The Density-Driven Winter Intensification of the Ross Sea Circulation

Author:

Jendersie Stefan12ORCID,Williams Michael J. M.1,Langhorne Pat J.2ORCID,Robertson Robin34ORCID

Affiliation:

1. National Institute of Water and Atmospheric Research; Wellington New Zealand

2. Department of Physics; University of Otago; Dunedin New Zealand

3. China-ASEAN College of Marine Science; Xiamen University Malaysia; Sepang Selangor Malaysia

4. School of Physical, Environmental, and Mathematical Sciences; UNSW Canberra (ADFA), ACT; Australia

Funder

Deep South National Science Challenge

Ministry of Business, Innovation and Employment

National Institute of Water and Atmospheric Research

University of Otago

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography

Reference136 articles.

1. Water-mass transformation by sea ice in the upper branch of the southern ocean overturning;Abernathey;Nature Geoscience,2016

2. Upwelling circulation on the Oregon continental shelf. Part I: Response to idealized forcing;Allen;Journal of Physical Oceanography,1995

3. Antonov , J. I. Seidov , D. Boyer , T. P. Locarnini , R. A. Mishonov , A. V. Garcia , H. E. Baranova , O. K. Zweng , M. M. Johnson , D. R. 2010 World Ocean Atlas 2009 2 Salinity, U.S. Gov. Print. Off., Washington, DC

4. Ocean variability contributing to basal melt rate near the ice front of Ross Ice Shelf, Antarctica;Arzeno;Journal of Geophysical Research: Oceans,2014

5. Does large-scale ocean circulation structure life history connectivity in Antarctic toothfish (Dissostichus mawsoni)?;Ashford;Canadian Journal of Fisheries and Aquatic Sciences,2012

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