Observations of debris-rich naled associated with a major glacier surge event, Disko Island, West Greenland

Glacier naled formation is associated with surge‐type glaciers both during active surging and in quiescence. During the 1995–98 surge of Kuannersuit Glacier, Disko Island, West Greenland, turbid winter runoff produced an extensive naled accretion with a distinct debris‐rich stratification. After sur...

Full description

Saved in:
Bibliographic Details
Published in:Permafrost and periglacial processes 2005-10, Vol.16 (4), p.319-325
Main Authors: Yde, Jacob Clement, Knudsen, N. Tvis
Format: Article
Language:English
Subjects:
Bgi / Prodig
Greenland
Hydrometeorology
naled
Nivology. Glaciology
Physical geography
surge-type glaciers
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-a3833-63b4b37e2e6f3678f52e3157dbd9a608ab857bbba0c28ac1231afdb340d181cc3
cites cdi_FETCH-LOGICAL-a3833-63b4b37e2e6f3678f52e3157dbd9a608ab857bbba0c28ac1231afdb340d181cc3
container_end_page 325
container_issue 4
container_start_page 319
container_title Permafrost and periglacial processes
container_volume 16
creator Yde, Jacob Clement
Knudsen, N. Tvis
description Glacier naled formation is associated with surge‐type glaciers both during active surging and in quiescence. During the 1995–98 surge of Kuannersuit Glacier, Disko Island, West Greenland, turbid winter runoff produced an extensive naled accretion with a distinct debris‐rich stratification. After surge termination the summer occurrence of naledi gradually decreased and disappeared within 5 years. The fine‐grained debris was deposited on top of outwash deposits on bars and banks. Observations at the margin of surrounding glaciers revealed that only surge‐type glaciers in their quiescent phase had proglacial naled assemblages, although these lacked incorporated debris. This indicates that surge‐type glaciers have a significant impact on the occurrence of naledi primarily because their subglacial thermal conditions and water storage capacity allow significant winter runoff implying high hydraulic pressure on proglacial outwash plains. Copyright © 2005 John Wiley & Sons, Ltd.
doi_str_mv 10.1002/ppp.533
format article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_17217008</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>17217008</sourcerecordid><originalsourceid>FETCH-LOGICAL-a3833-63b4b37e2e6f3678f52e3157dbd9a608ab857bbba0c28ac1231afdb340d181cc3</originalsourceid><addsrcrecordid>eNp1kEFv1DAQhS0EEmVB_AVfgEOb1s4kcfaIStlWqtpUAvZojZ1J6242CZ5sS_99s0oFJ07zRvr09PQJ8VGrY61UejIMw3EO8EocaLVcJjoH9XqfszwpTKbeinfM90qpEnR2IDbXjik-4Bj6jmXfyJpcDJzE4O9khy3VEpl7H3Cc4mMY7yTKLd73Ud626ANFybt4S5IeqBuP5LfAm15ecItdfSTXxKNcRaJu_78XbxpsmT683IX4-f3sx-l5cnm9ujj9epkglABJAS5zYCilooHClE2eEujc1K5eYqFKdGVunHOofFqi1ylobGoHmap1qb2Hhfg89w6x_72bJthtYE_ttIH6HVttUm32Ahbiywz62DNHauwQwxbjk9XK7mXaSaadZE7kp5dKZI9tE7Hzgf_hJjNL0HriDmfuMbT09L86W1XV3JrMdOCR_vylMW5sYcDkdn21suvqqvqV3xhbwTPqPZJI</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>17217008</pqid></control><display><type>article</type><title>Observations of debris-rich naled associated with a major glacier surge event, Disko Island, West Greenland</title><source>Wiley</source><creator>Yde, Jacob Clement ; Knudsen, N. Tvis</creator><creatorcontrib>Yde, Jacob Clement ; Knudsen, N. Tvis</creatorcontrib><description>Glacier naled formation is associated with surge‐type glaciers both during active surging and in quiescence. During the 1995–98 surge of Kuannersuit Glacier, Disko Island, West Greenland, turbid winter runoff produced an extensive naled accretion with a distinct debris‐rich stratification. After surge termination the summer occurrence of naledi gradually decreased and disappeared within 5 years. The fine‐grained debris was deposited on top of outwash deposits on bars and banks. Observations at the margin of surrounding glaciers revealed that only surge‐type glaciers in their quiescent phase had proglacial naled assemblages, although these lacked incorporated debris. This indicates that surge‐type glaciers have a significant impact on the occurrence of naledi primarily because their subglacial thermal conditions and water storage capacity allow significant winter runoff implying high hydraulic pressure on proglacial outwash plains. Copyright © 2005 John Wiley &amp; Sons, Ltd.