Ice and Snow as Land-Forming Agents

Darrel A. Swift, Simon Cook, Tobias Heckmann, Jeffrey Moore, Isabelle Gärtner-Roer, Oliver Korup

Research output: Chapter in Book/Report/Conference proceedingChapter (peer-reviewed)

6 Citations (Scopus)

Abstract

Many high-latitude and high-altitude regions are covered by ice and snow for substantial parts of the year, and typically, the landscape of such regions bears the strong imprint of ice- and snow-related processes operating over Quaternary to modern timescales. Despite strong research interest in the nature, rate, and efficacy of cold-region geomorphic processes, most research has been devoted to glacier and permafrost phenomena, whereas comparably few studies have quantitatively addressed the role of snow as a land-forming agent. In this chapter, we review the current research on land-forming processes related to glacial erosion and deposition; permafrost and periglacial processes; and snow-related processes such as nivation, snow creep, and snow avalanching. Our objective is to highlight those questions that drive current research and those that seem sufficiently promising to further our understanding of geomorphic form and process in the cryosphere. We do so bearing in mind that such process knowledge is essential for successfully predicting form and process, and hence avoiding snow- and ice-related hazards. We discuss whether certain aspects concerning the role of ice and snow as land-forming agents may have been overrated or underrated, if not overlooked, in the context of comprehensive studies on landscape evolution in polar and high mountainous terrain. We conclude by outlining a number of recommendations for future research in the field.

Original languageEnglish
Title of host publicationSnow and Ice-Related Hazards, Risks, and Disasters
EditorsWilfried Haeberli, Colin Whiteman, J. F. Shroder Jr.
Place of PublicationAmsterdam
PublisherElsevier Inc.
Pages167-199
Number of pages33
ISBN (Electronic)9780123964731
ISBN (Print)9780123948496
DOIs
Publication statusPublished - 2015

Fingerprint

snow
ice
permafrost
nivation
periglacial process
cryosphere
glacial erosion
land forming
cold region
landscape evolution
creep
glacier
hazard
timescale

Keywords

  • Avalanche
  • Erosion
  • Geomorphology
  • Glacial
  • Ice
  • Periglacial
  • Permafrost
  • Sediment
  • Snow

Cite this

Swift, D. A., Cook, S., Heckmann, T., Moore, J., Gärtner-Roer, I., & Korup, O. (2015). Ice and Snow as Land-Forming Agents. In W. Haeberli, C. Whiteman, & J. F. Shroder Jr. (Eds.), Snow and Ice-Related Hazards, Risks, and Disasters (pp. 167-199). Amsterdam: Elsevier Inc.. https://doi.org/10.1016/B978-0-12-394849-6.00006-8
Swift, Darrel A. ; Cook, Simon ; Heckmann, Tobias ; Moore, Jeffrey ; Gärtner-Roer, Isabelle ; Korup, Oliver. / Ice and Snow as Land-Forming Agents. Snow and Ice-Related Hazards, Risks, and Disasters. editor / Wilfried Haeberli ; Colin Whiteman ; J. F. Shroder Jr. Amsterdam : Elsevier Inc., 2015. pp. 167-199
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Swift, DA, Cook, S, Heckmann, T, Moore, J, Gärtner-Roer, I & Korup, O 2015, Ice and Snow as Land-Forming Agents. in W Haeberli, C Whiteman & JF Shroder Jr. (eds), Snow and Ice-Related Hazards, Risks, and Disasters. Elsevier Inc., Amsterdam, pp. 167-199. https://doi.org/10.1016/B978-0-12-394849-6.00006-8

Ice and Snow as Land-Forming Agents. / Swift, Darrel A.; Cook, Simon; Heckmann, Tobias; Moore, Jeffrey; Gärtner-Roer, Isabelle; Korup, Oliver.

Snow and Ice-Related Hazards, Risks, and Disasters. ed. / Wilfried Haeberli; Colin Whiteman; J. F. Shroder Jr. Amsterdam : Elsevier Inc., 2015. p. 167-199.

