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The concept of cryo-conditioning in landscape evolution

Published online by Cambridge University Press:  20 January 2017

Ivar Berthling  and
Bernd Etzelmüller
Ivar Berthling*
Affiliation:
Department of Geography, Norwegian University of Science and Technology, Norway
Bernd Etzelmüller
Affiliation:
Department of Geosciences, University of Oslo, Norway
*
⁎Corresponding author. Department of Geography, NTNU, N-7491, Norway. Fax: +47 73591878.
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Abstract

Recent accounts suggest that periglacial processes are unimportant for large-scale landscape evolution and that true large-scale periglacial landscapes are rare or non-existent. The lack of a large-scale topographical fingerprint due to periglacial processes may be considered of little relevance, as linear process–landscape development relationships rarely can be substantiated. Instead, periglacial landscapes may be classified in terms of specific landform associations. We propose “cryo-conditioning”, defined as the interaction of cryotic surface and subsurface thermal regimes and geomorphic processes, as an overarching concept linking landform and landscape evolution in cold regions. By focusing on the controls on processes, this concept circumvents scaling problems in interpreting long-term landscape evolution derived from short-term processes. It also contributes to an unambiguous conceptualization of periglacial geomorphology. We propose that the development of several key elements in the Norwegian geomorphic landscape can be explained in terms of cryo-conditioning.

Keywords

PeriglacialPeriglacial geomorphologyLandscapeLandscape evolutionCryo-conditioningScaleCryo-geomorphology
Type
Research Article
Information
Quaternary Research , Volume 75 , Issue 2 , March 2011 , pp. 378 - 384
Copyright
University of Washington

