“…The main methods for traditional TC forecast contain statistical methods and dynamic methods, most of which are along with complicated processes or lower precision. The statistical methods use the historical TCs' positions, intensity, and so on to predict TC's characteristic factors, such as fuzzy multicriteria decision support model [2], conditional nonlinear optimal perturbation, first singular vector, ensemble transform Kalman filter [3], back propagation-neural network [4], adaptive neural network classifier using a two-layer feature selector [5], and a support vector machine using data reduction methods [6]. Dynamic methods are mainly based on numerical forecast, such as a simplified dynamical system based on a logistic growth equation (LGE) [7], a regional coupled atmosphere-ocean model [8], the PSU-NCAR Mesoscale Model version 5 [9], and the GFDL 25-km-Resolution Global Atmospheric Model [10].…”