Received in revised form
only for improving our understanding of their long-term, decadal– centennial scale, palaeoclimatic history (e.g., Overpeck et al., 1997) but also for developing more accurate climate models that include Arctic amplification. In particular, existing attempts to understand the environmental and climat...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.699.4970 2023-05-15T15:02:40+02:00 Received in revised form The Pennsylvania State University CiteSeerX Archives 2009 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.699.4970 http://www.geo.umass.edu/faculty/jbg/Pubs/Swannetal2010LakeE.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.699.4970 http://www.geo.umass.edu/faculty/jbg/Pubs/Swannetal2010LakeE.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.geo.umass.edu/faculty/jbg/Pubs/Swannetal2010LakeE.pdf Quaternary Scie text 2009 ftciteseerx 2016-01-08T18:48:13Z only for improving our understanding of their long-term, decadal– centennial scale, palaeoclimatic history (e.g., Overpeck et al., 1997) but also for developing more accurate climate models that include Arctic amplification. In particular, existing attempts to understand the environmental and climatic history of west Beringia have been ice-cover with open-water conditions today typically lasting from July to October (Nolan et al., 2003). The catchment, 293 km2, is small relative to the lake surface areawith vegetation characterised by discontinuous lichen and herbaceous taxa and permafrost extending down to depths of 100–300 m (Glushkova,1993; Lozhkin et al., 2007). Importantly, there is strong evidence that neither Lake El’gygytgyn nor the catchment have been glaciated since the lake’s formation, with the nearest evidence of glacial activity located ca 40 km to the west of the catchment (Glushkova, 2001; Glushkova * Corresponding author. Contents lists availab Text Arctic Ice permafrost Beringia Unknown Arctic |
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ftciteseerx |
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English |
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Quaternary Scie |
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Quaternary Scie Received in revised form |
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Quaternary Scie |
description |
only for improving our understanding of their long-term, decadal– centennial scale, palaeoclimatic history (e.g., Overpeck et al., 1997) but also for developing more accurate climate models that include Arctic amplification. In particular, existing attempts to understand the environmental and climatic history of west Beringia have been ice-cover with open-water conditions today typically lasting from July to October (Nolan et al., 2003). The catchment, 293 km2, is small relative to the lake surface areawith vegetation characterised by discontinuous lichen and herbaceous taxa and permafrost extending down to depths of 100–300 m (Glushkova,1993; Lozhkin et al., 2007). Importantly, there is strong evidence that neither Lake El’gygytgyn nor the catchment have been glaciated since the lake’s formation, with the nearest evidence of glacial activity located ca 40 km to the west of the catchment (Glushkova, 2001; Glushkova * Corresponding author. Contents lists availab |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
title |
Received in revised form |
title_short |
Received in revised form |
title_full |
Received in revised form |
title_fullStr |
Received in revised form |
title_full_unstemmed |
Received in revised form |
title_sort |
received in revised form |
publishDate |
2009 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.699.4970 http://www.geo.umass.edu/faculty/jbg/Pubs/Swannetal2010LakeE.pdf |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Ice permafrost Beringia |
genre_facet |
Arctic Ice permafrost Beringia |
op_source |
http://www.geo.umass.edu/faculty/jbg/Pubs/Swannetal2010LakeE.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.699.4970 http://www.geo.umass.edu/faculty/jbg/Pubs/Swannetal2010LakeE.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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