</description><identifier>ISSN: 1045-6740</identifier><identifier>EISSN: 1099-1530</identifier><identifier>DOI: 10.1002/ppp.533</identifier><identifier>CODEN: PEPPED</identifier><language>eng</language><publisher>Chichester, UK: John Wiley &amp; Sons, Ltd</publisher><subject>Bgi / Prodig ; Greenland ; Hydrometeorology ; naled ; Nivology. Glaciology ; Physical geography ; surge-type glaciers</subject><ispartof>Permafrost and periglacial processes, 2005-10, Vol.16 (4), p.319-325</ispartof><rights>Copyright © 2005 John Wiley &amp; Sons, Ltd.</rights><rights>Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 2006</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a3833-63b4b37e2e6f3678f52e3157dbd9a608ab857bbba0c28ac1231afdb340d181cc3</citedby><cites>FETCH-LOGICAL-a3833-63b4b37e2e6f3678f52e3157dbd9a608ab857bbba0c28ac1231afdb340d181cc3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=17479311$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Yde, Jacob Clement</creatorcontrib><creatorcontrib>Knudsen, N. Tvis</creatorcontrib><title>Observations of debris-rich naled associated with a major glacier surge event, Disko Island, West Greenland</title><title>Permafrost and periglacial processes</title><addtitle>Permafrost Periglac. Process</addtitle><description>Glacier naled formation is associated with surge‐type glaciers both during active surging and in quiescence. During the 1995–98 surge of Kuannersuit Glacier, Disko Island, West Greenland, turbid winter runoff produced an extensive naled accretion with a distinct debris‐rich stratification. After surge termination the summer occurrence of naledi gradually decreased and disappeared within 5 years. The fine‐grained debris was deposited on top of outwash deposits on bars and banks. Observations at the margin of surrounding glaciers revealed that only surge‐type glaciers in their quiescent phase had proglacial naled assemblages, although these lacked incorporated debris. This indicates that surge‐type glaciers have a significant impact on the occurrence of naledi primarily because their subglacial thermal conditions and water storage capacity allow significant winter runoff implying high hydraulic pressure on proglacial outwash plains. Copyright © 2005 John Wiley &amp; Sons, Ltd.</description><subject>Bgi / Prodig</subject><subject>Greenland</subject><subject>Hydrometeorology</subject><subject>naled</subject><subject>Nivology. Glaciology</subject><subject>Physical geography</subject><subject>surge-type glaciers</subject><issn>1045-6740</issn><issn>1099-1530</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2005</creationdate><recordtype>article</recordtype><recordid>eNp1kEFv1DAQhS0EEmVB_AVfgEOb1s4kcfaIStlWqtpUAvZojZ1J6242CZ5sS_99s0oFJ07zRvr09PQJ8VGrY61UejIMw3EO8EocaLVcJjoH9XqfszwpTKbeinfM90qpEnR2IDbXjik-4Bj6jmXfyJpcDJzE4O9khy3VEpl7H3Cc4mMY7yTKLd73Ud626ANFybt4S5IeqBuP5LfAm15ecItdfSTXxKNcRaJu_78XbxpsmT683IX4-f3sx-l5cnm9ujj9epkglABJAS5zYCilooHClE2eEujc1K5eYqFKdGVunHOofFqi1ylobGoHmap1qb2Hhfg89w6x_72bJthtYE_ttIH6HVttUm32Ahbiywz62DNHauwQwxbjk9XK7mXaSaadZE7kp5dKZI9tE7Hzgf_hJjNL0HriDmfuMbT09L86W1XV3JrMdOCR_vylMW5sYcDkdn21suvqqvqV3xhbwTPqPZJI</recordid><startdate>200510</startdate><enddate>200510</enddate><creator>Yde, Jacob Clement</creator><creator>Knudsen, N. Tvis</creator><general>John Wiley &amp; Sons, Ltd</general><general>Wiley</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>KL.