2010
DOI: 10.4310/cms.2010.v8.n2.a5
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The multidimensional maximum entropy moment problem: a review of numerical methods

Abstract: Abstract. Recently the author developed a numerical method for the multidimensional momentconstrained maximum entropy problem, which is practically capable of solving maximum entropy problems in the two-dimensional domain with moment constraints of order up to 8, in the threedimensional domain with moment constraints of order up to 6, and in the four-dimensional domain with moment constraints of order up to 4, corresponding to the total number of moment constraints of 44, 83 and 69, respectively. In this work,… Show more

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Cited by 45 publications
(39 citation statements)
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“…The compressed quadratic form in [24] is relevant in determining the important practical information regarding whether, for example, changes in the mean climate statistics alone determine the most sensitive directions of climate change. Obviously, the same formulas in [22,23] can be applied also to any AOS model by utilizing π M L in [22,24]. For such a climate model, one can calculate the unknown information ∇~λ~E L ð~uÞ through statistics of the present modeled climate from a suitable version of algorithms based on the fluctuationdissipation theorem (FDT) (see refs.…”
Section: -29 For a Discussion) Since π~λJ~λ ¼0 ¼ π For Small Valumentioning
confidence: 99%
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“…The compressed quadratic form in [24] is relevant in determining the important practical information regarding whether, for example, changes in the mean climate statistics alone determine the most sensitive directions of climate change. Obviously, the same formulas in [22,23] can be applied also to any AOS model by utilizing π M L in [22,24]. For such a climate model, one can calculate the unknown information ∇~λ~E L ð~uÞ through statistics of the present modeled climate from a suitable version of algorithms based on the fluctuationdissipation theorem (FDT) (see refs.…”
Section: -29 For a Discussion) Since π~λJ~λ ¼0 ¼ π For Small Valumentioning
confidence: 99%
“…For PC-1, the exact most sensitive direction using [19] is given by~e Ã π ¼ ð0.969;0.249Þ T so that the projection on changes in external forcing is roughly 80% and this is reproduced exactly by the full two moment estimator through the formula in Fact 3; this is not surprising because A ¼ B ¼ 0 in [25], see SI Text. The functional with model error which utilizes the mean and covariance but a Gaussian approximate climate has the predicted most sensitive direction,~e à G ¼ ð0.937;0.349Þ T which has an error of 6.0°in the angle with~e à π ; the model error functional using only the mean alone for climate sensitivity but the non-Gaussian climate as in [23] yields e à 1 ¼ ð0.989;0.150Þ T with an error of −5.8°in the angle with~e à π . While the stochastic model for PC-1 is most sensitive to changes in external forcing, in contrast the most sensitive perturbation direction for the NAO is~e Ã π ¼ ð−0.076;0.997Þ and is overwhelmingly dominated by changes in dissipation.…”
Section: The Most Sensitive Climate Change Directions In a Stochasticmentioning
confidence: 99%
“…It should be noted that some numerical work already exists; see, for example, [2,18] and references therein. While MATLAB provides an excellent interface for learning, the computational effort required for the dual problem limits experimentation.…”
Section: Conclusion and Discussionmentioning
confidence: 99%
“…Those functions consist of single (univariate) and combined (bivariate) monomials of the standard Gaussians X and Y. The numerical implementation of joint ME-PDFs constrained by polynomials in dimensions d = 2, 3 and 4 was studied by Abramov [17][18][19], with particular emphasis on the efficiency and convergence of iterative algorithms. Here, we use the algorithm proposed in [21] and explained in the Appendix 1.…”
Section: The Sequence Of Non-gaussian MI Lower Bounds From Cross-consmentioning
confidence: 99%
“…The properties of multivariate ME distributions have been studied for various ME constraints, namely: (a) imposed marginals and covariance matrix [15]; (b) generic joint moments [16]. Abramov [17][18][19] has developed efficient and stable numerical iterative algorithms for computing ME distributions forced by sets of polynomial expectations. Here we use a bivariate version of the algorithm of [20], already tested in [21].…”
Section: Introductionmentioning
confidence: 99%