Brief communication: impacts of a developing polynya off Commonwealth Bay, East Antarctica, triggered by grounding of iceberg B09B

• Published in: The Cryosphere
• Main Authors: Fogwill, CJ, Van Sebille, E, Cougnon, EA, Turney, CSM, Rintoul, SR, Galton-Fenzi, BK, Clark, GF, Marzinelli, EM, Rainsley, EB, Carter, L
• Format: Article in Journal/Newspaper
• Language: English
• Published: European Geosciences Union (EGU) 2016
• Subjects: Science & Technology; Physical Sciences; Geography; Physical; Geosciences; Multidisciplinary; Physical Geography; Geology; SEA-ICE PRODUCTION; BOTTOM WATER; GLACIER; OCEAN; Meteorology & Atmospheric Sciences; 0405 Oceanography; 0406 Physical Geography And Environmental Geoscience; Antarctic; Commonwealth Bay; East Antarctica; Mertz Glacier; Mertz Glacier Tongue; Antarc*; Antarctica; Iceberg*; Sea ice
• Online Access: http://hdl.handle.net/10044/1/43088; http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000387128300001&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=1ba7043ffcc86c417c072aa74d649202; https://doi.org/10.5194/tc-10-2603-2016

The dramatic calving of the Mertz Glacier tongue in 2010, precipitated by the movement of iceberg B09B, reshaped the oceanographic regime across the Mertz Polynya and Commonwealth Bay, regions where high-salinity shelf water (HSSW) – the precursor to Antarctic bottom water (AABW) – is formed. Here we present post-calving observations that suggest that this reconfiguration and subsequent grounding of B09B have driven the development of a new polynya and associated HSSW production off Commonwealth Bay. Supported by satellite observations and modelling, our findings demonstrate how local icescape changes may impact the formation of HSSW, with potential implications for large-scale ocean circulation.