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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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 |
work_keys_str_mv |
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