Extended Data Fig. 1: Categorization of landfalling track modes.
![Extended Data Fig. 1](https://cdn.statically.io/img/media.springernature.com/full/springer-static/esm/art%3A10.1038%2Fs41586-022-04791-1/MediaObjects/41586_2022_4791_Fig3_ESM.jpg)
Following LC, at least four continuous inland data points should exist. The intensity of the landfalling hurricane at the first data point is ≥ 33 m s−1. The threshold of translation velocity at 10 km h−1 and the criterial angle between the landfalling track and coastline at 45° have been practically validated that can physically distinguish the characteristics among different landfalling track modes.