Research output: Chapter in Book/Report/Conference proceedingChapter (peer-reviewed)

TY - CHAP

T1 - Ice and Snow as Land-Forming Agents

AU - Swift, Darrel A.

AU - Cook, Simon

AU - Heckmann, Tobias

AU - Moore, Jeffrey

AU - Gärtner-Roer, Isabelle

AU - Korup, Oliver

N1 - Copyright © 2015 Elsevier Inc. All rights reserved.

PY - 2015

Y1 - 2015

N2 - Many high-latitude and high-altitude regions are covered by ice and snow for substantial parts of the year, and typically, the landscape of such regions bears the strong imprint of ice- and snow-related processes operating over Quaternary to modern timescales. Despite strong research interest in the nature, rate, and efficacy of cold-region geomorphic processes, most research has been devoted to glacier and permafrost phenomena, whereas comparably few studies have quantitatively addressed the role of snow as a land-forming agent. In this chapter, we review the current research on land-forming processes related to glacial erosion and deposition; permafrost and periglacial processes; and snow-related processes such as nivation, snow creep, and snow avalanching. Our objective is to highlight those questions that drive current research and those that seem sufficiently promising to further our understanding of geomorphic form and process in the cryosphere. We do so bearing in mind that such process knowledge is essential for successfully predicting form and process, and hence avoiding snow- and ice-related hazards. We discuss whether certain aspects concerning the role of ice and snow as land-forming agents may have been overrated or underrated, if not overlooked, in the context of comprehensive studies on landscape evolution in polar and high mountainous terrain. We conclude by outlining a number of recommendations for future research in the field.

AB - Many high-latitude and high-altitude regions are covered by ice and snow for substantial parts of the year, and typically, the landscape of such regions bears the strong imprint of ice- and snow-related processes operating over Quaternary to modern timescales. Despite strong research interest in the nature, rate, and efficacy of cold-region geomorphic processes, most research has been devoted to glacier and permafrost phenomena, whereas comparably few studies have quantitatively addressed the role of snow as a land-forming agent. In this chapter, we review the current research on land-forming processes related to glacial erosion and deposition; permafrost and periglacial processes; and snow-related processes such as nivation, snow creep, and snow avalanching. Our objective is to highlight those questions that drive current research and those that seem sufficiently promising to further our understanding of geomorphic form and process in the cryosphere. We do so bearing in mind that such process knowledge is essential for successfully predicting form and process, and hence avoiding snow- and ice-related hazards. We discuss whether certain aspects concerning the role of ice and snow as land-forming agents may have been overrated or underrated, if not overlooked, in the context of comprehensive studies on landscape evolution in polar and high mountainous terrain. We conclude by outlining a number of recommendations for future research in the field.

KW - Avalanche

KW - Erosion

KW - Geomorphology

KW - Glacial

KW - Ice

KW - Periglacial

KW - Permafrost

KW - Sediment

KW - Snow

U2 - 10.1016/B978-0-12-394849-6.00006-8

DO - 10.1016/B978-0-12-394849-6.00006-8

M3 - Chapter (peer-reviewed)

AN - SCOPUS:84942155490

SN - 9780123948496

SP - 167

EP - 199

BT - Snow and Ice-Related Hazards, Risks, and Disasters

A2 - Haeberli, Wilfried

A2 - Whiteman, Colin

A2 - Shroder Jr., J. F.

PB - Elsevier Inc.

CY - Amsterdam

ER -

Swift DA, Cook S, Heckmann T, Moore J, Gärtner-Roer I, Korup O. Ice and Snow as Land-Forming Agents. In Haeberli W, Whiteman C, Shroder Jr. JF, editors, Snow and Ice-Related Hazards, Risks, and Disasters. Amsterdam: Elsevier Inc. 2015. p. 167-199 https://doi.org/10.1016/B978-0-12-394849-6.00006-8