MLLGMEDec 20, 2024

Deep learning joint extremes of metocean variables using the SPAR model

arXiv:2412.15808v32 citationsh-index: 4Volume 3: Ocean Engineering; Polar and Arctic Sciences and Technology
Originality Incremental advance
AI Analysis

This addresses the challenge of modeling extreme environmental events for applications in fields like climate science and engineering, representing an incremental improvement over existing methods.

The paper tackles the problem of estimating multivariate joint extremes of metocean variables by developing a deep learning framework based on the SPAR model, showing that the fitted models provide a good description of joint extremes for five variables like wind speed and wave height.

This paper presents a novel deep learning framework for estimating multivariate joint extremes of metocean variables, based on the Semi-Parametric Angular-Radial (SPAR) model. When considered in polar coordinates, the problem of modelling multivariate extremes is transformed to one of modelling an angular density, and the tail of a univariate radial variable conditioned on angle. In the SPAR approach, the tail of the radial variable is modelled using a generalised Pareto (GP) distribution, providing a natural extension of univariate extreme value theory to the multivariate setting. In this work, we show how the method can be applied in higher dimensions, using a case study for five metocean variables: wind speed, wind direction, wave height, wave period, and wave direction. The angular variable is modelled using a kernel density method, while the parameters of the GP model are approximated using fully-connected deep neural networks. Our approach provides great flexibility in the dependence structures that can be represented, together with computationally efficient routines for training the model. Furthermore, the application of the method requires fewer assumptions about the underlying distribution(s) compared to existing approaches, and an asymptotically justified means for extrapolating outside the range of observations. Using various diagnostic plots, we show that the fitted models provide a good description of the joint extremes of the metocean variables considered.

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