z-logo
open-access-imgOpen Access
Seismic Network in Greenland Monitors Earth and Ice System
Author(s) -
Clinton John F.,
Nettles Meredith,
Walter Fabian,
Anderson Kent,
DahlJensen Trine,
Giardini Domenico,
Govoni Aladino,
Hanka Winfried,
Lasocki Stanislaw,
Lee Won Sang,
McCormack David,
Mykkeltveit Svein,
Stutzmann Eleonore,
Tsuboi Seiji
Publication year - 2014
Publication title -
eos, transactions american geophysical union
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.316
H-Index - 86
eISSN - 2324-9250
pISSN - 0096-3941
DOI - 10.1002/2014eo020001
Subject(s) - geology , meltwater , greenland ice sheet , glacier , climatology , ice sheet , antarctic sea ice , sea ice , cryosphere , ice sheet model , ice divide , arctic ice pack , ice stream , future sea level , climate change , ice albedo feedback , physical geography , oceanography , geomorphology , geography
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.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here
Accelerating Research

Address

John Eccles House
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom