Recent, very rapid retreat of a temperate glacier in SE Iceland

Bradwell, Tom; Sigurđsson, Oddur; Everest, Jez. 2013 Recent, very rapid retreat of a temperate glacier in SE Iceland. Boreas, 42 (4). 959-973. 10.1111/bor.12014

Before downloading, please read NORA policies.

Preview

Text bor12014.pdf Available under License Creative Commons Attribution. Download (3MB) | Preview

Abstract/Summary

Iceland's glaciers are particularly sensitive to climate change, and their margins respond to trends in air temperature. Most Icelandic glaciers have been in retreat since c. 1990, and almost all since 1995. Using ice-front measurements, photographic and geomorphological evidence, we examined the record of ice-front fluctuations of Virkisjökull–Falljökull, a steep high-mass-turnover outlet glacier in maritime SE Iceland, in order to place recent changes in a longer-term (80-year) context. Detailed geomorphological mapping identifies two suites of annual push moraines: one suite formed between c. 1935 and 1945, supported by lichenometric dating; the other between 1990 and 2004. Using moraine spacing as a proxy for ice-front retreat rates, we show that average retreat rates during the 1930s and 1940s (28 m a−1) were twice as high as during the period from 1990 to 2004 (14 m a−1). Furthermore, we show that both suites of annual moraines are associated with above-average summer temperatures. Since 2005, however, retreat rates have increased considerably – averaging 35 m a−1 – with the last 5 years representing the greatest amount of ice-front retreat (∼190 m) in any 5-year period since measurements began in 1932. We propose that this recent, rapid, ice-front retreat and thinning in a decade of unusually warm summers has resulted in a glaciological threshold being breached, with subsequent large-scale stagnation of the glacier terminus (i.e. no forward movement) and the cessation of annual push-moraine formation. Breaching this threshold has, we suggest, caused further very rapid non-uniform retreat and downwasting since 2005 via a system feedback between surface melting, glacier thinning, decreased driving stress and decreased forward motion.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1111/bor.12014
ISSN:	03009483
Additional Information. Not used in RCUK Gateway to Research.:	Article published Open Access using Creative Commons Attribution Licence
Date made live:	22 Apr 2013 10:32 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/501411

Actions (login required)

View Item

Document Downloads

More statistics for this item...