气旋的

基本解释 (translations)

cyclonic

与气旋的相关的网络例句 [注：此内容来源于网络，仅供参考]

Subject to the anticyclone anchored in central China, 21W will move along its southeastern periphery in a SW to WSW direction in the next 72 hours.

受到在中国大陆的一个反气旋影响，21W 将於未来 72 小时沿该反气旋的东南部向西南或西南偏西移动。

The SSTA of February and August in 1998 had two peaks, while the wind speed reached its maximum minus anomalies in January and August. In order to find the circulation anomaly in the South China Sea, the circulation of 19952000 had been calculated by the ECOM hydrodynamic numerical model. The elevation and circulation of January and August in 1998 indicated that there were great anomaly of elevation and circulation after this El Nio event.(1)In January, the whole South China Sea had positive sea level anomaly and anticyclonic velocity anomaly, so the cyclonic circulation was weaker than normal.(2) In August, the South China Sea had positive sea level anomaly, especially stronger in the east of Vietnam, and cyclonic velocity anomaly in south, anticyclonic velocity in north, especially strong in the east of Vietnam. So the cyclonic gyre in the north and the anticyclonic gyre in the south were both weaker than normal, and an anticyclonic gyre appeared in the east of Vietnam.

为研究南海环流在1997/1998年的异常变化，利用ECOM水动力模型计算了1995—2000年的南海环流场，分析了1998年1月和8月南海水位和环流的异常分布，二者均存在显著的异常：①1月，整个南海海盆为正的水位异常，流场为反气旋异常环流，冬季控制整个南海海盆的气旋式环流减弱；②8月，南海海盆水位为正异常，特别是越南东部海区出现较强的正水位异常，南海南部的高水位中心扩大北移；异常流场表现为南部为气旋式异常环流，北部为反气旋的异常环流，且在越南东部海区形成非常强的反气旋异常环流中心，使得控制南海南部的反气旋环流和北部的气旋环流均减弱。

Near the center, the pressure gradient force (from the pressure in the center of the cyclone compared to the pressure outside the cyclone) and the Coriolis force must be in an approximate balance, or the cyclone would collapse on itself as a result of the difference in pressure.

中心附近的气压梯度力（从压力中的中心气旋的压力相比，外气旋）和科氏力，必须在一个大致平衡，或气旋将会崩溃对本身所造成的差异在压力。

Dry, cold air is induced reaction of transformation.6vertical wind shearIS a important role 7 the interaction stage of tropical cyclone with a midlatitude baroclinic zone was an essentialcomponent.

垂直风切变相互作用是激发热带气旋的变性不可获缺的条件(7)热带风暴和中纬度斜压带相互作用是变性的必要条件：只有减弱的热带风暴嵌入先前存在的中纬度斜压带，才能完成正压向斜压的转变。正是热带气旋环流和斜压带和垂直风切变相互作用激发了热带气旋的变性。

Chen et al noted that there are three kinds of landfall typhoon tracks; subtropical high and polar front, whose evolutions and adjustments may modify typhoon movement, are the main synoptic systems which influence the track of landfall typhoon.

陈联寿等根据(1949-1976)年资料，指出：登陆台风路径可分为三类；副热带高压和极锋是影响热带气旋陆地路径的主要天气系统，它们的演变和调整会影响热带气旋的移向。

It is shown from this thesis that flow fields on synoptic maps can be decomposed into rotation and deformation fields. Geostrophic non-frictional cyclone and anticyclone vortex patterns are closed circulations around the center point, streamlines of frictional cyclone and anticyclone patterns have spiral forms around the focus point. Saddle fields have four vortex centers (two cyclones and two anticyclones) and a saddle point. Blocking high pressure and cut-off low pressure patterns consist of a vortex center and a saddle point.

本文说明了天气图上的流场可以分解为旋转场和变形场：地转无摩擦的气旋、反气旋的涡旋型式是围绕中心点的闭合环流；考虑摩擦的气旋、反气旋的流型是围绕焦点的螺旋型式；鞍型场有4个涡旋中心点（2个气旋和2个反气旋）与1个鞍点；阻塞高压和切断低压由1个涡旋中心点与1个鞍点组成。

One of factors which activize the explosive development of cyclone exists strong convective instability in lower layers from the analysis of the barotropic potential vorticity.

