Climatic controls on the equilibrium-line altitudes of Scandinavian cirque glaciers

Rachel P. Oien* (Corresponding Author), Matteo Spagnolo, Brice R. Rea, Iestyn D. Barr, Robert G. Bingham

*Corresponding author for this work

Research output: Contribution to journalArticle

Abstract

The equilibrium-line altitudes (ELAs) of reconstructed palaeoglaciers have been widely used to assess palaeoclimatic conditions, yet this concept has rarely been tested using modern glaciers. To address this shortcoming, correlations between the ELAs of 513 modern cirque glaciers and presentday climatic and topographic variables across Scandinavia, as well as regional trends in ELA and climate, are analysed. ELAs are calculated using the Area-Altitude-Balance-Ratio method, with a ratio of 1.5 ± 0.4. Results indicate that glacier ELAs are strongly correlated with distance from the coast. This reflects the present-day precipitation pattern of the region (characterised by high precipitation near the sea) and demonstrates a climate dominated by a maritime-continental transition. Temperature explains differences in glacier ELA regional trends as well as ELA changes with latitude. Following standard meteorological convention, Scandinavia is divided into two macroclimate regions and analyses are run within the macro-regions as well as the complete dataset. The strength of correlations between ELA and precipitation increases when the study is divided into northern and southern macro-regions. These results test long held assumptions about relationships between climate and cirque glacier ELA, which is of particular relevance to palaeoclimatic studies based on the reconstruction of former cirque glaciers.
Original languageEnglish
Article number106986
Number of pages11
JournalGeomorphology
Volume352
Early online date12 Dec 2019
DOIs
Publication statusE-pub ahead of print - 12 Dec 2019

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cirque
equilibrium line
glacier
climate

Keywords

  • equilibrium -line altitude (ELA)
  • Scandinavian cirque glaciers
  • precipitation
  • temperature
  • GIS

Cite this

Climatic controls on the equilibrium-line altitudes of Scandinavian cirque glaciers. / Oien, Rachel P. (Corresponding Author); Spagnolo, Matteo; Rea, Brice R.; Barr, Iestyn D.; Bingham, Robert G.

In: Geomorphology, Vol. 352, 106986, 01.03.2020.

Research output: Contribution to journalArticle

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abstract = "The equilibrium-line altitudes (ELAs) of reconstructed palaeoglaciers have been widely used to assess palaeoclimatic conditions, yet this concept has rarely been tested using modern glaciers. To address this shortcoming, correlations between the ELAs of 513 modern cirque glaciers and presentday climatic and topographic variables across Scandinavia, as well as regional trends in ELA and climate, are analysed. ELAs are calculated using the Area-Altitude-Balance-Ratio method, with a ratio of 1.5 ± 0.4. Results indicate that glacier ELAs are strongly correlated with distance from the coast. This reflects the present-day precipitation pattern of the region (characterised by high precipitation near the sea) and demonstrates a climate dominated by a maritime-continental transition. Temperature explains differences in glacier ELA regional trends as well as ELA changes with latitude. Following standard meteorological convention, Scandinavia is divided into two macroclimate regions and analyses are run within the macro-regions as well as the complete dataset. The strength of correlations between ELA and precipitation increases when the study is divided into northern and southern macro-regions. These results test long held assumptions about relationships between climate and cirque glacier ELA, which is of particular relevance to palaeoclimatic studies based on the reconstruction of former cirque glaciers.",
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note = "Dr. Dmitri Mauquoy is acknowledged for his help with the statistical analyses. We would like to thank the Scottish Alliance for Geoscience, Environment and Society for the funding, RO’s PhD scholarship and continual contributions towards travel and training. We would also like to extend thanks to The North Theme, at the University Aberdeen for support to attend a summer school in palaeoclimatology. Two anonymous reviewers and the Editor are acknowledged for their constructive and insightful comments.",
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N2 - The equilibrium-line altitudes (ELAs) of reconstructed palaeoglaciers have been widely used to assess palaeoclimatic conditions, yet this concept has rarely been tested using modern glaciers. To address this shortcoming, correlations between the ELAs of 513 modern cirque glaciers and presentday climatic and topographic variables across Scandinavia, as well as regional trends in ELA and climate, are analysed. ELAs are calculated using the Area-Altitude-Balance-Ratio method, with a ratio of 1.5 ± 0.4. Results indicate that glacier ELAs are strongly correlated with distance from the coast. This reflects the present-day precipitation pattern of the region (characterised by high precipitation near the sea) and demonstrates a climate dominated by a maritime-continental transition. Temperature explains differences in glacier ELA regional trends as well as ELA changes with latitude. Following standard meteorological convention, Scandinavia is divided into two macroclimate regions and analyses are run within the macro-regions as well as the complete dataset. The strength of correlations between ELA and precipitation increases when the study is divided into northern and southern macro-regions. These results test long held assumptions about relationships between climate and cirque glacier ELA, which is of particular relevance to palaeoclimatic studies based on the reconstruction of former cirque glaciers.

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