查询词典 cyclone center
- 与 cyclone center 相关的网络例句 [注:此内容来源于网络,仅供参考]
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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。
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Using the seale separation method, the meso-scale structure of Mcc occ- ured near the Delta Area of the Pearl River is studied. It is shown that there is a meso-scale cyclonic circulation at 1000 hpa level and a meso-scale anticyclon at 200 hpa level associated with the Mcc. The axis of the Meso-scale cyclone center tilts northwestward with height, stretching up to 400 hpa level.
用滤波方法分析了一例发生在珠江口附近地区的Mcc的中尺度结构,结果表明,在对流层下部有中尺度的气旋性涡旋与Mcc相应,涡旋的中心轴线随高度向西北方向倾斜,在地面涡旋的上方200hPa层上,是一中尺度的反气旋性涡旋,中尺度的辐合中心和上升运动中心偏于Mcc的西部,扰动温度场也是非对称的,在对流层上部没有中尺度的暖高压。
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There are only fine water vapor conditions at fore warm front and cyclone center.
只有暖锋前的冷层和气旋中心水汽较多。
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So the two methods have been chosen to detect and estimate the center of a tropical cyclone over China offshore.They are the Geometric Axisymmetric Center Positioning Method and the Velocity Distance Azimuth Display Positioning Method,respectively.The former decides the position of a tropical cyclone center using directly the Doppler radar radial velocity field,the latter does the position using the productV_(r×D of the Doppler radar radial velocity valueV_(r and the distance from observation site to radar center.
两种客观方法分别为几何轴对称中心定位法和速度距离方位显示中心定位法,前者直接应用多普勒径向速度场进行定位估计,后者则应用观测的多普勒径向速度场与观测点至雷达中心距离的乘积来估计台风中心位置。
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The change in the tropical cyclone intensity as it passes the area near to Shanghai is remarkable. In general, the minimum surface level pressure of tropical cyclone center near to Shanghai is greater than 920 hPa.
上海及其近海区域台风强度随纬度增加而减弱的变化特徵明显,在东海北部,近50 a内尚未出现过中心气压低920 hPa的台风。
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When the temperature is below 0℃, in nascent period of cyclone, it is showed there are fine water vapor conditions anywhere in cyclone. In developing period of cyclone, there are fine water vapor conditions at the fore of cold and warm fronts. After cyclone occlude, there are only fine water vapor conditions at fore warm front and cyclone center.
分析表明,在气旋初生期,气旋各部位的冷层都有较好的水汽条件;在气旋发展旺盛时,冷锋前和暖锋前的冷层水汽条件较好;在气旋锢囚后,只有暖锋前的冷层和气旋中心水汽较多。
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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。
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On the basis of the distribution feature and the hypothesis about the radius of maximum wind within the circulation of a tropical cyclone,a lot of methods are designed to decide a tropical cyclone center with the pattern recognition technique.The aim of the applied study in operational tropical cyclone monitoring is to establish some objective positioning methods for the center of a tropical cyclone using a single Doppler radar radial velocity.
在假设台风环流存在最大风速半径的前提下,利用多普勒雷达径向速度场的这种分布特性和型态识别技术,进行近海台风的雷达定位客观方法的应用研究,并选取两种客观定位方法对台风中心位置进行估计。
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The Doppler radar radial velocity field near a tropical cyclone center,which has characteristic of approximately axisymmetric distribution or Rankine vortex,has a particular dipole pattern distribution feature.
对于近似轴对称与类似兰金涡旋特性的台风近中心环流而言,其多普勒雷达径向速度场具有相当特殊的偶极型态分布特征。
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Results show that the heavy rainfall event occurred under the favorable environmental conditions, resulted from the interaction of mid-and low-latitude systems. The mesoscale convergence and the mesoscale low triggered the occurrence of the heavy rainfall. Rain clusters bringing the heavy rainfall were related to meso-β systems. The meso-β mesoscale rain clusters appeared to the north of the cyclone center on 1000 hPa after filtering and to the south of the meso-α convergence line on 850 hPa.
分析表明:暴雨发生在高低空流场及中低纬系统配置非常有利的天气背景下,是多种尺度天气系统相互作用的结果;在对流性不稳定层结中,冷空气沿等熵面侵入到中尺度辐合系统中,激发了中尺度低涡的迅速发展,在孟加拉湾和南海源源不断输送的水汽配合下,导致了暴雨的发生;中β尺度对流雨团发生在滤波后1000 hPa 等压面的低涡中心北侧和850 hPa 中α尺度辐合线南侧,呈现暖式切变的降雨特征。
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