Impact of the Mertz Glacier Tongue calving on dense water formation and export

Antarctic Bottom Water (AABW) is a critical component of the global climate system, occupying the abyssal layer of the World Ocean and driving the lower limb of the global meridional overturning circulation. Around East Antarctica, the dense shelf water (DSW) precursor to AABW is predominantly forme...

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Bibliographic Details
Published in:Nature Communications
Main Authors: Kusahara, K, Hasumi, H, Williams, GD
Format: Article in Journal/Newspaper
Language:English
Published: Nature Publishing Group 2011
Subjects:
Earth Sciences
Oceanography
Physical Oceanography
Antarctic
East Antarctica
Mertz Glacier
George V Land
Mertz Glacier Tongue
Antarc*
Antarctica
Iceberg*
Sea ice
Online Access:https://doi.org/10.1038/ncomms1156
http://ecite.utas.edu.au/96876
Description
Summary:Antarctic Bottom Water (AABW) is a critical component of the global climate system, occupying the abyssal layer of the World Ocean and driving the lower limb of the global meridional overturning circulation. Around East Antarctica, the dense shelf water (DSW) precursor to AABW is predominantly formed by enhanced sea ice formation in coastal polynyas. The dominant source region of AABW supply to the AustralianAntarctic Basin is the Adlie and George V Land coast, in particular, polynyas formed in the western lee of the Mertz Glacier Tongue (MGT) and the grounded iceberg B9b over the Adlie and the Mertz Depressions, respectively. The calving of the MGT, which occurred on 1213 February 2010, dramatically changed the environment for producing DSW. Here, we assess its impact using a state-of-the-art ice-ocean model. The model shows that oceanic circulation and sea ice production in the region changes immediately after the calving event, and that the DSW export is reduced by up to 23%.

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