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- W59686578 abstract "The pristine coasts of Spitsbergen, major island of Svalbard Archipelago provide a superb opportunity to quantify how High Arctic coasts are responding to glacier retreat and associated intensified sediment flux to the fjord and shelf zones. This study focuses on the mechanisms controlling the recent coastal evolution (1990–2009) in Northern Petuniabukta, one of the most sheltered bays of central Spitsbergen, characterised by a semi-arid subpolar climate, limited wave action and rapid retreat rate of all surrounding glaciers. The formation of the coastal landforms here was to a large degree dependent of the rate of sediment excavation from alluvial fans and outwash plains that developed across a wide coast plain between the glacier valleys and the fjord. During last two decades most of the sediments transported from proglacial zones has been accumulated on outwash plains and after reworking supplied a prograding tidal flat system. Despite sheltered location and drier climate the rates of coastal evolution in Petuniabukta are comparable to those seen along the W and S coasts of Spitsbergen." @default.
- W59686578 created "2016-06-24" @default.
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- W59686578 date "2014-09-07" @default.
- W59686578 modified "2023-09-28" @default.
- W59686578 title "The Influence of Recent Deglaciation and Associated Sediment Flux on the Functioning of Polar Coastal Zone – Northern Petuniabukta, Svalbard" @default.
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- W59686578 doi "https://doi.org/10.1007/978-94-017-9260-8_2" @default.
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