An assessment of Antarctic Circumpolar Current and Southern Ocean meridional overturning circulation during 1958–2007 in a suite of interannual CORE-II simulations
By R. Farneti, Stephanie M. Downesb, Stephen M. Griffiesc, Simon J. Marslandd, Erik Behrense, Mats Bentsenf, Daohua Bid, Arne Biastoche, Claus Böninge, Alexandra Bozecg and 28 more. 2015
160 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/477288a84a041e2d643f94341ae96f753a2ee9bf
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
- Robert Hallberg
- S. Griffies
- Gokhan Danabasoglu
- B. Fox‐Kemper
- Andrew T. Wittenberg
- I. Held
- Alistair Adcroft
- Patrick Heimbach
In Global and Planetary Change
- Robert Hallberg
- S. Griffies
- Gokhan Danabasoglu
- B. Fox‐Kemper
- Alistair Adcroft
- D. Marshall
- Sonya Legg
- S. Yeager
In Oceanography
- Robert Hallberg
- S. Griffies
- Gokhan Danabasoglu
- B. Fox‐Kemper
- Alistair Adcroft
- C. Böning
- D. Marshall
- I. Held
Citations in the corpus
- The GFDL Global Ocean and Sea Ice Model OM4.0: Model Description and Simulation Features (2019, background): “…in westerly wind stress increases more than 50% during the 60‐year CORE‐II cycle and it trends southward by a few degrees latitude (see Figures 1 and 2 from Farneti et al., 2015), in agreement with the observed positive trend in the Southern Annular Mode (Marshall, 2003; Thompson et al., 2000).”
- Challenges and Prospects in Ocean Circulation Models (2019, background): “Important large scale applications over the last decade are simulations of the Southern Ocean, the Meridional Overturning Circulation and its variability, and regional sea level change.”
- Resolving and Parameterising the Ocean Mesoscale in Earth System Models (2020, background): “Perhaps in consequence, representation of all of these ocean processes show considerable sensitivities to ocean model resolution and configuration, even including fairly subtle changes to closure schemes which represent the impacts of sub-gridscale processes [86, 87].”