2019
DOI: 10.1016/j.amc.2019.01.071
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An efficient SPDE approach for El Niño

Abstract: We consider the numerical approximation of stochastic partial differential equations (SPDEs) based models for a quasi-periodic climate pattern in the tropical Pacific Ocean known as El Niño phenomenon. We show that for these models the mean and the covariance are given by a deterministic partial differential equation and by an operator differential equation, respectively. In this context we provide a numerical framework to approximate these parameters directly. We compare this method to stochastic differential… Show more

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Cited by 6 publications
(5 citation statements)
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“…For analysing asymptotic properties of this estimator, it is crucial to investigate the correlation structure of quadratic temporal increments and the product of consecutive temporal increments, as evident by (21).…”
Section: Andmentioning
confidence: 99%
See 1 more Smart Citation
“…For analysing asymptotic properties of this estimator, it is crucial to investigate the correlation structure of quadratic temporal increments and the product of consecutive temporal increments, as evident by (21).…”
Section: Andmentioning
confidence: 99%
“…Therefore, it is intuitive that applications of these SPDEs is also of great relevance, especially for two-and three-dimensional spaces. See, for instance, [21] for an application in connection with the climate phenomenon El Niño and references therein for applications to sea temperature, [23] for an application in Geostatistics and dealing with seismic data and [10] for an application in climate science. For an overview with many references to specific applications in various fields we refer to [19].…”
Section: Introductionmentioning
confidence: 99%
“…; see, e.g. [20,75], for applications. When matrices are large, it is important to exploit that applying the right hand side in (9.63) does not increase the rank of X(t) too much, which is guaranteed here, if J is not too large and the matrix C is of low rank.…”
Section: Matrix Equationsmentioning
confidence: 99%
“…This is characterized by an unusual warming of the sea surface temperature in the Indo-Pacific ocean. It can be modeled by https://www.nvidia.com/en-us/data-center/tesla-p100/ a stochastic advection equation driven by additive noise [38] and its covariance is given by a DLE of the form Ṗ (t) = AP (t) + P (t)A T + Q, see [34,35] for details. The matrix A arises from a centered finite difference approximation of the advection operator and Q is the discretized covariance operator of the random noise.…”
Section: Example 1: Heat Equation Random Modelmentioning
confidence: 99%