The Southern Ocean Limb of the Global Deep Overturning Circulation
By B. Sloyan, S. Rintoul. 2001
380 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/0a137ad4dd42f17d554588889731a9465b48b9d0
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
- Raffaele Ferrari
- Jochem Marotzke
- John Marshall
- Johann Jungclaus
- M. Nikurashin
- Helmuth Haak
- N. Keenlyside
- M. Latif
In Global and Planetary Change
- Raffaele Ferrari
- Jochem Marotzke
- M. Nikurashin
- John Marshall
- Johann Jungclaus
- Helmuth Haak
- M. Latif
- N. Keenlyside
In Oceanography
- Raffaele Ferrari
- M. Nikurashin
- John Marshall
- Jochem Marotzke
- Johann Jungclaus
- N. Keenlyside
- M. Latif
- Helmuth Haak
Citations in the corpus
- Ocean Circulation and Tropical Variability in the Coupled Model ECHAM5/MPI-OM (2006, background): “Sloyan and Rintoul (2001) and Ganachaud and Wunsch (2000) suggested an AABW inflow of about 6 Sv.”
- Closure of the meridional overturning circulation through Southern Ocean upwelling (2012, background): “2a , and assumptions about the statistics of property distributio”
- Global Ocean Meridional Overturning (2007, methodology): “In both this model and in Sloyan and Rintoul (2001), independent layer-to-layer transfers are allowed for each property: that is, we do not assume that a single effective diffusivity value acts to transfer both heat and salt between two neutral density layers in a given box.”
- Radiation and Dissipation of Internal Waves Generated by Geostrophic Motions Impinging on Small-Scale Topography: Theory (2010, background): “Inverse calculations (Ganachaud and Wunsch 2000; Sloyan and Rintoul 2001) find that this vigorous turbulent mixing contributes crucially to”
- Radiation and Dissipation of Internal Waves Generated by Geostrophic Motions Impinging on Small-Scale Topography: Application to the Southern Ocean (2010, background): “Inverse analyses of the Southern Ocean hydrography confirm that high mixing rates in the deep Southern Ocean are required to close the heat and salt budgets (Ganachaud and Wunsch 2000; Sloyan and Rintoul 2001).”
- On the driving processes of the Atlantic meridional overturning circulation (2007, background): “In accordance with this, inverse model results [Sloyan and Rintoul, 2001b] and high-resolution ocean models [Killworth and Nanneh, 1994; Hallberg and Gnanadesikan, 2007] indicate considerable poleward transport at layers above topography.”