GĂINUŞĂ-BOGDAN, Alina; SWINGEDOUW, Didier; YIOU, Pascal; CATTIAUX, Julien; CODRON, Francis; MICHEL, Simon

doi:10.1016/j.gloplacha.2019.103055

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GĂINUŞĂ-BOGDAN, Alina
Environnements et Paléoenvironnements OCéaniques [EPOC]
Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] [LSCE]

SWINGEDOUW, Didier

Environnements et Paléoenvironnements OCéaniques [EPOC]

YIOU, Pascal
Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] [LSCE]
Extrèmes : Statistiques, Impacts et Régionalisation [ESTIMR]

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Este ítem está publicado en

Global and Planetary Change. 2020-01, vol. 184, p. 103055

Resumen en inglés

The mid-Holocene (6,000 years before present) was a warmer period than today in summer in most of the Northern Hemisphere. In winter, over Europe, pollen-based reconstructions show a dipole of temperature anomalies as compared to present-day, with warmer conditions in the north and colder in the south. It has been proposed that this pattern of temperature anomaly could be explained by a persisting positive phase of the North Atlantic Oscillation during this period, which was, however, not reproduced in general by climate models. Indeed, PMIP3 models show a large spread in their response to the mid-Holocene insolation changes, the physical origins of which are not understood. To improve the understanding of the< Leer menos

Palabras clave en inglés

PMIP3

AMOC

NAO

Mid-Holocene

Inter-model spread

URI

https://oskar-bordeaux.fr/handle/20.500.12278/187421

DOI

http://dx.doi.org/10.1016/j.gloplacha.2019.103055

Proyecto europeo

Infrastructure for the European Network for Earth System modelling - Phase 2

Proyecto ANR

LabEx Institut Pierre Simon Laplace (IPSL): Understand climate and anticipate future changes - ANR-10-LABX-0018

Centros de investigación

EPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805