Antarctic Katabatic Winds
Katabatic winds ('kata', from the Greek for downwards) are observed at every latitude of the globe as soon as a coarse of cooled air meets a significant slope, but nowhere are they as strong as Antarctica. Unlike winds in other parts of the world, Antarctica's katabatic winds are caus...
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University of Canterbury
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ftunivcanter:oai:ir.canterbury.ac.nz:10092/13972 2023-05-15T13:49:08+02:00 Antarctic Katabatic Winds Brockett, David 2005 application/pdf http://hdl.handle.net/10092/13972 English en eng University of Canterbury http://hdl.handle.net/10092/13972 All Rights Reserved Theses / Dissertations 2005 ftunivcanter 2022-09-08T13:37:29Z Katabatic winds ('kata', from the Greek for downwards) are observed at every latitude of the globe as soon as a coarse of cooled air meets a significant slope, but nowhere are they as strong as Antarctica. Unlike winds in other parts of the world, Antarctica's katabatic winds are caused by the shape of the land: cold, dense air on the high ice sheet flows down the coastal slopes under the influence of gravity. Simply put, katabatic wind is cold dense air that pours down the ice slope to the sea, becoming denser and picking up speed as it goes. Antarctica produces the strongest and most enduring katabatic winds as it is the highest and coldest continent. Other/Unknown Material Antarc* Antarctic Antarctica Ice Sheet University of Canterbury, Christchurch: UC Research Repository Antarctic |
institution |
Open Polar |
collection |
University of Canterbury, Christchurch: UC Research Repository |
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ftunivcanter |
language |
English |
description |
Katabatic winds ('kata', from the Greek for downwards) are observed at every latitude of the globe as soon as a coarse of cooled air meets a significant slope, but nowhere are they as strong as Antarctica. Unlike winds in other parts of the world, Antarctica's katabatic winds are caused by the shape of the land: cold, dense air on the high ice sheet flows down the coastal slopes under the influence of gravity. Simply put, katabatic wind is cold dense air that pours down the ice slope to the sea, becoming denser and picking up speed as it goes. Antarctica produces the strongest and most enduring katabatic winds as it is the highest and coldest continent. |
format |
Other/Unknown Material |
author |
Brockett, David |
spellingShingle |
Brockett, David Antarctic Katabatic Winds |
author_facet |
Brockett, David |
author_sort |
Brockett, David |
title |
Antarctic Katabatic Winds |
title_short |
Antarctic Katabatic Winds |
title_full |
Antarctic Katabatic Winds |
title_fullStr |
Antarctic Katabatic Winds |
title_full_unstemmed |
Antarctic Katabatic Winds |
title_sort |
antarctic katabatic winds |
publisher |
University of Canterbury |
publishDate |
2005 |
url |
http://hdl.handle.net/10092/13972 |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic Antarctica Ice Sheet |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet |
op_relation |
http://hdl.handle.net/10092/13972 |
op_rights |
All Rights Reserved |
_version_ |
1766250871036837888 |