sameAs
Climate change projections using the IPSL-CM5 Earth System Model: from CMIP3 to CMIP5Late-twentieth-century emergence of the El Niño propagation asymmetry and future projections.Multiyear predictability of tropical marine productivity.Bidecadal North Atlantic ocean circulation variability controlled by timing of volcanic eruptions.Tropical explosive volcanic eruptions can trigger El Niño by cooling tropical AfricaPublisher Correction: Tropical explosive volcanic eruptions can trigger El Niño by cooling tropical Africa.Comment on "Multiyear prediction of monthly mean Atlantic Meridional Overturning Circulation at 26.5°N".Author Correction: Tropical explosive volcanic eruptions can trigger El Niño by cooling tropical Africa.The impact of global warming on the tropical Pacific Ocean and El NiñoUsing palaeo-climate comparisons to constrain future projections in CMIP5Mid-Holocene and Last Glacial Maximum climate simulations with the IPSL model—part I: comparing IPSL_CM5A to IPSL_CM4Mid-Holocene and last glacial maximum climate simulations with the IPSL model: part II: model-data comparisonsENSO and greenhouse warmingIncreased frequency of extreme La Niña events under greenhouse warmingIncreasing frequency of extreme El Niño events due to greenhouse warmingObservation and integrated Earth-system science: A roadmap for 2016–2025Towards improved and more routine Earth system model evaluation in CMIPUnderstanding ENSO DiversityEl Niño–Southern Oscillation complexityFourth CLIVAR Workshop on the Evaluation of ENSO Processes in Climate Models: ENSO in a Changing ClimateResponse of El Niño sea surface temperature variability to greenhouse warmingNew Strategies for Evaluating ENSO Processes in Climate ModelsUsing seasonal hindcasts to understand the origin of the equatorial cold tongue bias in CGCMs and its impact on ENSOReconstructing the subsurface ocean decadal variability using surface nudging in a perfect model frameworkIdentifying causes of Western Pacific ITCZ drift in ECMWF System 4 hindcastsNorthward Pathway Across the Tropical North Pacific Ocean Revealed by Surface Salinity: How do El Niño Anomalies Reach Hawaii?Reconstructing extreme AMOC events through nudging of the ocean surface: a perfect model approachTentative reconstruction of the 1998–2012 hiatus in global temperature warming using the IPSL–CM5A–LR climate modelDecadal prediction skill in the ocean with surface nudging in the IPSL-CM5A-LR climate modelModulation of equatorial Pacific westerly/easterly wind events by the Madden–Julian oscillation and convectively-coupled Rossby wavesEffect of surface restoring on subsurface variability in a climate model during 1949–2005Processes driving intraseasonal displacements of the eastern edge of the warm pool: the contribution of westerly wind eventsReconciling two alternative mechanisms behind bi-decadal variability in the North AtlanticThe impact of westerly wind bursts and ocean initial state on the development, and diversity of El Niño eventsA systematic approach to identify the sources of tropical SST errors in coupled models using the adjustment of initialised experimentsDevelopment and exploitation of a controlled vocabulary in support of climate modellingENSO representation in climate models: from CMIP3 to CMIP5Erratum to: Initialisation and predictability of the AMOC over the last 50 years in a climate modelThe impact of westerly wind bursts on the diversity and predictability of El Niño events: An ocean energetics perspectiveDecadal predictability of the Atlantic meridional overturning circulation and climate in the IPSL-CM5A-LR model
P50
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P50
description
Frans klimatoloog
@nl
climate scientist
@en
հետազոտող
@hy
name
Eric Guilyardi
@ast
Eric Guilyardi
@en
Eric Guilyardi
@es
Eric Guilyardi
@nl
Eric Guilyardi
@sl
Éric Guilyardi
@fr
type
label
Eric Guilyardi
@ast
Eric Guilyardi
@en
Eric Guilyardi
@es
Eric Guilyardi
@nl
Eric Guilyardi
@sl
Éric Guilyardi
@fr
prefLabel
Eric Guilyardi
@ast
Eric Guilyardi
@en
Eric Guilyardi
@es
Eric Guilyardi
@nl
Eric Guilyardi
@sl
Éric Guilyardi
@fr
P1053
D-4868-2011
P21
P27
P31
P3630
P3829
P496
0000-0002-2255-8625
P569
1966-01-01T00:00:00Z