The secret life of ice sails

ABSTRACT We present the first dedicated study into the phenomenon of ice sails . These are clean ice structures that protrude from the surface of a small number of debris-covered glaciers and can grow to heights of over 25 m. We draw together what is known about them from the academic/exploration li...

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Published in:Journal of Glaciology
Main Authors: EVATT, GEOFFREY W., MAYER, CHRISTOPH, MALLINSON, AMY, ABRAHAMS, I. DAVID, HEIL, MATTHIAS, NICHOLSON, LINDSEY
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2017
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2017.72
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143017000727
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spelling crcambridgeupr:10.1017/jog.2017.72 2024-09-15T18:15:39+00:00 The secret life of ice sails EVATT, GEOFFREY W. MAYER, CHRISTOPH MALLINSON, AMY ABRAHAMS, I. DAVID HEIL, MATTHIAS NICHOLSON, LINDSEY 2017 http://dx.doi.org/10.1017/jog.2017.72 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143017000727 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Journal of Glaciology volume 63, issue 242, page 1049-1062 ISSN 0022-1430 1727-5652 journal-article 2017 crcambridgeupr https://doi.org/10.1017/jog.2017.72 2024-07-31T04:03:29Z ABSTRACT We present the first dedicated study into the phenomenon of ice sails . These are clean ice structures that protrude from the surface of a small number of debris-covered glaciers and can grow to heights of over 25 m. We draw together what is known about them from the academic/exploration literature and then analyse imagery. We show here that ice sails can develop by one of two mechanisms, both of which require clean ice to become surrounded by debris-covered ice, where the debris layer is shallow enough for the ice beneath it to melt faster than the clean ice. Once formed, ice sails can persist for decades, in an apparently steady state, before debris layer thickening eventually causes a reversal in the relative melt rates and the ice sails decay to merge back with the surrounding glacier surface. We support our image-based analysis with a surface energy-balance model and show that it compares well with available observations from Baltoro Glacier in the Karakoram. A sensitivity analysis of the model is performed and confirms the results from our empirical study that ice sails require a relatively high evaporative heat flux and/or a relatively low sensible heat flux in order to exist. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 63 242 1049 1062
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description ABSTRACT We present the first dedicated study into the phenomenon of ice sails . These are clean ice structures that protrude from the surface of a small number of debris-covered glaciers and can grow to heights of over 25 m. We draw together what is known about them from the academic/exploration literature and then analyse imagery. We show here that ice sails can develop by one of two mechanisms, both of which require clean ice to become surrounded by debris-covered ice, where the debris layer is shallow enough for the ice beneath it to melt faster than the clean ice. Once formed, ice sails can persist for decades, in an apparently steady state, before debris layer thickening eventually causes a reversal in the relative melt rates and the ice sails decay to merge back with the surrounding glacier surface. We support our image-based analysis with a surface energy-balance model and show that it compares well with available observations from Baltoro Glacier in the Karakoram. A sensitivity analysis of the model is performed and confirms the results from our empirical study that ice sails require a relatively high evaporative heat flux and/or a relatively low sensible heat flux in order to exist.
format Article in Journal/Newspaper
author EVATT, GEOFFREY W.
MAYER, CHRISTOPH
MALLINSON, AMY
ABRAHAMS, I. DAVID
HEIL, MATTHIAS
NICHOLSON, LINDSEY
spellingShingle EVATT, GEOFFREY W.
MAYER, CHRISTOPH
MALLINSON, AMY
ABRAHAMS, I. DAVID
HEIL, MATTHIAS
NICHOLSON, LINDSEY
The secret life of ice sails
author_facet EVATT, GEOFFREY W.
MAYER, CHRISTOPH
MALLINSON, AMY
ABRAHAMS, I. DAVID
HEIL, MATTHIAS
NICHOLSON, LINDSEY
author_sort EVATT, GEOFFREY W.
title The secret life of ice sails
title_short The secret life of ice sails
title_full The secret life of ice sails
title_fullStr The secret life of ice sails
title_full_unstemmed The secret life of ice sails
title_sort secret life of ice sails
publisher Cambridge University Press (CUP)
publishDate 2017
url http://dx.doi.org/10.1017/jog.2017.72
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143017000727
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 63, issue 242, page 1049-1062
ISSN 0022-1430 1727-5652
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2017.72
container_title Journal of Glaciology
container_volume 63
container_issue 242
container_start_page 1049
op_container_end_page 1062
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