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The missing TC parameters in the best track datasets were reconstructed with local regression models.
In this study, all parameters in the best track datasets were linearly interpolated to 10 min (Li et al. 2014).
The values of P c and V m, especially of R m, are not available in some TCs of the best track datasets.
Open image in new window Fig. 1 Global tropical cyclone tracks by ocean basin based on historical TC best track datasets.
Usually, the key parameters can be obtained from historical TC track datasets, and great efforts have been made to compile the best tracks around the globe (Knapp et al. 2010).
Based on the existing records in the best track datasets, the fitted relations between (V_{m}) and P c and their coefficients for the seven basins are established (Table 3).
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In this study, the TC best track dataset of seven ocean basins are used.
The present study used the TC best track dataset archived by the Regional Specialized Meteorological Center (RSMC)—Tokyo (http://www.jma.go.jp/en/typh/).jp/en/typh/
Fig. 4 As in Fig. 1, but for the annual variation in the central pressure averaged for the maximal approach to the boundary line of the K-TC area using the 6-h TC best track dataset.
Thus, the CPA was also applied to the interannual variation in the average central pressure in the maximal approach to the boundary line of the K-TC area using the 6-h TC best track dataset (Fig. 4).
The gradient wind can be simulated with observed TC parameters, such as location, intensity, size, moving direction, and speed, which are usually available or can be derived from the TC track dataset.
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