Understanding and Modelling Rapid Dynamic Changes of Tidewater Outlet Glaciers: Issues and Implications

Recent dramatic acceleration, thinning and retreat of tidewater outlet glaciers in Greenland raises concern regarding their contribution to future sea-level rise. These dynamic changes seem to be parallel to oceanic and climatic warming but the linking mechanisms and forcings are poorly understood a...

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Main Authors: Vieli, Andreas, Nick, Faezeh
Language:English
Published: 2018
Subjects:
Online Access:http://doc.rero.ch/record/318814/files/10712_2011_Article_9132.pdf
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spelling ftreroch:oai:doc.rero.ch:318814 2023-05-15T16:21:23+02:00 Understanding and Modelling Rapid Dynamic Changes of Tidewater Outlet Glaciers: Issues and Implications Vieli, Andreas Nick, Faezeh 2018-06-18T17:54:59Z http://doc.rero.ch/record/318814/files/10712_2011_Article_9132.pdf eng eng http://doc.rero.ch/record/318814/files/10712_2011_Article_9132.pdf 2018 ftreroch 2023-02-16T17:32:15Z Recent dramatic acceleration, thinning and retreat of tidewater outlet glaciers in Greenland raises concern regarding their contribution to future sea-level rise. These dynamic changes seem to be parallel to oceanic and climatic warming but the linking mechanisms and forcings are poorly understood and, furthermore, large-scale ice sheet models are currently unable to realistically simulate such changes which provides a major limitation in our ability to predict dynamic mass losses. In this paper we apply a specifically designed numerical flowband model to Jakobshavn Isbrae (JIB), a major marine outlet glacier of the Greenland ice sheet, and we explore and discuss the basic concepts and emerging issues in our understanding and modelling ability of the dynamics of tidewater outlet glaciers. The modelling demonstrates that enhanced ocean melt is able to trigger the observed dynamic changes of JIB but it heavily relies on the feedback between calving and terminus retreat and therefore the loss of buttressing. Through the same feedback, other forcings such as reduced winter sea-ice duration can produce similar rapid retreat. This highlights the need for a robust representation of the calving process and for improvements in the understanding and implementation of forcings at the marine boundary in predictive ice sheet models. Furthermore, the modelling uncovers high sensitivity and rapid adjustment of marine outlet glaciers to perturbations at their marine boundary implying that care should be taken in interpreting or extrapolating such rapid dynamic changes as recently observed in Greenland Other/Unknown Material glacier Greenland Ice Sheet Jakobshavn Sea ice Tidewater RERO DOC Digital Library Greenland
institution Open Polar
collection RERO DOC Digital Library
op_collection_id ftreroch
language English
description Recent dramatic acceleration, thinning and retreat of tidewater outlet glaciers in Greenland raises concern regarding their contribution to future sea-level rise. These dynamic changes seem to be parallel to oceanic and climatic warming but the linking mechanisms and forcings are poorly understood and, furthermore, large-scale ice sheet models are currently unable to realistically simulate such changes which provides a major limitation in our ability to predict dynamic mass losses. In this paper we apply a specifically designed numerical flowband model to Jakobshavn Isbrae (JIB), a major marine outlet glacier of the Greenland ice sheet, and we explore and discuss the basic concepts and emerging issues in our understanding and modelling ability of the dynamics of tidewater outlet glaciers. The modelling demonstrates that enhanced ocean melt is able to trigger the observed dynamic changes of JIB but it heavily relies on the feedback between calving and terminus retreat and therefore the loss of buttressing. Through the same feedback, other forcings such as reduced winter sea-ice duration can produce similar rapid retreat. This highlights the need for a robust representation of the calving process and for improvements in the understanding and implementation of forcings at the marine boundary in predictive ice sheet models. Furthermore, the modelling uncovers high sensitivity and rapid adjustment of marine outlet glaciers to perturbations at their marine boundary implying that care should be taken in interpreting or extrapolating such rapid dynamic changes as recently observed in Greenland
author Vieli, Andreas
Nick, Faezeh
spellingShingle Vieli, Andreas
Nick, Faezeh
Understanding and Modelling Rapid Dynamic Changes of Tidewater Outlet Glaciers: Issues and Implications
author_facet Vieli, Andreas
Nick, Faezeh
author_sort Vieli, Andreas
title Understanding and Modelling Rapid Dynamic Changes of Tidewater Outlet Glaciers: Issues and Implications
title_short Understanding and Modelling Rapid Dynamic Changes of Tidewater Outlet Glaciers: Issues and Implications
title_full Understanding and Modelling Rapid Dynamic Changes of Tidewater Outlet Glaciers: Issues and Implications
title_fullStr Understanding and Modelling Rapid Dynamic Changes of Tidewater Outlet Glaciers: Issues and Implications
title_full_unstemmed Understanding and Modelling Rapid Dynamic Changes of Tidewater Outlet Glaciers: Issues and Implications
title_sort understanding and modelling rapid dynamic changes of tidewater outlet glaciers: issues and implications
publishDate 2018
url http://doc.rero.ch/record/318814/files/10712_2011_Article_9132.pdf
geographic Greenland
geographic_facet Greenland
genre glacier
Greenland
Ice Sheet
Jakobshavn
Sea ice
Tidewater
genre_facet glacier
Greenland
Ice Sheet
Jakobshavn
Sea ice
Tidewater
op_relation http://doc.rero.ch/record/318814/files/10712_2011_Article_9132.pdf
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