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Model evidence for a seasonal bias in Antarctic ice cores

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Erb, Michael P. Jackson, Charles S. Broccoli, Anthony J. Lea, David W. Valdes, Paul J. Crucifix, Michel [UCL] DiNezio, Pedro N.

Much of the global annual mean temperature change over Quaternary glacial cycles can be attributed to slow ice sheet and greenhouse gas feedbacks, but analysis of the short-term response to orbital forcings has the potential to reveal key relationships in the climate system. In particular, obliquity and precession both produce highly seasonal temperature responses at high latitudes. Here, idealized single-forcing model experiments are used to quantify Earth’s response to obliquity, precession, CO2, and ice sheets, and a linear reconstruction methodology is used to compare these responses to long proxy records around the globe. This comparison reveals mismatches between the annual mean response to obliquity and precession in models versus the signals within Antarctic ice cores. Weighting the model-based reconstruction toward austral winter or spring reduces these discrepancies, providing evidence for a seasonal bias in ice cores.

Type de document Article de périodique (Journal article) – Article de recherche
Type d'accès Accès libre
Année de publication 2018
Langue Anglais
Information sur le périodique "Nature Communications" - Vol. 9, no.1, p. 1361 (2018)
Peer reviewed oui
Editeur Springer Nature
e-issn 2041-1723
Statut de la publication Publié
Affiliations UCL - SST/ELI/ELIC - Earth & Climate
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Référence bibliographique Erb, Michael P. ; Jackson, Charles S. ; Broccoli, Anthony J. ; Lea, David W. ; Valdes, Paul J. ; et. al. Model evidence for a seasonal bias in Antarctic ice cores. In: Nature Communications, Vol. 9, no.1, p. 1361 (2018)
Permalien http://hdl.handle.net/2078.1/199243