A New Grounding-line Proximal Sedimentary Record from Inner Pine Island Bay

Pine Island Glacier (PIG) is one of the fastest changing ice streams of the West Antarctic Ice Sheet. Its ice shelf underwent major calving events throughout recent years. The main factor for the considerable mass loss of PIG is sub-ice shelf melting caused by the advection of warm deep water into P...

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Bibliographic Details
Main Authors: Afanasyeva, Victoria, Kuhn, Gerhard, Hillenbrand, Claus-Dieter, Klages, Johann P., SzczuciƄski, Witold, Frederichs, Thomas, Leitchenkov, German
Format: Conference Object
Language:unknown
Published: SCAR 2018
Subjects:
Online Access:https://epic.awi.de/id/eprint/51988/
https://epic.awi.de/id/eprint/51988/1/Afanasyeva_et_al_2018_polar2018_abstr.pdf
http://www.professionalabstracts.com/POLAR2018/iPlanner
https://hdl.handle.net/10013/epic.5cd2e9cc-339a-4eec-9a09-82332fe1a2f0
https://hdl.handle.net/