A reconstruction of warm water inflow to Upernavik Isstrøm since AD 1925 and its relation to glacier retreat

International audience The mass loss from the Greenland Ice Sheet has increased over the past 2 decades. Marine-terminating glaciers contribute significantly to this mass loss due to increased melting and ice discharge. Periods of rapid retreat of these tidewater glaciers have been linked to the con...

Full description

Bibliographic Details
Published in:Climate of the Past
Main Authors: Vermassen, Flor, Andreasen, Nanna, Wangner, David, Thibault, Nicolas, Seidenkrantz, Marit-Solveig, Jackson, Rebecca, Schmidt, Sabine, Kjær, Kurt, Andresen, Camilla
Other Authors: Geological Survey of Denmark and Greenland (GEUS), Department of Geosciences and Natural Resource Management Copenhagen (IGN), Faculty of Science Copenhagen, University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH), Aarhus University Aarhus, Ohio State University Columbus (OSU), UMR 5805 Environnements et Paléoenvironnements Océaniques et Continentaux (EPOC), Observatoire aquitain des sciences de l'univers (OASU), Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École pratique des hautes études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2019
Subjects:
Online Access:https://hal.science/hal-02357272
https://hal.science/hal-02357272/document
https://hal.science/hal-02357272/file/cp-15-1171-2019.pdf
https://doi.org/10.5194/cp-15-1171-2019