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typhoon depression
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  台风低压
     In this paper,climatic analysis on 3 case heavy rain around making land typhoon depression in the Loess Plateau since 1980's and dynamic diagnosis analysis about torrential rain around 9608 typhoon depression have been done.
     对80年代以来3次登陆台风低压外围影响黄土高原的大暴雨作了气候分析,对9608号台风进行了天气动力诊断分析。
短句来源
     The results show that the main mechanism of heavy rain formation is the influence of the esterly jet around typhoon depression,low-pressure system in westerly belt and the lifting of surface cold front.
     结果表明:登陆台风低压外围产生大暴雨的主要机制是台风外围低空偏东急流与西风带低值系统的共同作用以及地面冷锋的动力抬升作用。
短句来源
     Contrastive analysis on the two processes of the rainstorm impacted by typhoon depression in the southwest of Shandong province in 2004
     2004年鲁西南两次台风低压暴雨过程对比分析
短句来源
     We analyze the two rainstorm ~ heavy rainstorm process impacted by the typhoon from the southwest of Shandong province in 2004,the results show that the precipitation under the function of typhoon depression and westerly trough will intensify ulteriorly.
     对2004年鲁西南两次台风影响造成的大~暴雨过程分析结果表明,西风槽作用下的降水,若有台风低压参与,系统均得以发展,雨势进一步加强。
短句来源
     The vapor for the cold-front heavy rainfall was transported by the easterly jet around the typhoon depression. The vapor transportation was mostly found at the 850 hPa level.
     冷锋暴雨的水汽输送主要依靠台风低压外围的偏东急流来传递,水汽输送以850 hPa层附近最为显著。
短句来源
更多       
  台风
     In this paper,climatic analysis on 3 case heavy rain around making land typhoon depression in the Loess Plateau since 1980's and dynamic diagnosis analysis about torrential rain around 9608 typhoon depression have been done.
     对80年代以来3次登陆台风低压外围影响黄土高原的大暴雨作了气候分析,对9608号台风进行了天气动力诊断分析。
短句来源
     The results show that the main mechanism of heavy rain formation is the influence of the esterly jet around typhoon depression,low-pressure system in westerly belt and the lifting of surface cold front.
     结果表明:登陆台风低压外围产生大暴雨的主要机制是台风外围低空偏东急流与西风带低值系统的共同作用以及地面冷锋的动力抬升作用。
短句来源
     Contrastive analysis on the two processes of the rainstorm impacted by typhoon depression in the southwest of Shandong province in 2004
     2004年鲁西南两次台风低压暴雨过程对比分析
短句来源
     The importance of nonlinear action effect in the process of generation and development of typhoon depression on its special structure formation has been confirmed.
     部分地揭示了台风发生发展过程中的非线性作用对形成台风特殊结构影响的重要性。
短句来源
     THE EFFECT OF NONLINEAR ACTION IN THE PROCESS OF GENERATION AND DEVELOPMENT OF TYPHOON DEPRESSION ON ITS STRUCTURE FORMATION
     台风发生发展过程中的非线性作用对台风结构形成的影响
短句来源
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  “typhoon depression”译为未确定词的双语例句
     SELF-EXCITING HEATING DISSIPATION AND NONLINEAR ACTION IN THE PROCESS OF GENERATION AND DEVELOPMENT OF TYPHOON DEPRESSION
     热带低压、台风发生发展过程中的自激加热、耗散和非线性作用
短句来源
     THE EFFECT OF MAKING LAND TYPHOON DEPRESSION ON HEAVY RAIN IN EASTERN PART OF LOESS PLATEAU
     登陆台风对黄土高原东部暴雨的影响
短句来源
     A highly truncated spectral model is used to study the self-exciting heating, dissipation and nonlinear action in the typhoon depression system.
     本文用非线性耗散理论研究第二类条件不稳定下的自激加热的热带低压、台风系统。
短句来源
     It is pointed out that the process of typhoon depression generation and development is the process in which steady-state equilbrium of the model envolves from gradual change to sudden change and from sudden change to gradual change in the phase space.
     热带低压、台风的发生发展和消亡过程就是系统平衡态在相空间里由渐变到突变,由突变到渐变的往复循环过程。
短句来源
     typhoon depression moved northwest,came into Shandong province from Yellow Sea on August 9 night,11-12 with westerlies system interaction,and caused a heavy rain or very heavy rain in part area of Shandong.
     990 7号热带风暴西北上减弱成低气压之后 ,从黄海进入山东 ,分别于 8月 9日夜间、1 1~ 1 2日与西风带系统相互作用 ,造成了山东部分地、市出现大暴雨或特大暴雨。
短句来源
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In this paper, the shearing basic flow is introduced into the CISK theory developed by Charney and Eliassen (1964). Then, the growth rate of typhoon depression is investigated with a simple numerical model under the effect of cyclonic shearing basic flow in lower troposphere and the effect of shearing basic flow in upper troposphere.The cyclonic shearing basic flow in lower troposphere increases the growth rate. It is explained with dynamic point of view that the enhancement of equatorial westerly or southwest...

