Multivariate stochastic bias corrections with optimal transport

<p>Bias correction methods are used to calibrate climate model outputs with respect to observational records. The goal is to ensure that statistical features (such as means and variances) of climate simulations are coherent with observations. In this article, a multivariate stochastic bias cor...

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Main Authors: Y. Robin, M. Vrac, P. Naveau, P. Yiou
Format: Article
Language:English
Published: Copernicus Publications 2019-02-01
Series:Hydrology and Earth System Sciences
Online Access:https://www.hydrol-earth-syst-sci.net/23/773/2019/hess-23-773-2019.pdf
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spelling doaj-9b0aaf9a221d4ea282016b64fa63cad02020-11-24T23:56:45ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382019-02-012377378610.5194/hess-23-773-2019Multivariate stochastic bias corrections with optimal transportY. Robin0M. Vrac1P. Naveau2P. Yiou3Laboratoire des Sciences du Climat et de l'Environnement, UMR 8212, CEA-CNRS-UVSQ, IPSL & U Paris-Saclay, Gif-sur-Yvette, FranceLaboratoire des Sciences du Climat et de l'Environnement, UMR 8212, CEA-CNRS-UVSQ, IPSL & U Paris-Saclay, Gif-sur-Yvette, FranceLaboratoire des Sciences du Climat et de l'Environnement, UMR 8212, CEA-CNRS-UVSQ, IPSL & U Paris-Saclay, Gif-sur-Yvette, FranceLaboratoire des Sciences du Climat et de l'Environnement, UMR 8212, CEA-CNRS-UVSQ, IPSL & U Paris-Saclay, Gif-sur-Yvette, France<p>Bias correction methods are used to calibrate climate model outputs with respect to observational records. The goal is to ensure that statistical features (such as means and variances) of climate simulations are coherent with observations. In this article, a multivariate stochastic bias correction method is developed based on optimal transport. Bias correction methods are usually defined as transfer functions between random variables. We show that such transfer functions induce a joint probability distribution between the biased random variable and its correction. The optimal transport theory allows us to construct a joint distribution that minimizes an energy spent in bias correction. This extends the classical univariate quantile mapping techniques in the multivariate case. We also propose a definition of non-stationary bias correction as a transfer of the model to the observational world, and we extend our method in this context. Those methodologies are first tested on an idealized chaotic system with three variables. In those controlled experiments, the correlations between variables appear almost perfectly corrected by our method, as opposed to a univariate correction. Our methodology is also tested on daily precipitation and temperatures over 12 locations in southern France. The correction of the inter-variable and inter-site structures of temperatures and precipitation appears in agreement with the multi-dimensional evolution of the model, hence satisfying our suggested definition of non-stationarity.</p>https://www.hydrol-earth-syst-sci.net/23/773/2019/hess-23-773-2019.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Y. Robin
M. Vrac
P. Naveau
P. Yiou
spellingShingle Y. Robin
M. Vrac
P. Naveau
P. Yiou
Multivariate stochastic bias corrections with optimal transport
Hydrology and Earth System Sciences
author_facet Y. Robin
M. Vrac
P. Naveau
P. Yiou
author_sort Y. Robin
title Multivariate stochastic bias corrections with optimal transport
title_short Multivariate stochastic bias corrections with optimal transport
title_full Multivariate stochastic bias corrections with optimal transport
title_fullStr Multivariate stochastic bias corrections with optimal transport
title_full_unstemmed Multivariate stochastic bias corrections with optimal transport
title_sort multivariate stochastic bias corrections with optimal transport
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2019-02-01
description <p>Bias correction methods are used to calibrate climate model outputs with respect to observational records. The goal is to ensure that statistical features (such as means and variances) of climate simulations are coherent with observations. In this article, a multivariate stochastic bias correction method is developed based on optimal transport. Bias correction methods are usually defined as transfer functions between random variables. We show that such transfer functions induce a joint probability distribution between the biased random variable and its correction. The optimal transport theory allows us to construct a joint distribution that minimizes an energy spent in bias correction. This extends the classical univariate quantile mapping techniques in the multivariate case. We also propose a definition of non-stationary bias correction as a transfer of the model to the observational world, and we extend our method in this context. Those methodologies are first tested on an idealized chaotic system with three variables. In those controlled experiments, the correlations between variables appear almost perfectly corrected by our method, as opposed to a univariate correction. Our methodology is also tested on daily precipitation and temperatures over 12 locations in southern France. The correction of the inter-variable and inter-site structures of temperatures and precipitation appears in agreement with the multi-dimensional evolution of the model, hence satisfying our suggested definition of non-stationarity.</p>
url https://www.hydrol-earth-syst-sci.net/23/773/2019/hess-23-773-2019.pdf
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