Skip to main content
Publications | Persons | Institutes | Projects
[ report an error in this record ]basket (0): add | show Print this page

The climate memory of an Arctic polythermal glacier
Delcourt, C.; van Liefferinge, B.; Nolan, M.; Pattyn, F. (2013). The climate memory of an Arctic polythermal glacier. J. Glaciol. 59(218): 1084-1092. dx.doi.org/10.3189/2013JoG12J109
In: Journal of Glaciology. International Glaciological Society: Cambridge. ISSN 0022-1430; e-ISSN 1727-5652, more
Peer reviewed article  

Available in  Authors 

Keyword
    Marine/Coastal

Authors  Top 
  • Delcourt, C., more
  • van Liefferinge, B., more
  • Nolan, M.
  • Pattyn, F., more

Abstract
    Knowledge of glacier equilibrium-line altitude (ELA) changes and trends in time is essential for future predictions of glacier volumes. We present a novel method for determining trends in ELA change at McCall Glacier, Alaska, USA, over the last 50 years, based on mapping of the cold temperate transition surface (CTS), marking the limit between cold and temperate ice of a polythermal glacier. Latent heat release from percolating meltwater and precipitation keeps the ice column temperate in the accumulation area. A change from accumulation to ablation zone reduces this heat release, leading locally to glacier ice cooling. By mapping the CTS along the whole glacier length using radio-echo sounding and employing a thermodynamic model, the timing of the cooling was determined, from which past ELAs were constructed. These are in accord with mass-balance measurements carried out on McCall Glacier since the 1950s. We show that with a warming climate, McCall Glacier tends to cool in a counter-intuitive way.

All data in the Integrated Marine Information System (IMIS) is subject to the VLIZ privacy policy Top | Authors