Numerical simulations of drumlin formation

We summarize the present form of the instability theory for drumlin formation, which describes the coupled subglacial flow of ice, water and sediment. This model has evolved over the last 20 years, and is now at the point where it can predict instabilities corresponding to ribbed moraine, drumlins a...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Proceedings of the Royal Society. A, Mathematical, physical, and engineering sciences Mathematical, physical, and engineering sciences, 2017-08, Vol.473 (2204), p.1-19
Hauptverfasser: Fannon, J. S., Fowler, A. C., Moyles, I. R.
Format: Artikel
Sprache:eng
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 19
container_issue 2204
container_start_page 1
container_title Proceedings of the Royal Society. A, Mathematical, physical, and engineering sciences
container_volume 473
creator Fannon, J. S.
Fowler, A. C.
Moyles, I. R.
description We summarize the present form of the instability theory for drumlin formation, which describes the coupled subglacial flow of ice, water and sediment. This model has evolved over the last 20 years, and is now at the point where it can predict instabilities corresponding to ribbed moraine, drumlins and mega-scale glacial lineations, but efforts to provide numerical solutions of the model have been limited. The present summary adds some slight nuances to previously published versions of the theory, notably concerning the constitutive description of the subglacial water film and its flow. A new numerical method is devised to solve the model, and we show that it can be solved for realistic values of most of the parameters, with the exception of that corresponding to the water film thickness. We show that evolved bedforms can be three-dimensional and of the correct sizes, and we explore to some extent the variation of the solutions with the model's parameters.
format Article
fullrecord <record><control><sourceid>jstor</sourceid><recordid>TN_cdi_jstor_primary_44683259</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><jstor_id>44683259</jstor_id><sourcerecordid>44683259</sourcerecordid><originalsourceid>FETCH-jstor_primary_446832593</originalsourceid><addsrcrecordid>eNpjYeA0NDYz0TU1MDLkYOAqLs4yMDCwNLUw52TQ8ivNTS3KTE7MUSjOzC3NSSzJzM8rVshPU0gpKs3NycxTSMsvygWL8jCwpiXmFKfyQmluBlk31xBnD92s4pL8oviCoszcxKLKeBMTMwtjI1NLY0LyAKg3LKE</addsrcrecordid><sourcetype>Publisher</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>Numerical simulations of drumlin formation</title><source>JSTOR Mathematics &amp; Statistics</source><source>JSTOR Archive Collection A-Z Listing</source><source>Alma/SFX Local Collection</source><creator>Fannon, J. S. ; Fowler, A. C. ; Moyles, I. R.</creator><creatorcontrib>Fannon, J. S. ; Fowler, A. C. ; Moyles, I. R.</creatorcontrib><description>We summarize the present form of the instability theory for drumlin formation, which describes the coupled subglacial flow of ice, water and sediment. This model has evolved over the last 20 years, and is now at the point where it can predict instabilities corresponding to ribbed moraine, drumlins and mega-scale glacial lineations, but efforts to provide numerical solutions of the model have been limited. The present summary adds some slight nuances to previously published versions of the theory, notably concerning the constitutive description of the subglacial water film and its flow. A new numerical method is devised to solve the model, and we show that it can be solved for realistic values of most of the parameters, with the exception of that corresponding to the water film thickness. We show that evolved bedforms can be three-dimensional and of the correct sizes, and we explore to some extent the variation of the solutions with the model's parameters.</description><identifier>ISSN: 1364-5021</identifier><language>eng</language><publisher>THE ROYAL SOCIETY</publisher><ispartof>Proceedings of the Royal Society. A, Mathematical, physical, and engineering sciences, 2017-08, Vol.473 (2204), p.1-19</ispartof><rights>The Royal Society, 2017</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/44683259$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/44683259$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,803,832,58017,58021,58250,58254</link.rule.ids></links><search><creatorcontrib>Fannon, J. S.</creatorcontrib><creatorcontrib>Fowler, A. C.</creatorcontrib><creatorcontrib>Moyles, I. R.