Deglacial change of Antarctic Bottom Water in transient simulations

The deglacial change of Antarctic Bottom Water (AABW) since the Last Glacial Maximum (LGM) was investigated using transient simulations of climate evolution forced by individual deglacial forcings. The TraCE21k simulation faithfully reproduces the ∼500 m deepening of the cell interface between AABW...

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Veröffentlicht in:	Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao 2023-11, Vol.16 (6), p.100333-7, Article 100333
1. Verfasser:	Zhu, Chenyu
Format:	Artikel
Sprache:	eng
Schlagworte:	Antarctic Bottom Water Deglacial change Southern ocean sea-ice Transient simulations 关键词 冰消期演变 南大洋海冰 南极底层水 瞬变模拟
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