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Exploring the use of transformation group priors and the method of maximum relative entropy for Bayesian glaciological inversions

机译:探索转换组先验的使用和贝叶斯冰川学反演的最大相对熵方法

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摘要

Ice-sheet models can be used to forecast ice losses from Antarctica and Greenland, but to fully quantify the risks associated with sea-level rise, probabilistic forecasts are needed. These require estimates of the probability density function (PDF) for various model parameters (e.g. the basal drag coefficient and ice viscosity). To infer such parameters from satellite observations it is common to use inverse methods. Two related approaches are in use: (1) minimization of a cost function that describes the misfit to the observations, often accompanied by explicit or implicit regularization, or (2) use of Bayes’ theorem to update prior assumptions about the probability of parameters. Both approaches have much in common and questions of regularization often map onto implicit choices of prior probabilities that are made explicit in the Bayesian framework. In both approaches questions can arise that seem to demand subjective input. One way to specify prior PDFs more objectively is by deriving transformation group priors that are invariant to symmetries of the problem, and then maximizing relative entropy, subject to any additional constraints. Here we investigate the application of these methods to the derivation of priors for a Bayesian approach to an idealized glaciological inverse problem.
机译:冰盖模型可用于预测南极洲和格陵兰岛的冰损失,但要完全量化与海平面上升相关的风险,则需要概率预测。这些要求估算各种模型参数(例如基础阻力系数和冰粘度)的概率密度函数(PDF)。为了从卫星观测中推断出此类参数,通常使用反演方法。正在使用两种相关方法:(1)最小化描述与观测值不匹配的成本函数,通常伴随显式或隐式正则化;或(2)使用贝叶斯定理更新有关参数概率的先前假设。两种方法都有很多共同点,正则化问题经常映射到贝叶斯框架中明确提出的先验概率的隐式选择。在这两种方法中,都会出现似乎需要主观投入的问题。一种更客观地指定先验PDF的方法是,通过推导对问题的对称性不变的变换组先验,然后在任何其他约束条件下最大化相对熵。在这里,我们研究了这些方法在贝叶斯方法对理想化冰川逆问题的先验推导中的应用。

著录项

  • 作者

    Arthern Robert J.;

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  • 年度 2015
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  • 原文格式 PDF
  • 正文语种 en
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