Historical ablation rates on south-east Greenland glaciers measured in the 1933 warm summer

Ice ablation rates measured on four glaciers in south-east Greenland in summer 1933 are recovered from an old field book of geologist K. Milthers. These unpublished ablation data are among the first measured in Greenland and were obtained during a warm period comparable to that of recent years. Abla...

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Bibliographic Details
Published in:Polar Research
Main Authors: Bent Hasholt, Dirk van As, Niels Tvis Knudsen
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 2016
Subjects:
geo
Online Access:https://doi.org/10.3402/polar.v35.28858
https://doaj.org/article/2c0337a81b4a474795a1a830ef6565d7
Description
Summary:Ice ablation rates measured on four glaciers in south-east Greenland in summer 1933 are recovered from an old field book of geologist K. Milthers. These unpublished ablation data are among the first measured in Greenland and were obtained during a warm period comparable to that of recent years. Ablation rates of up to 45 mm ice eq. d−1 were observed. Using the Tasiilaq meteorological record, we calculate degree-day factors of ca. 3–5 mm ice eq. d−1°C−1. Comparing these results with 1996–2012 observations at one of Milthers’ glaciers (Mittivakkat), we find that ablation rates and degree-day factors are significantly higher (61±50%) in recent years. We speculate this to be due to a reduction in surface albedo, and perhaps the retreat of the glaciers out of the cold maritime inversion layer. Our findings suggest that using a temperature-index method that assumes constant degree-day factors may produce inaccurate long-term ablation estimates for south-east Greenland glaciers, further emphasizing the value of the rare 1933 measurements for validation of ablation models.