon landfalls occur. The violence of the storms is etched indelibly in his memory. For the past 15 years he has been unlocking their secrets.

吴俊杰博士是台湾大学大气科学系的教授，他生长在台风登陆最频繁的台湾东南沿岸，狂风暴雨在他心中留下深刻的记忆，十五年来他一直为了解开台风背后的秘密而努力。

As for the mid-June 2006 Mei-yu case, the assimilation of both kinds of data can help the simulation of radar reflectivity. Further investigations show that the assimilation of dropsonde and QuikSCAT data produces stronger southerly environmental winds in the Bilis case, resulting in a better simulated track than the runs without these data. In these runs, the simulated tracks are too far to the south compared with the observed. In the Kaemi case, the tracks of simulations without dropsonde/QuikSCAT data assimilation were shifted to the north/south of the observed track, respectively.

从影响实验研究发现，同化投落送及QuikSCAT资料后，碧利斯台风个案於模拟后期具有较强的南风分量，使其模拟路径不至於像未同化该两种资料者过於偏南；凯米台风个案同化投落送资料后於模拟后期具有较弱的南风分量，而同化QuikSCAT资料后则具有较强的南风分量，使其模拟路径不至於像未同化投落送及QuikSCAT资料者过於偏北及偏南，而与观测路径较为接近。

For a big chunk of credit-card losses; the number of filings (and thus charge-off rates) would be rising again, whether

年美国个人破产法的一个改动使得破产登记急速下降，而后引起了信用卡大规模的亏损。

Eph. 4:23 And that you be renewed in the spirit of your mind

弗四23 而在你们心思的灵里得以更新