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References

Ahnert, F. Equilibrium, scale and inheritance in geomorphology. Geomorphology 11, (1994). 125–140.Google Scholar
Ahnert, F. Einführung in die Geomorphologie. (1996). Stuttgart, UTB. 440 pp.Google Scholar
Anderson, R.S. Near-surface thermal profiles in alpine bedrock: implications for the frost weathering of rock. Arctic and Alpine Research 30, (1998). 362–372.Google Scholar
André, M.F. Do periglacial landscapes evolve under periglacial conditions?. Geomorphology 52, (2003). 149–164.CrossRefGoogle Scholar
Barsch, D. Rockglaciers. (1996). Springer, Berlin. 331 pp.Google Scholar
Boogart, P.W., Tucker, G.E., and De Vries, J.J. Channel network morphology and sediment dynamics under alternating periglacial and temperatue regimes: a numerical sumulation study. Geomorphology 54, (2003). 257–277.Google Scholar
Church, M. Space, time and the mountain — how do we order what we see?. Rhoads, B.L., and Thorn, C.E. The Scientific Nature of Geomorphology. (1996). John Wiley and Sons, Chichester. 147–170.Google Scholar
Davies, M.C.R., Hamza, O., and Harris, C. The effect of rise in mean annual temperature on the stability of rock slopes containing ice-filled discontinuities. Permafrost and Periglacial Processes 12, (2001). 137–144.CrossRefGoogle Scholar
Dixon, J. Scale in periglacial geomorphology. Geomorphologie-Relief Processus Environnement no. 3, (2006). 175–185.Google Scholar
Etzelmüller, B. Quantification of thermo-erosion in pro-glacial areas — examples from Spitsbergen. Zeitschrift für Geomorphologie, NF 44, (2000). 343–361.Google Scholar
Etzelmüller, B., Berthling, I., and Sollid, J.L. Aspects and concepts on the geomorphological significance of Holocene permafrost in southern Norway. Geomorphology 52, (2003). 87–104.Google Scholar
Etzelmüller, B., and Frauenfelder, R. Factors controlling the distribution of mountain permafrost in the Northern Hemisphere and their influence on sediment transfer. Arctic Antarctic and Alpine Research 41, (2009). 48–58.Google Scholar
Etzelmüller, B., and Hagen, J.O. Glacier-permafrost interaction in Arctic and alpine mountain environments with examples from southern Norway and Svalbard. Harris, C., and Murton, J. Cryosperic Systems. Glaciers and Permafrost, Geological Society of London Special Publications 242, (2005). 11–27.Google Scholar
Etzelmüller, B., Hagen, J.O., Vatne, G., Ødegård, R., and Sollid, J.L. Glacier debris accumulation and sediment deformation influenced by permafrost — examples from Spitsbergen, Svalbard. Annals of Glaciology 22, (1996). 53–62.Google Scholar
Etzelmüller, B., Romstad, B., and Fjellanger, J. Automatic regional classification of topography in Norway. Norwegian Journal of Geology 87, (2007). 167–180.Google Scholar
Fitzsimons, S., Webb, N., Mager, S., MacDonell, S., Lorrain, R., and Samyn, D. Mechanisms of basal ice formation in polar glaciers: an evaluation of the apron entrainment model. Journal of Geophysical Research-Earth Surface 113, (2008). F02010 Google Scholar
Fjellanger, J., Sørbel, L., Linge, H., Brook, E.J., Raisbeck, G.M., and Yiou, F. Glacial survival of blockfields on the Varanger Peninsula, northern Norway. Geomorphology 82, (2006). 255–272.Google Scholar
Fortier, R., and Aubé-Maurice, B. Fast permafrost degradation near Umiujaq in Nunavik (Canada) since 1957 assessed from time-lapse aerial and satellite photographs. Proceedings of the Ninth International Conference on Permafrost, Institute of Northern Engineering, University of Alaska Fairbanks 1, (2008). 457–462.Google Scholar
French, H. Introduction. Evans, D.J.A. Perglacial geomorphology. Critical Concepts in Geography, Routledge UK 5, (2004). 1–40.Google Scholar
French, H. The Periglacial Environment. (2007). John Wiley and Sons, 458 pp.Google Scholar
French, H., and Thorn, C.E. The changing nature of periglacial geomorphology. Geomorphologie-Relief Processus Environnement nº3, (2006). 165–173.Google Scholar
Gjessing, J. Norway's paleic surface. Norsk Geografisk Tidsskrift — Norwegian Journal of Gegraphy 21, (1967). 69–132.Google Scholar
Goodfellow, B.W. Relict non-glacial surfaces in formerly glaciated landscapes. Earth-Science Reviews 80, (2007). 47–73.Google Scholar
Gruber, S., and Haeberli, W. Permafrost in steep bedrock slopes and its temperature-related destabilization following climate change. Journal of Geophysical Research-Earth Surface 112, (2007). F020S18 Google Scholar
Gruber, S., and Hoelzle, M. The cooling effect of coarse blocks revisited: a modeling study of a purely conductive mechanism. Proceedings of the Ninth International Conference on Permafrost, Institute of Northern Engineering, University of Alaska Fairbanks 1, (2008). 557–561.Google Scholar
