Toggle Main Menu Toggle Search

Open Access padlockePrints

The Newcastle University research output collection, currently available on ePrints, will shortly be moving to a new open repository platform, Figshare. To prepare for the data migration we have paused adding new content to ePrints, and will resume once the new repository is launched. During this time you will continue to have access to ePrints (but no new content will appear). We will share updates here when available.

A multi-dimensional analysis of pro-glacial landscape change at Sólheimajökull, southern Iceland

Lookup NU author(s): Emeritus Professor Andrew Russell

Downloads

Full text for this publication is not currently held within this repository. Alternative links are provided below where available.


Abstract

Pro-glacial landscapes are some of the most active on Earth. Previous studies of pro-glacial landscape change have often been restricted to considering either sedimentological, geomorphological or topographic parameters in isolation and are often mono-dimensional. This study utilized field surveys and digital elevation model (DEM) analyses to quantify planform, elevation and volumetric pro-glacial landscape change at Sólheimajökull in southern Iceland for multiple time periods spanning from 1960 to 2010. As expected, the most intense geomorphological changes persistently occurred in the ice-proximal area. During 1960 to 1996 the pro-glacial river was relatively stable. However, after 2001 braiding intensity was higher, channel slope shallower and there was a shift from overall incision to aggradation. Attributing these pro-glacial river channel changes to the 1999 jökulhlaup is ambiguous because it coincided with a switch from a period of glacier advance to that of glacier retreat. Furthermore, glacier retreat (of ~40 m yr−1) coincided with ice-marginal lake development and these two factors have both altered the pro-glacial river channel head elevation. From 2001 to 2010 progressive increase in channel braiding and progressive downstream incision occurred; these together probably reflecting stream power due to increased glacier ablation and reduced sediment supply due to trapping of sediment by the developing ice-marginal lake. Overall, this study highlights rapid spatiotemporal pro-glacial landscape reactions to changes in glacial meltwater runoff regimes, glacier terminus position, sediment supply and episodic events such as jökuhlaups. Recognizing the interplay of these controlling factors on pro-glacial landscapes will be important for understanding the geological record and for landscape stability assessments.


Publication metadata

Author(s): Staines KEH, Carrivick JL, Tweed FS, Evans AJ, Russell AJ, Jóhannesson T, Roberts MJ

Publication type: Article

Publication status: Published

Journal: Earth Surface Processes and Landforms

Year: 2015

Volume: 4

Issue: 6

Pages: 809–822

Print publication date: 01/05/2015

Online publication date: 14/11/2014

Acceptance date: 09/10/2014

ISSN (print): 0197-9337

ISSN (electronic): 1096-9837

Publisher: John Wiley & Sons, Ltd.

URL: http://onlinelibrary.wiley.com/doi/10.1002/esp.3662/abstract

DOI: 10.1002/esp.3662


Altmetrics

Altmetrics provided by Altmetric


Share