In this paper, the shearing basic flow is introduced into the CISK theory developed by Charney and Eliassen (1964). Then, the growth rate of typhoon depression is investigated with a simple numerical model under the effect of cyclonic shearing basic flow in lower troposphere and the effect of shearing basic flow in upper troposphere.The cyclonic shearing basic flow in lower troposphere increases the growth rate. It is explained with dynamic point of view that the enhancement of equatorial westerly or southwest monsoon and the influnce of cold front with moderate strength are conducive to generation and development of Typhoon.The effect of anticyclonic shearing basic flow in upper troposphere is condu-cible for development of Typhoon. But, the cyclonic shearing basic flow in upper troposphere will depress Typhoon. The effects of ambient flow in upper troposphere are weak on development of Typhoon.

本文用简单的数学模式、基于CISK理论,从动力学角度分别讨论了在对流层低层气旋性切变基本气流作用下以及对流层上层切变基本气流作用下,台风低压增长率的改变。结果表明,对流层低层的气旋性切变基本气流可以使增长率明显增大,这从动力学角度解释了赤道西风或西南季风的加强以及适中强度的冷空气影响有利于台风生成和发展的天气事实。对流层上层反气旋性切变基本气流有利于台风发展,而对流层上层气旋性切变基本气流使台风削弱。但对流层上层环境流场的影响相对比较微弱。

By using a 2-dimensional axial symmetrical PEM, in which the Ekmau pumping and the cumulus momentum transport are included, the influences of the condensational heating profile on the development of the typhoon depression have been investigated in this paper. The results of numerical simulation show that ths circulation of the modeling typhoon develops faster in the lower troposphere if there is stronger heating in the middle-lower troposphere; the structure of the modling typhoon is more similar...

By using a 2-dimensional axial symmetrical PEM, in which the Ekmau pumping and the cumulus momentum transport are included, the influences of the condensational heating profile on the development of the typhoon depression have been investigated in this paper. The results of numerical simulation show that ths circulation of the modeling typhoon develops faster in the lower troposphere if there is stronger heating in the middle-lower troposphere; the structure of the modling typhoon is more similar to real typhoon when the stronger heating is in upper troposphere.

本文用一个同时考虑Ekman抽吸和积云动量输送作用的二维轴对称原始方程模式,就对流凝结加热廓线对台风低压发展的影响进行了数值模拟研究。试验结果表明,对流层中下部有较强加热时,模式台风低压的低压环流发展较快;对流层上部有较强加热时,系统结构更类似于实际台风。 在台风低压发展过程中,对流凝结加热廓线也会改变,最强加热可能由对流层中下部向中上层发展和传播,从而,台风低压发展既快、系统结构又类似于实际台风。这样一种过程可能正是热带低压发展为台风的一般过程。

A highly truncated spectral model is used to study the self-exciting heating, dissipation and nonlinear action in the typhoon depression system. In the certain intensely heating condition of cumulus convection, the model exist three equilibrium states. A stability investigation of the equilibrium state triplets shows that two are stable while one is unstable. It is pointed out that the process of typhoon depression generation and development is the process in which steady-state equilbrium of the...

A highly truncated spectral model is used to study the self-exciting heating, dissipation and nonlinear action in the typhoon depression system. In the certain intensely heating condition of cumulus convection, the model exist three equilibrium states. A stability investigation of the equilibrium state triplets shows that two are stable while one is unstable. It is pointed out that the process of typhoon depression generation and development is the process in which steady-state equilbrium of the model envolves from gradual change to sudden change and from sudden change to gradual change in the phase space.

本文用非线性耗散理论研究第二类条件不稳定下的自激加热的热带低压、台风系统。本文用高截断谱方法建立的非线性耗散系统,在一定的积云对流加热条件下,存在两个稳定的平衡态,分别表示热带低压、台风的平衡态及静态平衡态;另外还存在一个不稳平衡态。热带低压、台风的发生发展和消亡过程就是系统平衡态在相空间里由渐变到突变,由突变到渐变的往复循环过程。

 
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