Haeberli, W. Investigating glacier–permafrost relationships in high-mountain areas: historical background, selected examples and research needs. Harris, C., and Murton, J. Cryosperic Systems. Glaciers and Permafrost, Geological Society of London Special Publications 242, (2005). 29–37.Google Scholar
Hales, T.C., and Roering, J.J. Climatic controls on frost cracking and implications for the evolution of bedrock landscapes. Journal of Geophysical Research-Earth Surface 112, (2007). F02033 Google Scholar
Hall, K., and André, M.F. New insights into rock weathering from high-frequency rock temperature data: an Antarctic study of weathering by thermal stress. Geomorphology 41, (2001). 23–35.Google Scholar
Hall, K., Thorn, C.E., Matsuoka, N., and Prick, A. Weathering in cold regions: some thoughts and perspectives. Progress In Physical Geography 26, (2002). 577–603.CrossRefGoogle Scholar
Hallet, B. The breakdown of rock due to freezing: a theoretical model. Proceedings of the 4th International Conference on Permafrost, Fairbanks, Alaska (1983). National Academy Press, Washington D.C. 433–438.Google Scholar
Hallet, B., Walder, J.S., and Stubbs, C.W. Weathering by segregation ice growth in microcracks at sustained subzero temperatures: verification from an experimental study using acoustic emissions. Permafrost and Periglacial Processes 2, (1991). 283–300.Google Scholar
Hanson, S., and Hoelzle, M. The thermal regime of the active layer at the Murtel rock glacier based on data from 2002. Permafrost and Periglacial Processes 15, (2004). 273–282.Google Scholar
Harris, C., and Lewkowicz, A.G. An analysis of the stability of thawing slopes, Ellesmere Island, Nunavut, Canada. Canadian Geotechnical Journal 37, (2000). 449–462.Google Scholar
Harrison, S. On reductionism and emergence in geomorphology. Transactions of the Institute of British Geographers 26, (2001). 327–339.CrossRefGoogle Scholar
Haschenburger, J.K., and Souch, C. Contributions to the understanding of geomorphic loandscapes published in the Annals. Annals of the Association of American Geographers 94, (2004). 771–793.Google Scholar
Hättestrand, C. Boulder depressions in central Sweden — remnants of a pre-late Weichselian landscape?. Geografiska Annaler A76, (1994). 153–160.Google Scholar
Heggem, E.S.F., Juliussen, H., and Etzelmüller, B. The permafrost distribution in central-eastern Norway. Norsk Geografisk Tidsskrift — Norwegian Journal of Geography 59, (2005). 94–108.Google Scholar
Heimsath, A.M., and McGlynn, R. Quantifying periglacial erosion in the Nepal high Himalaya. Geomorphology 97, (2008). 5–23.Google Scholar
Isaksen, K., Hauck, C., Gudevang, E., Ødegård, R.S., and Sollid, J.L. Mountain permafrost distribution in Dovrefjell and Jotunheimen, southern Norway, based on BTS and DC resistivity tomography data. Norsk Geografisk Tidsskrift — Norwegian Journal of Geography 56, (2002). 122–136.Google Scholar
Isaksen, K., Holmlund, P., Sollid, J.L., and Harris, C. Three deep alpine-permafrost boreholes in Svalbard and Scandinavia. Permafrost and Periglacial Processes 12, (2001). 13–25.Google Scholar
Juliussen, H., and Humlum, O. Towards a TTOP ground temperature model for mountainous terrain in central-eastern Norway. Permafrost and Periglacial Processes 18, (2007). 161–184.Google Scholar
Juliussen, H., and Humlum, O. Preservation of block fields beneath Pleistocene ice sheets on Sølen og Elgåhogna, south-eastern Norway. Zeitschrift für Geomorphologie Suppl. Bd. 51 (2007). 113–138.Google Scholar
Juliussen, H., and Humlum, O. Thermal regime of openwork block fields on the mountains Elgåhogna and Sølen, central-eastern Norway. Permafrost and Periglacial Processes 19, (2008). 1–18.Google Scholar
King, E.C., Smith, A.M., Murray, T., and Stuart, G.W. Glacier-bed characteristics of midtre Lovenbreen, Svalbard, from high-resolution seismic and radar surveying. Journal of Glaciology 54, (2008). 145–156.Google Scholar
Kleman, J., and Glasser, N.F. The subglacial thermal organisation (STO) of ice sheets. Quaternary Science Reviews 26, (2007). 585–597.Google Scholar
Kleman, J., and Stroeven, A.P. Preglacial surface remnants and Quaternery glacial regimes in northwestern Sweden. Geomorphology 19, (1997). 35–54.CrossRefGoogle Scholar
Larsson, S. Geomorphological effects on the slopes of Longyear Valley, Spitsbergen, after a heavy rainstorm in July 1972. Geografiska Annaler A64, (1982). 105–125.Google Scholar
Lewkowicz, A.G., and Harris, C. Morphology and geotechnique of active-layer detachment failures in discontinuous and continuous permafrost, northern Canada. Geomorphology 69, (2005). 275–297.Google Scholar
Lidmar-Bergstrom, K., Ollier, C.D., and Sulebak, J.R. Landforms and uplift history of southern Norway. Global and Planetery Change 24, (2000). 211–231.Google Scholar
Luoto, M., and Hjort, J. Generalized linear modelling in periglacial studies: terrain parameters and patterned ground. Permafrost and Periglacial Processes 15, (2004). 327–338.Google Scholar
