Abstract
You have accessMoreSectionsView PDF ToolsAdd to favoritesDownload CitationsTrack Citations ShareShare onFacebookTwitterLinked InRedditEmail Cite this article Mantelli Elisa and Schoof Christian 2021Correction to ‘Ice sheet flow with thermally activated sliding. Part 2: the stability of subtemperate regions’Proc. R. Soc. A.4772021046320210463http://doi.org/10.1098/rspa.2021.0463SectionSupplemental MaterialYou have accessCorrectionCorrection to ‘Ice sheet flow with thermally activated sliding. Part 2: the stability of subtemperate regions’ Elisa Mantelli Elisa Mantelli http://orcid.org/0000-0001-5096-7998 Google Scholar Find this author on PubMed Search for more papers by this author and Christian Schoof Christian Schoof http://orcid.org/0000-0002-7532-2296 Google Scholar Find this author on PubMed Search for more papers by this author Elisa Mantelli Elisa Mantelli http://orcid.org/0000-0001-5096-7998 Google Scholar Find this author on PubMed Search for more papers by this author and Christian Schoof Christian Schoof http://orcid.org/0000-0002-7532-2296 Google Scholar Find this author on PubMed Search for more papers by this author Published:07 July 2021https://doi.org/10.1098/rspa.2021.0463This article corrects the followingResearch ArticleIce sheet flow with thermally activated sliding. Part 2: the stability of subtemperate regionshttps://doi.org/10.1098/rspa.2019.0411 E. Mantelli and C. Schoof volume 475issue 2231Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences20 November 2019Proc. R. Soc. A475, 20190411. (Published 20 November 2019) (doi:10.1098/rspa.2019.0411)Sections 3 and 4. The statement above equation (3.4) on page 12, namely that we assume ‘the distinguished limit δ ∼ ε1/2’ is incorrect. Instead, the boundary layer model equation (3.5a,b) assumes Peδ = 1, with Peδ = Pe δ2ε−1. Analogously, the model in §4a (equation (4.6a)), figures 4–7 as well as the formula (4.16), all assume Peδ = 1. A more general version of the model that treats Peδ as a distinguished limit can be found in the electronic supplementary material, §2.3. Previous Article VIEW FULL TEXT DOWNLOAD PDF FiguresRelatedReferencesDetailsRelated articlesIce sheet flow with thermally activated sliding. Part 2: the stability of subtemperate regions20 November 2019Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences This IssueJuly 2021Volume 477Issue 2251 Article InformationDOI:https://doi.org/10.1098/rspa.2021.0463Published by:Royal SocietyOnline ISSN:1471-2946History: Published online07/07/2021Published in print28/07/2021 License:© 2021 The Author(s)Published by the Royal Society. All rights reserved. Citations and impact Subjectsfluid mechanicsglaciology
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