The Role of Mesoscale Eddies in the Rectification of the Southern Ocean Response to Climate Change

By R. Farneti, T. Delworth, A. Rosati, S. Griffies, F. Zeng. 2010

225 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/5d8f53d7625db7892cf7a357904de2cf6ea5e134

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In Global and Planetary Change

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Citations in the corpus

Antarctic climate response to stratospheric ozone depletion in a fine resolution ocean climate model (2012, background): “[19] Several recent studies have shown that a greatly intensified zonal surface wind stress in the Southern Ocean gives rise to an enhanced southward heat flux south of about 60 S [Farneti et al., 2010; Gent and Danabasoglu, 2011], which would bring heat into the sea-ice covered ocean.”
The Dependence of Southern Ocean Meridional Overturning on Wind Stress (2011, background): “This is true of both realistic models (Hallberg and Gnanadesikan 2006; Farneti et al. 2010) and models with simplified geometry and forcing (Henning and Vallis 2005).”
The GFDL CM3 Coupled Climate Model: Characteristics of the Ocean and Sea Ice Simulations (2011, methodology): “As suggested by the modeling study of Farneti et al. (2010), the CM2.”
Universal structure of mesoscale eddies in the ocean (2013, background): “…world oceans, they are approximately in geostrophic balance, strongly constrained by the Earth’s rotation and ocean stratification, affecting motions of larger and smaller scales [Farneti et al., 2010; Capet et al., 2008], and effectively transporting various tracers [Roemmich and Gilson, 2001].”
An assessment of Antarctic Circumpolar Current and Southern Ocean meridional overturning circulation during 1958–2007 in a suite of interannual CORE-II simulations (2015, background): “Consistent with previous studies (Danabasoglu and Marshall, 2007; Eden et al., 2009; Farneti and Gent, 2011; Gent ( l t m A r E C w I h t G i a q D C M m H D L s ( C C u r s e A o t s 0 O N t A a t m A d t a t a a b M E v w a and Danabasoglu, 2011; Hofmann and Maqueda, 2011; Kuhlbrodt et al.,…”
Spatial Variability of Sea Level Rise in Twenty-First Century Projections (2010, background): “Recent studies suggest that in an eddy-permitting coupled model, the DSL, ACC, and overturning circulation in the Southern Ocean become relatively insensitive in the twenty-ﬁrst century projection (Farneti et al. 2010).”
On the Relationship between Southern Ocean Overturning and ACC Transport (2013, background): “7d of Farneti et al. (2010) reveals a similar response of the isopycnal slopes in a coupled eddypermitting model, with a flattening of isopycnals in the northern part of the ACC region and steepening limited to the south.”
Observations, inferences, and mechanisms of the Atlantic Meridional Overturning Circulation: A review (2016, background): “…and Radko, 2003; Abernathey et al., 2011], and hence, the response of the AMOC to Southern Ocean winds is relatively modest [Hallberg and Gnanadesikan, 2006; Farneti et al., 2010; Farneti and Delworth, 2010; Farneti and Gent, 2011; Gent and Danabasoglu, 2011; Bryan et al., 2013; Gent, 2015].”