Matsuoka, N. Frost weathering and rockwall erosion in the southeastern Swiss Alps: long-term (1994–2006) observations. Geomorphology 99, (2008). 353–368.Google Scholar
Nesje, A., and Whillans, I.M. Erosion of Sognefjord, Norway. Geomorphology 9, (1994). 33–45.Google Scholar
Ødegård, R., Etzelmüller, B., Vatne, G., Sollid, J.L. Slaymaker, O. Near-surface spring temperatures in an Arctic coastal rock cliff: possible implications for rock breakdown. Steepland Geomorphology (1995). John Wiley and Sons, Chichester. 89–102.Google Scholar
Ødegård, R.S., Sollid, J.L., and Liestøl, O. Ground temperature measurements in mountain permafrost, Jotunheimen, southern Norway. Permafrost and Periglacial Processes 3, (1992). 231–234.Google Scholar
Østrem, G Ice-cored moraines in Scandinavia. Geografiska Annaler A 46, (1964). 282–337.Google Scholar
Phillips, J.D. Evolutionary geomorphology: thresholds and nonlinearity in landform response to environmental change. Hydrology and Earth System Sciences 10, (2006). 731–742.Google Scholar
Pissart, A., (2005). Book Review: Geomorphology. Critical concepts in geography. Series editor: David, J. A. Evans Volume V, : Periglacial Geomorphology. Edited by Hugh, M. French. Rouledge, Taylor and Francis Group, London and New York., (2005). 641 pp. Volume V, (ISBN 0-415-27613-6). Permafrost and Periglacial Processes 16, 223–226.Google Scholar
Pomeroy, J.W., Gray, D.M., Brown, T., Hedstrom, N.R., Quinton, W.L., Granger, R.J., and Carey, S.K. The cold regions hydrological model: a platform for basing process representation and model structure on physical evidence. Hydrological Processes 21, (2007). 2650–2667.Google Scholar
Rea, B.R., Whalley, W.B., Rainey, M.M., and Gordon, J.E. Blockfields, old or new? Evidence and implications from some plateaus in northern Norway. Geomorphology 15, (1996). 109–121.Google Scholar
Reusch, H. Nogle bidrag til forstaaelsen af, hvorledes Norges dal og fjelde er blevne til. N.G.U Årbok. (1900). 125–263.Google Scholar
Reusser, L.J., Bierman, P.R., Pavich, M.J., Zen, E.A., Larsen, J., and Finkel, R. Rapid late Pleistocene incision of Atlantic passive-margin river gorges. Science 305, (2004). 499–502.Google Scholar
Rhoads, B.L., and Thorn, C.E. Toward a philosophy of geomorphology. Rhoads, B.L., and Thorn, C.E. The Scientific Nature of Geomorphology. (1996). John Wiley and Sons, Chichester. 115–143.Google Scholar
Roaldset, E., Pettersen, E., Longva, O., and Mangerud, J. Remnants of preglacial weathering in western Norway. Norwegian Journal of Geology 62, (1982). 169–178.Google Scholar
Rossi, A.P., van Gasselt, S., Pondrelli, M., Zegers, T., Hauber, E., and Neukum, G. Periglacial Landscape Evolution at Lower Mid-Latitudes on Mars: The Thaumasia Highlands. Proceedings of the Ninth International Conference on Permafrost 2, (2008). Institute of Northern Engineering, University of Alaska Fairbanks, 1531–1536.Google Scholar
Schomacker, A. What controls dead-ice melting under different climate conditions? A discussion. Earth-Science Reviews 90, (2008). 103–113.Google Scholar
Schomacker, A., and Kjær, K.H. Quantification of dead-ice melting in ice-cored moraines at the high-Arctic glacier Holmströmbreen, Svalbard. Boreas 37, (2008). 211–225.CrossRefGoogle Scholar
Shur, Y., Hinkel, K.M., and Nelson, F.E. The transient layer: implications for geocryology and climate-change science. Permafrost and Periglacial Processes 16, (2005). 5–17.Google Scholar
Sidorchuk, A.Y., Panin, A.V., and Borisova, O.K. Climate-induced changes in surface runoff on the North-Eurasian plains during the late glacial and Holocene. Water Resources 35, (2008). 386–396.Google Scholar
Stroeven, A.P., Fabel, D., Hattestrand, C., and Harbor, J. A relict landscape in the centre of Fennoscandian glaciation: cosmogenic radionuclide evidence of tors preserved through multiple glacial cycles. Geomorphology 44, (2002). 145–154.CrossRefGoogle Scholar
Thorn, C.E. Periglacial geomorphology: what, where, when. Dixon, J.C., and Abrahams, A.D. Periglacial Geomorphology. (1992). John Wiley and Sons, New York. 1–30.Google Scholar
von Lozinski, W. Die Periglaziale Fazies der Mechanischen Verwitterung. Comptes Rendus, XI Congres Internationale Geologie, Stockholm 1910 (1912). 1039–1053.Google Scholar
Woo, M.K., Kane, D.L., Carey, S.K., and Yang, D.Q. Progress in permafrost hydrology in the new millennium. Permafrost and Periglacial Processes 19, (2008). 237–254.Google Scholar
Yumoto, M., Ogata, T., Matsuoka, N., and Matsumoto, E. Riverbank freeze–thaw erosion along a small mountain stream, Nikko volcanic area, central Japan. Permafrost and Periglacial Processes 17, (2006). 325–339.Google Scholar
Zhang, P.Z., Molnar, P., and Downs, W.R. Increased sedimentation rates and grain sizes 2–4 Myr ago due to the influence of climate change on erosion rates. Nature 410, (2001). 891–897.Google Scholar