| 1. | Center locating of non - eye typhoon based on satellite cloud image
基于卫星云图的无眼台风中心定位算法 |
| 2. | Typhoon threatening zone
台风中心区 |
| 3. | The eye wall is the inner most ring of convection near the centre of a typhoon , containing most intense winds and fiercest rain
眼壁是最接近台风中心的环型对流雨带，该区的风力最强，雨势最大。 |
| 4. | The eye wall is the inner most ring of convection near the centre of a typhoon , containing most intense winds and fiercest rain
眼壁是最接近台风中心的环型对流雨带，该区的风力最强，雨势最大。 |
| 5. | The in of nonlinear advection into the model weakens the intensity of both inward and outward propagation of vorticity , but makes the inward propagation up to a posi
非线性平流的引进，使涡量向内区传输以及向外传输的强度均减弱：但内传的涡量更加接近于台风中心。 |
| 6. | The satellite image on the top shows a typhoon with a distinct eye at the centre over the northern hemisphere . the image below shows another over the southern hemisphere
上方的卫星图像显示有一台风中心的风眼清晰可见在北半球，而下方的图像显示另一台风在南半球。 |
| 7. | The strong winds associated with a typhoon will also drag and pile water up towards the coast . a storm surge is the anomalous rise in sea water brought about by the combined effects of pressure and wind stress
台风中心的气压比外围低，令海面承受较低的大气压力，导致海面升高，而其强大风力会把海水往岸边推高，气压和风力共同作用下造成风暴潮。 |
| 8. | The strong winds associated with a typhoon will also drag and pile water up towards the coast . a storm surge is the anomalous rise in sea water brought about by the combined effects of pressure and wind stress
台风中心的气压比外围低，令海面承受较低的大气压力，导致海面升高，而其强大风力会把海水往岸边推高，气压和风力共同作用下造成风暴潮。 |
| 9. | The azimuthally linear advection may results in that the meso - scale vortex of initially circular shape becomes the elongated and spiral vorticity bands ; the radial linear advection may transfer the vorticity of the outer region towards the center of the typhoon
沿e方向的线性平流可使初始圆形的中尺度涡旋演变为狭长的螺旋状的涡量带;沿径向线性平流的引进可使外区涡量向台风中心方向传播。 |
| 10. | The traditional solution to the problem is to plot the forecast position of typhoon center and the ship ' s position on the < < typhoon position diagram > > , to pay much attention to the relative position between the ship and typhoon , and the tendency of their movements , to consider the affects of all kinds of factors and leave enough room , to use the plotting method of geometric relative motion to figure out the course which the ship should take to keep away from typhoon on the small scale chart
传统的解决办法是，将台风中心的预报位置和本船的船位点绘在《台风位置标示图》上，研究本船与台风的相对位置以及相互间动态的发展态势，考虑各种因素的影响并留有充分余地，在小比例尺海图上用几何相对运动标绘的方法作图绘算出本船应采取的避台航向。 |
