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Typhoon eye trajectory based on a mathematical model: comparing with observational data

机译:基于数学模型的台风眼轨迹:与   观测数据

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We propose a model based on the primitive system of the Navier-Stokesequations in a bidimensional framework as the $l$ - plane approximation, whichallows us to explain the variety of tracks of tropical cyclones (typhoons). Ouridea is to construct special analytical solutions with a linear velocityprofile for the Navier-Stokes systems. The evidence of the structure of linearvelocity near the center of vortex can be proven by the observational data. Westudy solutions with the linear-velocity property for both barotropic andbaroclinic cases and show that they follow the same equations in describing thetrajectories of the typhoon eye at the equilibrium state (that relates to theconservative phase of the typhoon dynamics). Moreover, at the equilibriumstate, the trajectories can be viewed as a superposition of two circularmotions: one has period $2\pi/l,$ the other one has period $2\pi/b_0,$ where$l$ is the Coriolis parameter and $b_0$ is the height-averaged vorticity at thecenter of cyclone. Also, we compare our theoretical trajectories based on initial conditionsfrom the flow with tracks obtained from the observational database. It is worthto mention that under certain conditions our results are still compatible withobservational data although we did not truly consider the influence of steeringeffect. %Note that the %motion of the typhoon eye can not be totallydeterminated by initial %conditions due to the effect of ambient pressure field("steering" %effect). Finally, we propose the parameter-adopting method so thatone could correct the weather prediction in real time. Examples of our analysisand the use of parameter-adopting method for the historic trajectories areprovided.
机译:我们以二维框架中的Navier-Stokesequations原始系统为基础,提出了一个模型,即$ l $-平面近似,这使我们能够解释热带气旋(台风)的变化。 Ouridea将为Navier-Stokes系统构建具有线性速度分布的特殊分析解决方案。涡旋中心附近的线速度结构的证据可以通过观测数据来证明。对正压和斜压两种情况都具有线速度性质的Westudy解,表明它们在描述台风眼处于平衡状态时的轨迹时遵循相同的方程(与台风动力学的保守阶段有关)。而且,在平衡状态下,轨迹可以看作是两个圆周运动的叠加:一个周期为$ 2 \ pi / l,$另一个周期为$ 2 \ pi / b_0,$,其中$ l $是科里奥利参数,$ b_0 $是旋风中心的平均涡度。此外,我们还将基于流动的初始条件的理论轨迹与从观测数据库获得的轨迹进行比较。值得一提的是,尽管我们并未真正考虑转向效果的影响,但在某些条件下我们的结果仍与观测数据兼容。 %请注意,由于环境压力场的影响(“转向”效果),台风眼的运动%不能完全由初始条件确定。最后,我们提出了采用参数的方法,以便可以实时校正天气预报。提供了我们的分析实例,并为历史轨迹提供了参数采用方法。

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