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Controls on the altitude of Scandinavian cirques: What do they tell us about palaeoclimate?

Oien, Rachel P.; Barr, Iestyn D.; Spagnolo, Matteo; Bingham, Robert G.; Rea, Brice R.; Jansen, John

Authors

Iestyn D. Barr

Matteo Spagnolo

Robert G. Bingham

Brice R. Rea

John Jansen



Abstract

Cirques are glacially eroded, bowl-shaped depressions, characterised by steep headwalls and flat or overdeepened floors. Given their association with past glaciers, cirques are sometimes used as proxies for palaeoclimate. However, cirques are shaped over multiple glacial cycles, and their usefulness as palaeoclimate indicators therefore remains open to question. In this paper, we map 3984 glacier-free cirques across the Scandinavian Peninsula and analyse variations in cirque floor altitude (CFA). We explore the relationships between CFAs and cirque aspect, latitude, longitude, and distance to the coast. We test the validity of using CFAs as indicators of palaeoclimate through comparison with the equilibrium-line altitudes (ELAs) of 513 modern cirque glaciers. Results indicate that both CFAs and modern cirque-glacier ELAs decrease with latitude and vary with aspect, being generally lowest on east-facing slopes. However, the clearest and strongest trend in both CFAs and modern cirque glacier ELAs is an increase in elevation with distance from the modern coast (i.e., distance ‘inland’). This likely indicates that similar climatic gradients, particularly an inland reduction in precipitation, acted to regulate former sites of glacier initiation (reflected by CFAs) and modern glacier ELAs. This would imply that CFAs are a useful proxy for palaeoclimate. However, we note that both CFAs and modern ELAs reflect the general topography of this region (with increasing elevations moving inland), and the glacial history of the area (indirectly linked to palaeoclimate) may have played a role in regulating where cirques have formed. For these reasons, we suggest that palaeoclimatic interpretations derived from CFAs should be treated with caution.

Citation

Oien, R. P., Barr, I. D., Spagnolo, M., Bingham, R. G., Rea, B. R., & Jansen, J. (2022). Controls on the altitude of Scandinavian cirques: What do they tell us about palaeoclimate?. Palaeogeography, Palaeoclimatology, Palaeoecology, 600, 111062. https://doi.org/10.1016/j.palaeo.2022.111062

Journal Article Type Article
Acceptance Date May 17, 2022
Online Publication Date May 26, 2022
Publication Date Aug 15, 2022
Deposit Date Mar 22, 2024
Journal Palaeogeography, Palaeoclimatology, Palaeoecology
Print ISSN 0031-0182
Electronic ISSN 1872-616X
Publisher Elsevier
Peer Reviewed Peer Reviewed
Volume 600
Pages 111062
DOI https://doi.org/10.1016/j.palaeo.2022.111062
Keywords ELA, Cirques, Palaeoclimate, Climate, Glacier
Public URL https://durham-repository.worktribe.com/output/1874800