C. Yang1,2 and J. Xu31CAMS & China Re CRM · Joint Open Lab on Meteorological Risk and Insurance, Beijing, China.2Faculty of Geographical Science, Beijing Normal University, Beijing, China.3Qingdao Joint Institute of Marine Meteorology, Chinese Academy of Meteorological Sciences, Beijing, China.Corresponding author: C. Yang ([email protected]), J. Xu ([email protected])Key Points:A modified Rankine vortex model with four free parameters is adopted to reconstruct wind fields along the tropical cyclone tracksA Bayesian hierarchical model with a latent neural network is developed to estimate the parameters based on the best-track data setBayesian model averaging is used to predict wind field parameters for synthetic tropical cyclones over the western North Pacific basinAbstractTropical cyclones (TCs) are one of the biggest threats to life and property around the world. Accurate estimation of TC wind hazard requires estimation of catastrophic TCs having a very long return period spanning up to thousands of years. Since reliable TC data are available only for recently decades, stochastic modeling and simulation turned out to be an effective approach to achieve more stable hazard estimates. In common practice, hundreds of thousands of synthetic TCs are generated first, then wind fields are reconstructed along synthetic TC tracks for hazard estimation. A Bayesian hierarchical modeling approach to the reconstruction of TC wind field is proposed. A modified Rankine vortex is adopted as the wind field model, of which the four free parameters are modeled simultaneously through a multi-output neural network as a latent process of the wind field. The four parameters are finally represented, spatially and temporally, by a set of neural network weights, The Bayesian model averaging technique is used for parameter estimation and wind field reconstruction, based on a ensemble of maximum a posteriori estimates of the set of weights. Together with previously proposed algorithm for synthetic TC simulation, a two-stage scheme for TC wind hazard estimation has been formed, which is based on best-track data only and thus is highly consistent. Application of this scheme to the offshore waters in the western North Pacific basin shows inspiring performance and great flexibility for various purposes of TC wind hazard estimation.

Chi Yang

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