Ice scour disturbance in Antarctic waters

The West Antarctic Peninsula is one of the fastest warming regions on Earth, and, as a consequence, most maritime glaciers and ice shelves in the region have significantly retreated over the past few decades. We collected a multiyear data set on ice scouring frequency from Antarctica by using unique...

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Published in:Science
Main Authors: Smale, Dan A., Brown, Kirsty M., Barnes, David K.A., Fraser, Keiron P.P., Clarke, Andrew
Format: Article in Journal/Newspaper
Language:unknown
Published: 2008
Subjects:
Online Access:https://eprints.soton.ac.uk/348310/
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spelling ftsouthampton:oai:eprints.soton.ac.uk:348310 2023-07-30T03:59:26+02:00 Ice scour disturbance in Antarctic waters Smale, Dan A. Brown, Kirsty M. Barnes, David K.A. Fraser, Keiron P.P. Clarke, Andrew 2008-07-18 https://eprints.soton.ac.uk/348310/ unknown Smale, Dan A., Brown, Kirsty M., Barnes, David K.A., Fraser, Keiron P.P. and Clarke, Andrew (2008) Ice scour disturbance in Antarctic waters. Science, 321 (5887), 371. (doi:10.1126/science.1158647 <http://dx.doi.org/10.1126/science.1158647>). Article PeerReviewed 2008 ftsouthampton https://doi.org/10.1126/science.1158647 2023-07-09T21:44:12Z The West Antarctic Peninsula is one of the fastest warming regions on Earth, and, as a consequence, most maritime glaciers and ice shelves in the region have significantly retreated over the past few decades. We collected a multiyear data set on ice scouring frequency from Antarctica by using unique experimental markers and scuba diving surveys. We show that the annual intensity of ice scouring is negatively correlated with the duration of the winter fast ice season. Because fast ice extent and duration is currently in decline in the region after recent rapid warming, it is likely that marine benthic communities are set for even more scouring in the near future. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctica Ice Shelves University of Southampton: e-Prints Soton Antarctic Antarctic Peninsula Science 321 5887 371 371
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id ftsouthampton
language unknown
description The West Antarctic Peninsula is one of the fastest warming regions on Earth, and, as a consequence, most maritime glaciers and ice shelves in the region have significantly retreated over the past few decades. We collected a multiyear data set on ice scouring frequency from Antarctica by using unique experimental markers and scuba diving surveys. We show that the annual intensity of ice scouring is negatively correlated with the duration of the winter fast ice season. Because fast ice extent and duration is currently in decline in the region after recent rapid warming, it is likely that marine benthic communities are set for even more scouring in the near future.
format Article in Journal/Newspaper
author Smale, Dan A.
Brown, Kirsty M.
Barnes, David K.A.
Fraser, Keiron P.P.
Clarke, Andrew
spellingShingle Smale, Dan A.
Brown, Kirsty M.
Barnes, David K.A.
Fraser, Keiron P.P.
Clarke, Andrew
Ice scour disturbance in Antarctic waters
author_facet Smale, Dan A.
Brown, Kirsty M.
Barnes, David K.A.
Fraser, Keiron P.P.
Clarke, Andrew
author_sort Smale, Dan A.
title Ice scour disturbance in Antarctic waters
title_short Ice scour disturbance in Antarctic waters
title_full Ice scour disturbance in Antarctic waters
title_fullStr Ice scour disturbance in Antarctic waters
title_full_unstemmed Ice scour disturbance in Antarctic waters
title_sort ice scour disturbance in antarctic waters
publishDate 2008
url https://eprints.soton.ac.uk/348310/
geographic Antarctic
Antarctic Peninsula
geographic_facet Antarctic
Antarctic Peninsula
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Ice Shelves
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Ice Shelves
op_relation Smale, Dan A., Brown, Kirsty M., Barnes, David K.A., Fraser, Keiron P.P. and Clarke, Andrew (2008) Ice scour disturbance in Antarctic waters. Science, 321 (5887), 371. (doi:10.1126/science.1158647 <http://dx.doi.org/10.1126/science.1158647>).
op_doi https://doi.org/10.1126/science.1158647
container_title Science
container_volume 321
container_issue 5887
container_start_page 371
op_container_end_page 371
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