气旋发展后期气旋中心上空300hPa以上位于位涡平流零线附近。850hPa以下的斜压位涡的正负值的变化与气旋的发展有很好的对应关系。

The team interpreted those shifts as the effect of cyclonic winds moving above and below the black hole at speeds of about 4000 kilometers per second, tens of thousands of times stronger than the most intense cyclones on Earth.

研究小组认为这些变化是黑洞上方和下方速度达每秒4000公里的猛烈气旋运动造成的。这气旋的速度相当于地球上最猛烈飓风的数万倍。

The mositened air can be lifted to the 320-340K potential temperater levels firstly, and then transport toward North-West conved by largen scale advection.

对流抬升作用下，湿空气可向上输送到位温320-340K高度，然后在南亚反气旋大尺度平流作用下，在反气旋的西侧向北输送。

The force of low-level frontal zone disturbance is a major factor of the development of middle and low level cyclone. The large center of negative geopotential perturbation inversed by low-level disturbance potential vorticity is located in the front of cyclone providing a favourable condition for the eastward moving and development of cyclone. The high-level system plays a role of indirect force action. The interaction of the development of high-level trough and ridge and low-level frontal zone becomes an important mechanism of the developing of cyclone.

低层锋区扰动强迫是中低层气旋发展的最主要因子，低层位涡扰动反演所得的负位势扰动大值中心位于气旋的前方，有导前现象，为气旋继续东移、发展提供一个铺垫；高层系统起着间接强迫作用，高层槽脊系统的发展和低层锋区的相互作用所导致的斜压扰动成为气旋发展的重要机制。

与气旋的相关的网络解释 [注：此内容来源于网络，仅供参考]

anticyclone：反气旋

要成分度随高度而增加)为特征的反气旋(Anticyclone)的情况下,再加上下垫面2.似榆树(elmlike)是被叫着被子植物的开花植物中最大的一类.图为动.因此常常把反气旋表示为高压.反气旋通常与气旋(Cyclone)共存.反因为它有高含量的钾(K),

anticyclone：反气旋区域

anticyclolysis 反气旋消散 | anticyclone 反气旋区域 | anticyclonic 反气旋的

anticyclonic：反气旋的

Johnin [免疫]副结核菌素 | anticyclonic 反气旋的 | circular reflector 圆形反射器

cyclone：气旋

(斐济处于热带亚热带边的大洋上,类似台风那样的"气旋"(cyclone)常年不断,这些气旋多吹往纳迪那边的西部,而较少从苏瓦这边的东部经过. )

Dvorak：(德沃夏克)

德沃夏克分析法 气象卫星的发展让人们能透过卫星云图来评估热带气旋的强度,让人们及早对热带气旋作出适当的警告. 要对热带气旋的强度进行分析,德沃夏克(Dvorak)所发明的分析法便是现时国际通

external force：外力

直至热带气旋用尽了所有有利自己发展的条件时,热带气旋便停止进一步增强 .热带气旋的移动受著两大因素影响-内力(Internal force)和外力(External force).

internal force：内力

直至热带气旋用尽了所有有利自己发展的条件时,热带气旋便停止进一步增强 .热带气旋的移动受著两大因素影响-内力(Internal force)和外力(External force).

resultant force：合力

地面偏北风加上高空引导气流东风带或西风带得出的合力 (Resultant Force)就使热带气旋绕过大陆性反气旋的南部向西南偏西移动. 大陆性反气旋亦会使西风带南下,如果长波槽掠过,就会使热带气旋绕过反气旋东侧向东北移动.

cyclonic：气旋的

cyclone 飓风 | cyclonic 气旋的 | cyclonite 炸药

cyclonic：气旋的, 飓风的

cyclonic whirl | 旋风形涡流 | cyclonic | 气旋的, 飓风的 | cyclonite | 一种高性能的炸药