</scope></search><sort><creationdate>200510</creationdate><title>Observations of debris-rich naled associated with a major glacier surge event, Disko Island, West Greenland</title><author>Yde, Jacob Clement ; Knudsen, N. Tvis</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a3833-63b4b37e2e6f3678f52e3157dbd9a608ab857bbba0c28ac1231afdb340d181cc3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2005</creationdate><topic>Bgi / Prodig</topic><topic>Greenland</topic><topic>Hydrometeorology</topic><topic>naled</topic><topic>Nivology. Glaciology</topic><topic>Physical geography</topic><topic>surge-type glaciers</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Yde, Jacob Clement</creatorcontrib><creatorcontrib>Knudsen, N. Tvis</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><jtitle>Permafrost and periglacial processes</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Yde, Jacob Clement</au><au>Knudsen, N. Tvis</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Observations of debris-rich naled associated with a major glacier surge event, Disko Island, West Greenland</atitle><jtitle>Permafrost and periglacial processes</jtitle><addtitle>Permafrost Periglac. Process</addtitle><date>2005-10</date><risdate>2005</risdate><volume>16</volume><issue>4</issue><spage>319</spage><epage>325</epage><pages>319-325</pages><issn>1045-6740</issn><eissn>1099-1530</eissn><coden>PEPPED</coden><abstract>Glacier naled formation is associated with surge‐type glaciers both during active surging and in quiescence. During the 1995–98 surge of Kuannersuit Glacier, Disko Island, West Greenland, turbid winter runoff produced an extensive naled accretion with a distinct debris‐rich stratification. After surge termination the summer occurrence of naledi gradually decreased and disappeared within 5 years. The fine‐grained debris was deposited on top of outwash deposits on bars and banks. Observations at the margin of surrounding glaciers revealed that only surge‐type glaciers in their quiescent phase had proglacial naled assemblages, although these lacked incorporated debris. This indicates that surge‐type glaciers have a significant impact on the occurrence of naledi primarily because their subglacial thermal conditions and water storage capacity allow significant winter runoff implying high hydraulic pressure on proglacial outwash plains. Copyright © 2005 John Wiley &amp; Sons, Ltd.</abstract><cop>Chichester, UK</cop><pub>John Wiley &amp; Sons, Ltd</pub><doi>10.1002/ppp.533</doi><tpages>7</tpages></addata></record>
fulltext fulltext
identifier ISSN: 1045-6740
ispartof Permafrost and periglacial processes, 2005-10, Vol.16 (4), p.319-325
issn 1045-6740
1099-1530
language eng
recordid cdi_proquest_miscellaneous_17217008
source Wiley
subjects Bgi / Prodig
Greenland
Hydrometeorology
naled
Nivology. Glaciology
Physical geography
surge-type glaciers
title Observations of debris-rich naled associated with a major glacier surge event, Disko Island, West Greenland
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-07T21%3A40%3A22IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Observations%20of%20debris-rich%20naled%20associated%20with%20a%20major%20glacier%20surge%20event,%20Disko%20Island,%20West%20Greenland&rft.jtitle=Permafrost%20and%20periglacial%20processes&rft.au=Yde,%20Jacob%20Clement&rft.date=2005-10&rft.volume=16&rft.issue=4&rft.spage=319&rft.epage=325&rft.pages=319-325&rft.issn=1045-6740&rft.eissn=1099-1530&rft.coden=PEPPED&rft_id=info:doi/10.1002/ppp.533&rft_dat=%3Cproquest_cross%3E17217008%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-a3833-63b4b37e2e6f3678f52e3157dbd9a608ab857bbba0c28ac1231afdb340d181cc3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=17217008&rft_id=info:pmid/&rfr_iscdi=true