On the response of rockglacier cree

entire deactivation. By means of three scenarios, we exemplify the possible consequences of an increase in rockglacier temperature and ditions are able to form prominent creep streams — so-called rockglaciers. These features creep with surface speeds in the order of centimetres to several metres per...

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Bibliographic Details
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2005
Subjects:
rockglacier
creep
mountain permafrost
climate change
warming
slope stability
permafrost
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.488.8093
http://folk.uio.no/kaeaeb/publications/gpc_rockglacier.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.488.8093 2023-05-15T17:57:23+02:00 On the response of rockglacier cree The Pennsylvania State University CiteSeerX Archives 2005 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.488.8093 http://folk.uio.no/kaeaeb/publications/gpc_rockglacier.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.488.8093 http://folk.uio.no/kaeaeb/publications/gpc_rockglacier.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://folk.uio.no/kaeaeb/publications/gpc_rockglacier.pdf rockglacier creep mountain permafrost climate change warming slope stability text 2005 ftciteseerx 2016-01-08T08:20:54Z entire deactivation. By means of three scenarios, we exemplify the possible consequences of an increase in rockglacier temperature and ditions are able to form prominent creep streams — so-called rockglaciers. These features creep with surface speeds in the order of centimetres to several metres per Global and Planetary Change 56 ⁎ Corresponding author. Department of Geosciences, University ofsubsequent acceleration: (1) increasing sensitivity of rockglacier creep to seasonal influences, (2) activation of so far stable frozen debris slopes, and (3) rockglacier destabilization. Text permafrost Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic rockglacier
creep
mountain permafrost
climate change
warming
slope stability
spellingShingle rockglacier
creep
mountain permafrost
climate change
warming
slope stability
On the response of rockglacier cree
topic_facet rockglacier
creep
mountain permafrost
climate change
warming
slope stability
description entire deactivation. By means of three scenarios, we exemplify the possible consequences of an increase in rockglacier temperature and ditions are able to form prominent creep streams — so-called rockglaciers. These features creep with surface speeds in the order of centimetres to several metres per Global and Planetary Change 56 ⁎ Corresponding author. Department of Geosciences, University ofsubsequent acceleration: (1) increasing sensitivity of rockglacier creep to seasonal influences, (2) activation of so far stable frozen debris slopes, and (3) rockglacier destabilization.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
title On the response of rockglacier cree
title_short On the response of rockglacier cree
title_full On the response of rockglacier cree
title_fullStr On the response of rockglacier cree
title_full_unstemmed On the response of rockglacier cree
title_sort on the response of rockglacier cree
publishDate 2005
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.488.8093
http://folk.uio.no/kaeaeb/publications/gpc_rockglacier.pdf
genre permafrost
genre_facet permafrost
op_source http://folk.uio.no/kaeaeb/publications/gpc_rockglacier.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.488.8093
http://folk.uio.no/kaeaeb/publications/gpc_rockglacier.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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