Iceberg calving flux and mass balance of the Austfonna ice cap on Nordaustlandet, Svalbard

• Published in: Journal of Geophysical Research. F. Earth Surface 2008-09, Vol.113 (F3), p.n/a
• Main Authors: Dowdeswell, J. A., Benham, T. J., Strozzi, T., Hagen, J. O.
• Format: Article
• Language: English
• Subjects: Earth sciences; Earth, ocean, space; Exact sciences and technology; icebergs; mass balance; Svalbard
• ISSN: 0148-0227; 2156-2202
• DOI: 10.1029/2007JF000905

Satellite radar interferometry, 60 MHz airborne ice‐penetrating radar data, and visible band satellite imagery were used to calculate the velocity structure, ice thickness, and the changing ice‐marginal extent of Austfonna (8000 km2 and 2500 km3), the largest ice cap in the Eurasian Arctic. Ice cap motion is generally less than about 10 m a−1, except where faster flowing curvilinear features with velocities of several tens to over 200 m a−1 are present. Most drainage basins of Austfonna have undergone ice‐marginal retreat over the past few decades at an average of a few tens of meters per year. Integrating margin change around the whole ice cap gives a total area loss of about 10 km2 a−1. Iceberg flux from the marine margins of Austfonna is about 2.5 ± 0.5 km3 a−1 (water equivalent), about 45% of the total calving flux from the whole Svalbard archipelago. When mass loss by iceberg production is taken into account, the total mass balance of Austfonna is negative by between about 2.5 and 4.5 km3 a−1. This iceberg flux represents about 33 ± 5% of total annual mass loss from Austfonna, with the remainder lost through surface ablation. Iceberg flux should be included in calculations of the total mass balance of the many large Arctic ice caps, including those located in the Russian and Canadian Arctic that end in tidewater. The neglect of this term has led to underestimates of mass loss from these ice caps and, thus, to underestimates of the contribution of Arctic ice caps to global sea level rise.