The ocean-driven instability of the South Pacific sector of the West Antarctic Ice Sheet since 773 ka-Reference-Cited by-同舟云学术

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The ocean-driven instability of the South Pacific sector of the West Antarctic Ice Sheet since 773 ka

Published:2021-05-21 Issue: Volume: Page:
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Author:

Wang Jiakai¹^ORCID,Tang Zheng²,Chang Fengming³^ORCID,Nan Qingyun³,Xiong Zhifang⁴^ORCID,Li Tiegang⁵²⁶⁷

Affiliation:

1. Institute of Oceanology of the Chinese Academy of Sciences

2. First Institute of Oceanography

3. Institute of Oceanology, Chinese Academy of Sciences

4. First Institute of Oceanography, State Oceanic Administration, China

5. Qingdao National Laboratory for Marine Science and Technology

6. Ministry of Natural and Resources

7. University of Chinese Academy of Sciences

Publisher

Wiley

Reference7 articles.

1. Geochronology of granite terranes in the Ford Ranges, Marie Byrd Land, West Antarctica;Adams C. J.;New Zealand Journal of Geology and Geophysics.,1987

2. Geochronology of Cretaceous granites and metasedimentary basement on Edward VII Peninsula, Marie Byrd Land, West Antarctica;Adams C. J.;Antarctic Science.,2004

3. Interannual variations in meltwater input to the Southern Ocean from Antarctic ice shelves;Adusumilli S.;Nature Geoscience.,2020

4. Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2;Anderson R. F.;Science.,2009

5. Topographic Effects on the Mean Tropospheric Flow Patterns around Antarctica;Baines P. G.;Journal of the Atmospheric Sciences.,1988

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