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hal-00951429v1  Journal articles
Bernard GarelJulien BoucharelBoris DewitteYves Du Penhoat. Non-stationary and non-Gaussian characters of ENSO: the role of climate shift.
Nonlinear Processes in Geophysics, European Geosciences Union (EGU), 2009, 16, pp.1-21
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hal-00760423v1  Conference papers
Christoph GarbeAndre ButzIsabelle DadouBoris DewitteVeronique Garcon et al.  Climatically-Active Gases In The Eastern Boundary Upwelling And Oxygen Minimum Zone (Omz) Systems
Geoscience and Remote Sensing Symposium (IGARSS), 2012 IEEE International, IEEE, Jul 2012, Munich, Germany. pp.6150 - 6153, ⟨10.1109/IGARSS.2012.6352740⟩
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hal-01078314v1  Conference papers
Ismael Hernandez-CarrascoJ SudreV. GarçonHussein YahiaBoris Dewitte et al.  Validation of inferred high resolution ocean pCO2 and air-sea fluxes with in-situ and remote sensing data
Earth Observation for Ocean-Atmosphere Interactions Science 2014, ESA-ESRIN, Oct 2014, Frascati, Italy
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hal-00951088v1  Journal articles
Sulian ThualBoris DewitteNadia AyoubOlivier Thual. An Asymptotic Expansion for the Recharge-Discharge Model of ENSO
Journal of Physical Oceanography, American Meteorological Society, 2013, 43, pp.1407-1416. ⟨10.1175/JPO-D-12-0161.1⟩
hal-02333501v1  Journal articles
Francisco TapiadorRémy RocaAnthony del GenioBoris DewitteWalt Petersen et al.  Is Precipitation a Good Metric for Model Performance?
Bulletin of the American Meteorological Society, American Meteorological Society, 2019, 100 (2), pp.223-233. ⟨10.1175/BAMS-D-17-0218.1⟩
hal-00280344v1  Journal articles
Serena IlligDaria GushchinaBoris DewitteNadia AyoubYves Du Penhoat. The 1996 Equatorial Atlantic warm event: origin and mechanisms
Geophysical Research Letters, American Geophysical Union, 2006, 33 (9), pp.L09701. ⟨10.1029/2005GL025632.⟩
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hal-00766394v1  Journal articles
Ali BelmadaniBoris DewitteS.-I. An. ENSO feedbacks and associated time scales of variability in a multimodel ensemble
Journal of Climate, American Meteorological Society, 2010, 23 (12), pp.3181-3204. ISSN 0894-8755. ⟨10.1175/2010jcli2830.1⟩
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