On the Relationship of the Circumpolar Current to Southern Hemisphere Winds in Coarse-Resolution Ocean Models
By A. Gnanadesikan, Robert Hallberg. 2000
151 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/2d90ef3d19f8cb199fad0df4d2138ecf81f714e1
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- John Marshall
- Robert Hallberg
- T. Radko
- S. Griffies
- A. Gnanadesikan
- Helen Jones
- Richard Karsten
- A. Morrison
In Global and Planetary Change
In Oceanography
- John Marshall
- Robert Hallberg
- Raffaele Ferrari
- S. Griffies
- A. Gnanadesikan
- T. Radko
- Helen Jones
- A. Morrison
Citations in the corpus
- Constructing the Residual Circulation of the ACC from Observations (2002, background): “Recent studies have focused on the combined effect of wind and thermohaline forcing (Marshall 1997; Gnanadesikan and Hallberg 2000; Speer et al. 2000; Marshall et al. 2002; KJM).”
- Residual-Mean Solutions for the Antarctic Circumpolar Current and Its Associated Overturning Circulation (2003, result): “This dependence should be compared with the predictions of other authors who argue that the baroclinic transport varies like (Johnson and BrydenÏt 1989), is independent of the wind (Straub 1993), or varies like t (Gnanadesikan and Hallberg 2000; Karsten et al. 2002, and this study).”
- The Role of Mesoscale Eddies in the Rectification of the Southern Ocean Response to Climate Change (2010, background): “We note that there is no buoyancy forcing in the eddy-saturation theory of Straub (1993) and that local and remote buoyancy forcings play a role in setting the stratification and transport of the ACC (Gnanadesikan and Hallberg 2000).”
- The Role of Eddy Transfer in Setting the Stratification and Transport of a Circumpolar Current (2002, methodology): “Recent simulations by Gnanadesikan and Hallberg (2000) using a two-layer model, which parameterized diapycnal fluxes in terms of a vertical velocity, resulted in an ACC with a transport that varied linearly with the wind stress.”
- 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 (2006, methodology): “However, MESO does have implications for the question of the role of surface wind stress in driving the global overturning circulation.”
- On the Relationship between Southern Ocean Overturning and ACC Transport (2013, background): “saturation (Straub 1993) to a linear dependence on applied wind stress (Gnanadesikan and Hallberg 2000; Marshall and Radko 2003).”