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Michel Rixen

Researcher at World Climate Research Programme

Publications -  112
Citations -  4780

Michel Rixen is an academic researcher from World Climate Research Programme. The author has contributed to research in topics: Mediterranean sea & Data assimilation. The author has an hindex of 31, co-authored 110 publications receiving 3867 citations. Previous affiliations of Michel Rixen include Centre for Maritime Research and Experimentation & University of Liège.

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The Subseasonal to Seasonal (S2S) Prediction Project Database

TL;DR: The Subseasonal to Seasonal (S2S) Prediction research project has been established by the World Weather Research Programme/World Climate Research Programme as discussed by the authors, which is the main deliverable of this project is the establishment of an extensive database containing sub-seasonal (up to 60 days) forecasts, 3 weeks behind real time, and reforecasts from 11 operational centers, modeled in part on the The Observing System Research and Predictability Experiment (THORPEX) Interactive Grand Global Ensemble (TIGGE) database for medium-range forecasts.
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EOF Calculations and Data Filling from Incomplete Oceanographic Datasets

TL;DR: In this article, a self-consistent method is proposed to infer missing data from oceanographic data series and to extract the relevant empirical orthogonal functions, which allows for the detection of statistically significant EOFs by a cross-validation procedure for a complete or incomplete dataset, as well as the noise level and interpolation error.
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Reconstruction of incomplete oceanographic data sets using empirical orthogonal functions: application to the Adriatic Sea surface temperature

TL;DR: A method for the reconstruction of missing data based on an EOF decomposition has been applied to a large data set, a test case of Sea Surface Temperature satellite images of the Adriatic Sea as mentioned in this paper.
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The Western Mediterranean Deep Water: A proxy for climate change

TL;DR: This paper showed a proxy relationship between heat content changes in the North Atlantic and the Western Mediterranean Deep Water (WMDW) formed in the Gulf of Lions in winter, because of consistent air-sea heat fluxes over these areas.