</creatorcontrib><title>Numerical simulations of drumlin formation</title><title>Proceedings of the Royal Society. A, Mathematical, physical, and engineering sciences</title><description>We summarize the present form of the instability theory for drumlin formation, which describes the coupled subglacial flow of ice, water and sediment. This model has evolved over the last 20 years, and is now at the point where it can predict instabilities corresponding to ribbed moraine, drumlins and mega-scale glacial lineations, but efforts to provide numerical solutions of the model have been limited. The present summary adds some slight nuances to previously published versions of the theory, notably concerning the constitutive description of the subglacial water film and its flow. A new numerical method is devised to solve the model, and we show that it can be solved for realistic values of most of the parameters, with the exception of that corresponding to the water film thickness. We show that evolved bedforms can be three-dimensional and of the correct sizes, and we explore to some extent the variation of the solutions with the model's parameters.</description><issn>1364-5021</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid/><recordid>eNpjYeA0NDYz0TU1MDLkYOAqLs4yMDCwNLUw52TQ8ivNTS3KTE7MUSjOzC3NSSzJzM8rVshPU0gpKs3NycxTSMsvygWL8jCwpiXmFKfyQmluBlk31xBnD92s4pL8oviCoszcxKLKeBMTMwtjI1NLY0LyAKg3LKE</recordid><startdate>20170801</startdate><enddate>20170801</enddate><creator>Fannon, J. S.</creator><creator>Fowler, A. C.</creator><creator>Moyles, I. R.</creator><general>THE ROYAL SOCIETY</general><scope/></search><sort><creationdate>20170801</creationdate><title>Numerical simulations of drumlin formation</title><author>Fannon, J. S. ; Fowler, A. C. ; Moyles, I. R.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-jstor_primary_446832593</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Fannon, J. S.</creatorcontrib><creatorcontrib>Fowler, A. C.</creatorcontrib><creatorcontrib>Moyles, I. R.</creatorcontrib><jtitle>Proceedings of the Royal Society. A, Mathematical, physical, and engineering sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Fannon, J. S.</au><au>Fowler, A. C.</au><au>Moyles, I. R.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Numerical simulations of drumlin formation</atitle><jtitle>Proceedings of the Royal Society. A, Mathematical, physical, and engineering sciences</jtitle><date>2017-08-01</date><risdate>2017</risdate><volume>473</volume><issue>2204</issue><spage>1</spage><epage>19</epage><pages>1-19</pages><issn>1364-5021</issn><abstract>We summarize the present form of the instability theory for drumlin formation, which describes the coupled subglacial flow of ice, water and sediment. This model has evolved over the last 20 years, and is now at the point where it can predict instabilities corresponding to ribbed moraine, drumlins and mega-scale glacial lineations, but efforts to provide numerical solutions of the model have been limited. The present summary adds some slight nuances to previously published versions of the theory, notably concerning the constitutive description of the subglacial water film and its flow. A new numerical method is devised to solve the model, and we show that it can be solved for realistic values of most of the parameters, with the exception of that corresponding to the water film thickness. We show that evolved bedforms can be three-dimensional and of the correct sizes, and we explore to some extent the variation of the solutions with the model's parameters.</abstract><pub>THE ROYAL SOCIETY</pub></addata></record>
fulltext fulltext
identifier ISSN: 1364-5021
ispartof Proceedings of the Royal Society. A, Mathematical, physical, and engineering sciences, 2017-08, Vol.473 (2204), p.1-19
issn 1364-5021
language eng
recordid cdi_jstor_primary_44683259
source JSTOR Mathematics & Statistics; JSTOR Archive Collection A-Z Listing; Alma/SFX Local Collection
title Numerical simulations of drumlin formation
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-06T17%3A27%3A23IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-jstor&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Numerical%20simulations%20of%20drumlin%20formation&rft.jtitle=Proceedings%20of%20the%20Royal%20Society.%20A,%20Mathematical,%20physical,%20and%20engineering%20sciences&rft.au=Fannon,%20J.%20S.&rft.date=2017-08-01&rft.volume=473&rft.issue=2204&rft.spage=1&rft.epage=19&rft.pages=1-19&rft.issn=1364-5021&rft_id=info:doi/&rft_dat=%3Cjstor%3E44683259%3C/jstor%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rft_jstor_id=44683259&rfr_iscdi=true