The Role of Eddies in Determining the Structure and Response of the Wind-Driven Southern Hemisphere Overturning: Results from the Modeling Eddies in the Southern Ocean (MESO) Project

By Robert Hallberg, A. Gnanadesikan. 2006

487 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/14fd19123d8af52a8eacccd9f399da06bf001749

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Citations in the corpus

Suppression of Eddy Diffusivity across Jets in the Southern Ocean (2010, methodology): “) and numerical models (e.g., Hallberg and Gnanadesikan 2006) show that the ACC system is best described as the superposition of permanent jets and propagating eddies.”
Response to Increasing Southern Hemisphere Winds in CCSM4 (2011, methodology): “This supports the conclusions in Hofmann and Morales-Maqueda (2011) and Farneti and Gent (2011),”
The GFDL Global Ocean and Sea Ice Model OM4.0: Model Description and Simulation Features (2019, result): “These results are consistent with the general view of the role of eddies (e.g., Farneti et al., 2010; Griffies et al., 2015; Hallberg & Gnanadesikan, 2006).”
Challenges and Prospects in Ocean Circulation Models (2019, methodology): “Adcroft and Hallberg (2006) classify generalized coordinates ocean models as either Lagrangian Vertical Direction (LVD) or Eulerian Vertical Direction (EVD) models.”
Using a resolution function to regulate parameterizations of oceanic mesoscale eddy effects (2013, background): “For instance, in the case of the Southern Ocean, Hallberg and Gnanadesikan (2006) demonstrate that explicitly modeled eddies lead to a coherent transport of water over significant distances, including southward transports of watermasses that are lighter than any that exist at a given location in the”
The Dependence of Southern Ocean Meridional Overturning on Wind Stress (2011, background): “Of the various simplifications we have made, perhaps the most restrictive and unrealistic is the fixed stratification imposed by the northern boundary sponge layer.”
Parameterizing the fresh-water flux from land ice to ocean with interactive icebergs in a coupled climate model (2010, background): “Some details of the new model can be found in Hallberg and Gnanadesikan (2006).”
The Role of Poleward-Intensifying Winds on Southern Ocean Warming (2007, background): “However, recent high-resolution ocean modeling results ( Hallberg and Gnanadesikan 2006 ) suggest that increased mesoscale eddy activity can offset the effect of increased surface winds on the meridional overturning, and subsurface density structure, in the Southern Ocean.”