Seismic Network in Greenland Monitors Earth and Ice System

International audience Some of the most dramatic effects of climate change have been observed in the Earth's polar regions. In Greenland, ice loss from the Greenland ice sheet has accelerated in recent years [Shepherd et al., 2012]. Outlet glaciers are changing their behavior rapidly, with many...

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Bibliographic Details
Published in:Eos, Transactions American Geophysical Union
Main Authors: Clinton, John F., Nettles, Meredith, Walter, Fabian, Anderson, Kent, Dahl-Jensen, Trine, Giardini, Domenico, Govoni, Aladino, Hanka, Winfried, Lasocki, Stanislaw, Lee, Won Sang, Mccormack, David, Mykkeltveit, Svein, Stutzmann, Eleonore, Tsuboi, Seiji
Other Authors: Université Grenoble Alpes (UGA), Institut de Physique du Globe de Paris (IPGP), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2014
Subjects:
Online Access:https://hal-insu.archives-ouvertes.fr/insu-03581159
https://hal-insu.archives-ouvertes.fr/insu-03581159/document
https://hal-insu.archives-ouvertes.fr/insu-03581159/file/EoS%20Transactions%20-%202014%20-%20Clinton%20-%20Seismic%20Network%20in%20Greenland%20Monitors%20Earth%20and%20Ice%20System.pdf
https://doi.org/10.1002/2014EO020001
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Summary:International audience Some of the most dramatic effects of climate change have been observed in the Earth's polar regions. In Greenland, ice loss from the Greenland ice sheet has accelerated in recent years [Shepherd et al., 2012]. Outlet glaciers are changing their behavior rapidly, with many thinning, retreating, and accelerating [Joughin et al., 2004]. The loss of ice weighing on the crust and mantle below has allowed both to rebound, resulting in high rock uplift rates [Bevis et al., 2012]. Changes in ice cover and meltwater production influence sea level and climate feedbacks; they are expected to contribute to increasing vulnerability to geohazards such as landslides, flooding, and extreme weather.