Email this article Equilibrium Line Altitude on Bellingshausen Ice Dome, Antarctic
- Authors: Mavlyudov B.R.1
-
Affiliations:
- Institute of Geography RAS
- Issue: Vol 63, No 4 (2023)
- Pages: 540-552
- Section: Glaciers and ice sheets
- URL: https://journals.rcsi.science/2076-6734/article/view/162314
- DOI: https://doi.org/10.31857/S2076673423040117
- EDN: https://elibrary.ru/FQSJXK
- ID: 162314
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Abstract
Received June 9, 2023; revised September15, 2023; accepted October 2, 2023
We present an analysis of the equilibrium line altitude (ELA) on the Bellingshausen Ice Dome on King George Island (Waterloo), Antarctica, derived only from ground-based glaciological surveys for the period 2007–2012 and 2014–2023. A good relationship was found between ELA and mean summer air temperature (XII-II months) with a coefficient of determination of about 0.8. Assuming the stability of this relation in the past, the changes in the ELA during the entire period of observations at Bellingshausen weather station (from 1968) were reconstructed. Since negative ELA values were obtained for some years, which is physically impossible, they were artificially adjusted to sea level. A good correlation of air temperature between the Bellingshausen and Deception Island weather stations allowed extending the reconstruction of ELA for a longer period (from 1947).
By cleaning up the strong interannual fluctuations in ELA using five-year moving averages, two complete periods of ELA change (from minimum to minimum) were identified for approximately 20 years (1947–1968) and 45 years (1968–2013). From 2014 to present time, the third period has been continuing. At the apogee of each period, the ELA was higher than the Bellingshausen Ice Dome height, which indicates that in these years the ice dome completely lost accumulation area. For the Bellingshausen and Warsaw ice domes, a pattern of higher ELA position on the western and southern slopes compared to the eastern slopes was revealed, which is probably applicable to the entire King George Island.
Since the ELA variations on King George Island are generally synchronous with its variations on Livingston Island, the reconstructed ELA on the Bellingshausen Ice Dome can probably be useful for reconstructing the glaciation history of the South Shetland Islands.
About the authors
B. R. Mavlyudov
Institute of Geography RAS
Author for correspondence.
Email: bulatrm@bk.ru
Russia, Moscow
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