Toggle Main Menu Toggle Search

Open Access padlockePrints

Uplift rates from a new high-density GPS network in Palmer Land indicate significant late Holocene ice loss in the southwestern Weddell Sea

Lookup NU author(s): Professor Matt King, Grace Nield

Downloads


Licence

This work is licensed under a Creative Commons Attribution 4.0 International License (CC BY 4.0).


Abstract

The measurement of ongoing ice-mass loss and associated melt water contribution to sea-level change from regions such as West Antarctica is dependent on a combination of remote sensing methods. A key method, the measurement of changes in Earth's gravity via the GRACE satellite mission, requires a potentially large correction to account for the isostatic response of the solid Earth to ice-load changes since the Last Glacial Maximum. In this study, we combine glacial isostatic adjustment modelling with a new GPS dataset of solid Earth deformation for the southern Antarctic Peninsula to test the current understanding of ice history in this region. A sufficiently complete history of past ice-load change is required for glacial isostatic adjustment models to accurately predict the spatial variation of ongoing solid Earth deformation, once the independently-constrained effects of present-day ice mass loss have been accounted for. Comparisons between the GPS data and glacial isostatic adjustment model predictions reveal a substantial misfit. The misfit is localized on the southwestern Weddell Sea, where current ice models under-predict uplift rates by approximately 2 mm yr(-1). This under-prediction suggests that either the retreat of the ice sheet grounding line in this region occurred significantly later in the Holocene than currently assumed, or that the region previously hosted more ice than currently assumed. This finding demonstrates the need for further fieldwork to obtain direct constraints on the timing of Holocene grounding line retreat in the southwestern Weddell Sea and that GRACE estimates of ice sheet mass balance will be unreliable in this region until this is resolved.


Publication metadata

Author(s): Wolstencroft M, King MA, Whitehouse PL, Bentley MJ, Nield GA, King EC, McMillan M, Shepherd A, Barletta V, Bordoni A, Riva REM, Didova O, Gunter BC

Publication type: Article

Publication status: Published

Journal: Geophysical Journal International

Year: 2015

Volume: 203

Issue: 1

Pages: 737-754

Print publication date: 01/10/2015

Acceptance date: 03/08/2015

Date deposited: 05/04/2016

ISSN (print): 0956-540X

ISSN (electronic): 1365-246X

Publisher: Oxford University Press

URL: http://dx.doi.org/10.1093/gji/ggv327

DOI: 10.1093/gji/ggv327


Altmetrics

Altmetrics provided by Altmetric


Funding

Funder referenceFunder name
New Netherlands Polar Programme of the Netherlands Organization for Scientific Research
864.12.012Netherlands Organisation for Scientific Research VIDI grant
EAR-0735156National Aeronautics and Space Administration (NASA) under NSF
FT110100207Australian Research Council
NE/F01452X/1NERC
NE/K009958/1NERC

Share