Document Type
Article
Publication Date
2015
Keywords
glacier flow, glaciological instruments and methods, ice/ocean interactions, remote sensing
Digital Object Identifier (DOI)
https://doi.org/10.3189/2015JoG14J099
Abstract
Terrestrial radar interferometry (TRI) is a new technique for studying ice motion and volume change of glaciers. TRI is especially useful for temporally and spatially dense measurements of highly dynamic glacial termini. We conducted a TRI survey of Breiðamerkurjökull, a marine-terminating glacier in Iceland, imaging its terminus near the end of the melt season in 2011, 2012 and 2013. The ice velocities were as high as 5 m d−1, with the fastest velocities near the calving front. Retreat of the glacier over the 3 year observation period was accompanied by strong embayment formation. Iceberg tracking with the radar shows high current velocities near the embayment, probably indicating strong meltwater outflow and mixing with relatively warm lagoon water.
Rights Information
This work is licensed under a Creative Commons Attribution 4.0 License.
Was this content written or created while at USF?
Yes
Citation / Publisher Attribution
Journal of Glaciology, v. 61, issue 225, p. 42-54
© Authors retain copyright
Scholar Commons Citation
Voytenko, Denis; Dixon, Timothy H.; Howat, Ian M.; Gourmelen, Noel; Lembke, Chad; Werner, Charles L.; De La Peña, Santiago; and Oddsson, Björn, "Multi-Year Observations of Breiðamerkurjökull, a Marine-Terminating Glacier in Southeastern Iceland, using Terrestrial Radar Interferometry" (2015). School of Geosciences Faculty and Staff Publications. 1533.
https://digitalcommons.usf.edu/geo_facpub/1533
