Modelling the instantaneous response of glaciers after the collapse of the Larsen B Ice Shelf

De Rydt, J.; Gudmundsson, G.H. ORCID: https://orcid.org/0000-0003-4236-5369; Rott, H.; Bamber, J.L.. 2015 Modelling the instantaneous response of glaciers after the collapse of the Larsen B Ice Shelf. Geophysical Research Letters, 42 (13). 5355-5363. https://doi.org/10.1002/2015GL064355

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Abstract/Summary

Following the disintegration of the Larsen B Ice Shelf, Antarctic Peninsula, in 2002, regular surveillance of its ~20 tributary glaciers has revealed a response which is varied and complex in both space and time. The major outlets have accelerated and thinned, smaller glaciers have shown little or no change, and glaciers flowing into the remnant SCAR Inlet Ice Shelf have responded with delay. In this study we present the first area-wide numerical analysis of glacier dynamics before and immediately after the collapse of the ice shelf, combining new datasets and a state-of-the art numerical ice flow model. We simulate the loss of buttressing at the grounding line, and find a good qualitative agreement between modelled changes in glacier flow and observations. Through this study, we seek to improve confidence in our numerical models, and their ability to capture the complex mechanical coupling between floating ice shelves and grounded ice.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1002/2015GL064355
Programmes:	BAS Programmes > BAS Programmes 2015 > Ice Dynamics and Palaeoclimate
ISSN:	0094-8276
Additional Keywords:	Larsen B, glacier speed-up, buttressing, ice-shelf collapse
Date made live:	01 Jul 2015 10:38 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/510979

Item Type:

Publication - Article

Digital Object Identifier (DOI):

https://doi.org/10.1002/2015GL064355

Programmes:

BAS Programmes > BAS Programmes 2015 > Ice Dynamics and Palaeoclimate

ISSN:

0094-8276

Additional Keywords:

Larsen B, glacier speed-up, buttressing, ice-shelf collapse

Date made live:

01 Jul 2015 10:38 +0 (UTC)