Bathymetric controls on calving processes at Pine Island Glacier

Pine Island Glacier is the largest current Antarctic contributor to sea-level rise. Its ice loss has substantially increased over the last 25 years through thinning, acceleration and grounding line retreat. However, the calving line positions of the stabilising ice shelf did not show any trend withi...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: Arndt, Jan Erik, Larter, Robert D., Friedl, Peter, Gohl, Karsten, Höppner, Kathrin, the Science Team of Expedition PS104
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2018
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Online Access:https://doi.org/10.5194/tc-12-2039-2018
https://noa.gwlb.de/receive/cop_mods_00005516
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00005473/tc-12-2039-2018.pdf
https://tc.copernicus.org/articles/12/2039/2018/tc-12-2039-2018.pdf
Description
Summary:Pine Island Glacier is the largest current Antarctic contributor to sea-level rise. Its ice loss has substantially increased over the last 25 years through thinning, acceleration and grounding line retreat. However, the calving line positions of the stabilising ice shelf did not show any trend within the observational record (last 70 years) until calving in 2015 led to unprecedented retreat and changed the alignment of the calving front. Bathymetric surveying revealed a ridge below the former ice shelf and two shallower highs to the north. Satellite imagery shows that ice contact on the ridge was likely lost in 2006 but was followed by intermittent contact resulting in back stress fluctuations on the ice shelf. Continuing ice-shelf flow also led to occasional ice-shelf contact with the northern bathymetric highs, which initiated rift formation that led to calving. The observations show that bathymetry is an important factor in initiating calving events.