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...
Main Authors: | , , , , , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
SCAR
2018
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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/ |