Glacimarine sedimentation processes at Kronebreen and Kongsvegen, Svalbard

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Glacimarine sedimentation processes at Kronebreen and Kongsvegen, Svalbard

Tidewater glaciers deposit sediment at their terminus, thereby reducing the relative water depth. Reduced water depth can lead to increased glacier stability through decreased rates of iceberg calving, glacier thinning and submarine melting. Here we investigate sedimentation processes at the termini of Kronebreen and Kongsvegen, Svalbard. We mapped the fjord floor bathymetry in August 2009 and ...

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ژورنال

عنوان ژورنال: Journal of Glaciology

سال: 2011

ISSN: 0022-1430,1727-5652

DOI: 10.3189/002214311798043708