Wind-borne redistribution of snow across an Antarctic ice rise
[1] Redistribution of snow by the wind can drive spatial and temporal variations in snow accumulation that may affect the reconstruction of paleoclimate records from ice cores. In this paper we investigate how spatial variations in snow accumulation along a 13 km transect across Lyddan Ice Rise, Ant...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.573.6889 2023-05-15T13:56:11+02:00 Wind-borne redistribution of snow across an Antarctic ice rise J. C. King P. S. Anderson D. G. Vaughan G. W. Mann S. D. Mobbs S. B. Vosper The Pennsylvania State University CiteSeerX Archives 2004 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.573.6889 http://appconv.metoffice.com/3dvom_op/king_et_al_lyddan_jgr_2004.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.573.6889 http://appconv.metoffice.com/3dvom_op/king_et_al_lyddan_jgr_2004.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://appconv.metoffice.com/3dvom_op/king_et_al_lyddan_jgr_2004.pdf Dynamics text 2004 ftciteseerx 2016-01-08T12:39:10Z [1] Redistribution of snow by the wind can drive spatial and temporal variations in snow accumulation that may affect the reconstruction of paleoclimate records from ice cores. In this paper we investigate how spatial variations in snow accumulation along a 13 km transect across Lyddan Ice Rise, Antarctica, are related to wind-borne snow redistribution. Lyddan Ice Rise is an approximately two-dimensional ridge which rises about 130 m above the surrounding ice shelves. Local slopes on its flanks never exceed 0.04. Despite this very smooth profile, there is a pronounced gradient in snow accumulation across the feature. Accumulation is highest on the ice shelf to the east (climatologically upwind) of the ice rise and decreases moving westward, with the lowest accumulation seen to the west (climatologically downwind) of the ice rise crest. Superimposed on this broad-scale gradient are large (20–30%), localized variations in accumulation on a scale of around 1 km that appear to be associated with local variations in surface slope of less than 0.01. The broad-scale accumulation gradient is consistent with estimates of wind-borne redistribution of snow made using wind speed observations from three automatic weather stations. The small-scale variability in accumulation is reproduced quite well using a snow transport Text Antarc* Antarctic Antarctica Ice Shelf Ice Shelves Unknown Antarctic Lyddan Ice Rise ENVELOPE(-21.000,-21.000,-74.167,-74.167) |
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English |
topic |
Dynamics |
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Dynamics J. C. King P. S. Anderson D. G. Vaughan G. W. Mann S. D. Mobbs S. B. Vosper Wind-borne redistribution of snow across an Antarctic ice rise |
topic_facet |
Dynamics |
description |
[1] Redistribution of snow by the wind can drive spatial and temporal variations in snow accumulation that may affect the reconstruction of paleoclimate records from ice cores. In this paper we investigate how spatial variations in snow accumulation along a 13 km transect across Lyddan Ice Rise, Antarctica, are related to wind-borne snow redistribution. Lyddan Ice Rise is an approximately two-dimensional ridge which rises about 130 m above the surrounding ice shelves. Local slopes on its flanks never exceed 0.04. Despite this very smooth profile, there is a pronounced gradient in snow accumulation across the feature. Accumulation is highest on the ice shelf to the east (climatologically upwind) of the ice rise and decreases moving westward, with the lowest accumulation seen to the west (climatologically downwind) of the ice rise crest. Superimposed on this broad-scale gradient are large (20–30%), localized variations in accumulation on a scale of around 1 km that appear to be associated with local variations in surface slope of less than 0.01. The broad-scale accumulation gradient is consistent with estimates of wind-borne redistribution of snow made using wind speed observations from three automatic weather stations. The small-scale variability in accumulation is reproduced quite well using a snow transport |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
J. C. King P. S. Anderson D. G. Vaughan G. W. Mann S. D. Mobbs S. B. Vosper |
author_facet |
J. C. King P. S. Anderson D. G. Vaughan G. W. Mann S. D. Mobbs S. B. Vosper |
author_sort |
J. C. King |
title |
Wind-borne redistribution of snow across an Antarctic ice rise |
title_short |
Wind-borne redistribution of snow across an Antarctic ice rise |
title_full |
Wind-borne redistribution of snow across an Antarctic ice rise |
title_fullStr |
Wind-borne redistribution of snow across an Antarctic ice rise |
title_full_unstemmed |
Wind-borne redistribution of snow across an Antarctic ice rise |
title_sort |
wind-borne redistribution of snow across an antarctic ice rise |
publishDate |
2004 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.573.6889 http://appconv.metoffice.com/3dvom_op/king_et_al_lyddan_jgr_2004.pdf |
long_lat |
ENVELOPE(-21.000,-21.000,-74.167,-74.167) |
geographic |
Antarctic Lyddan Ice Rise |
geographic_facet |
Antarctic Lyddan Ice Rise |
genre |
Antarc* Antarctic Antarctica Ice Shelf Ice Shelves |
genre_facet |
Antarc* Antarctic Antarctica Ice Shelf Ice Shelves |
op_source |
http://appconv.metoffice.com/3dvom_op/king_et_al_lyddan_jgr_2004.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.573.6889 http://appconv.metoffice.com/3dvom_op/king_et_al_lyddan_jgr_2004.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766263556450287616 |