NAUGHTON, Filipa; SANCHEZ GONI, Maria Fernanda; LANDAIS, Amaelle; RODRIGUES, Teresa; RIVEIROS, Natalia Vazquez; TOUCANNE, Samuel

doi:10.1016/B978-0-323-91899-2.00015-2

Métadonnées

Afficher la notice complète

Licence d’utilisation du document

NAUGHTON, Filipa

SANCHEZ GONI, Maria Fernanda
Environnements et Paléoenvironnements OCéaniques [EPOC]

LANDAIS, Amaelle

Langue

Chapitre d'ouvrage

Ce document a été publié dans

European Glacial Landscapes: The Last Deglaciation. 2023-01-01p. 45-50

Résumé en anglais

The Bølling–Allerød (B-A), the terrestrial counterpart of Dansgaard–Oeschger 1, is the first abrupt northern hemisphere climate warming episode of the last deglaciation. Several hypotheses have been proposed to explain this event: all involve the strengthening of the Atlantic Meridional Overturning Circulation (AMOC) prior or during the Heinrich Stadial 1/B-A transition and the consequent warming of the northern hemisphere. Terrestrial proxies (mainly pollen and speleothems) reflect a progressive increase in moisture availability from the Bølling to the Allerød in Europe contrasting with Greenland isotope records which show maxima in temperature and precipitation at the onset of the Bølling and a gradual decrease to the end of the Allerød. Changes in moisture availability in Europe are triggered by coupled interactions between the AMOC and changes in atmospheric dynamics led by the westerlies.< Réduire

Métadonnées

Partager cette publication !

Licence d’utilisation du document

Chapter 6 - The Bølling–Allerød Interstadial

Langue

Ce document a été publié dans

Résumé en anglais

URI

DOI

Unités de recherche