eCite Digital Repository

Southern Ocean

Citation

Mazloff, MR and Sallee, J-B and Menezes, VV and Macdonald, AM and Meredith, MP and Newman, L and Pellichero, V and Roquet, F and Swart, S and Wahlin, A, Southern Ocean, Bulletin of the American Meteorological Society, 98, (8) pp. S166-167. ISSN 0003-0007 (2017) [Refereed Article]


Preview		PDF
4Mb		  

Copyright Statement

Copyright 2017 American Meteorological Society (AMS). Permission to use figures, tables, and brief excerpts from this work in scientific and educational works is hereby granted provided that the source is acknowledged. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act or that satisfies the conditions specified in Section 108 of the U.S. Copyright Act (17 USC §108) does not require the AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a website or in a searchable database, or other uses of this material, except as exempted by the above statement, requires written permission or a license from the AMS. All AMS journals and monograph publications are registered with the Copyright Clearance Center (http://www.copyright.com). Questions about permission to use materials for which AMS holds the copyright can also be directed to permissions@ametsoc.org. Additional details are provided in the AMS Copyright Policy statement, available on the AMS website (http://www.ametsoc.org/CopyrightInformation).

DOI: doi:10.1175/2017BAMSStateoftheClimate.1

Abstract

By connecting the deep ocean reservoir of carbon and heat to the atmosphere, the Southern Ocean is a primary climate regulator. A readily observed component of regulation is the sea ice cover, which provides insulation and affects albedo. As noted in Section 6f, 2016 showed a spectacular decline late in the year, with the lowest ever recorded spring sea ice cover (see Fig. 6.8a). The upper ocean experienced large temperature anomalies consistent with the sea ice patterns discussed in Section 6f (Figs. 6.10b,c). In addition, the open-ocean polynya observed over Maud Rise in August (e.g., see Fig. 6.8c) was likely driven by unusually weak haline stratification (Fig. 6.10f). Observed salinity changes suggest cryospheric influences on multiyear time scales.

Item Details

Item Type:Refereed Article
Keywords:Southern Ocean, climate
Research Division:Earth Sciences
Research Group:Oceanography
Research Field:Physical Oceanography
Objective Division:Environment
Objective Group:Other Environment
Objective Field:Antarctic and Sub-Antarctic Oceanography
UTAS Author:Newman, L (Dr Louise Newman)
ID Code:128086
Year Published:2017
Web of Science® Times Cited:37
Deposited By:Oceans and Cryosphere
Deposited On:2018-09-03
Last Modified:2018-10-08
Downloads:95 View Download Statistics

Repository Staff Only: item control page