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Modelling ocean wave climate with a Bayesian hierarchical space-time model and a log-transform of the data

机译:使用贝叶斯分层时空模型和数据的对数转换来模拟海浪气候

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摘要

Long-term trends in the ocean wave climate because of global warming are of major concern to many stakeholders within the maritime industries, and there is a need to take severe sea state conditions into account in design of marine structures and in marine operations. Various stochastic models of significant wave height are reported in the literature, but most are based on point measurements without exploiting the flexible framework of Bayesian hierarchical space-time models. This framework allows modelling of complex dependence structures in space and time and incorporation of physical features and prior knowledge, yet remains intuitive and easily interpreted. This paper presents a Bayesian hierarchical space-time model with a log-transform for significant wave height data for an area in the North Atlantic ocean. The different components of the model will be outlined, and the results from applying the model to data of different temporal resolutions will be discussed. Different model alternatives have been tried and long-term trends in the data have been identified for all model alternatives. Overall, these trends are in reasonable agreement and also agree fairly well with previous studies. The log-transform was included in order to account for observed heteroscedas-ticity in the data, and results are compared to previous results where a similar model was employed without a log-transform. Furthermore, a discussion of possible extensions to the model, e.g. incorporating regression terms with relevant meteorological data, will be presented.
机译:由于全球变暖,海浪气候的长期趋势是海事行业中许多利益相关者所关注的主要问题,在海洋结构的设计和海洋作业中需要考虑到严峻的海况条件。文献中报道了各种重要波高的随机模型,但是大多数是基于点测量的,没有利用贝叶斯分层时空模型的灵活框架。该框架允许对时空复杂的依存结构进行建模,并结合物理特征和先验知识,但仍保持直观且易于解释。本文针对北大西洋某个区域的重要波高数据,提出了一种具有对数变换的贝叶斯分层时空模型。将概述模型的不同组件,并讨论将模型应用于不同时间分辨率的数据的结果。已经尝试了不同的模型替代方案,并且为所有模型替代方案确定了数据的长期趋势。总体而言,这些趋势在合理的范围内,并且也与先前的研究非常吻合。包括对数转换是为了说明数据中观察到的异方差性,并将结果与​​以前的结果进行比较,在以前的结果中采用了类似的模型而没有对数转换。此外,讨论了模型的可能扩展,例如将介绍将回归项与相关气象数据结合起来的方法。

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