The Agulhas system as a key region of the global oceanic circulation

The Agulhas system at the interface between the Indian and Atlantic Ocean is an important region in the global oceanic circulation with a recognized key role in global climate and climate change. It is dominated by high temporal and horizontal variability. This project aims to realistically simulate this complex current system and its effect on the interoceanic transport with the highest spatial resolution to date. Using a hierarchy of global ocean models with realistic and idealized atmospheric forcing, the effect of inter-ocean transport on the large-scale circulation in the Atlantic will be established. This includes the variability of the meridional overturning and heat transports. The core of the project is a high-resolution model of the Agulhas region that is nested in a global one at lower resolution. Both models are able to interact, which allows one to study the feedbacks from the high-resolution model on the large-scale circulation. This project is embedded in the European ocean modeling effort DRAKKAR.

[1]  R. Weiss,et al.  Thermocline and intermediate water communication between the south Atlantic and Indian oceans , 1992 .

[2]  Thierry Penduff,et al.  Eddy-permitting ocean circulation hindcasts of past decades , 2007 .

[3]  M. Maqueda,et al.  Sensitivity of a global sea ice model to the treatment of ice thermodynamics and dynamics , 1997 .

[4]  J. Lutjeharms,et al.  The Natal pulse: An extreme transient on the Agulhas Current , 1988 .

[5]  S. Drijfhout,et al.  The Lagrangian View of South Atlantic Interocean Exchange in a Global Ocean Model Compared with Inverse Model Results , 2004 .

[6]  P. Leeuwen,et al.  Upstream control of Agulhas ring shedding , 2002 .

[7]  Thierry Penduff,et al.  Impact of partial steps and momentum advection schemes in a global ocean circulation model at eddy-permitting resolution , 2006 .

[8]  W. Cai Antarctic ozone depletion causes an intensification of the Southern Ocean super‐gyre circulation , 2006 .

[9]  J. Lutjeharms Remote sensing corroboration of retroflection of the East Madagascar Current , 1988 .

[10]  A nested primitive equation model of the Iceland-Faeroe front , 1996 .

[11]  Y. Masumoto A fifty-year eddy-resolving simulation of the world ocean : Preliminary outcomes of OFES (OGCM for the Earth Simulator) , 2004 .

[12]  S. Speich,et al.  Warm and cold water routes of an O.G.C.M. thermohaline conveyor belt , 2001 .

[13]  W. Hazeleger,et al.  Stability of the thermohaline circulation under millennial CO2 forcing and two alternative controls on Atlantic salinity , 2007 .

[14]  P. Leeuwen,et al.  Eddies and variability in the Mozambique Channel , 2003 .

[15]  R. Schneider,et al.  Vigorous exchange between the Indian and Atlantic oceans at the end of the past five glacial periods , 2004, Nature.

[16]  R. Evans,et al.  Rings of the Agulhas current , 1986 .

[17]  G. Knorr,et al.  Southern Ocean origin for the resumption of Atlantic thermohaline circulation during deglaciation , 2003, Nature.

[18]  J. R. E. Lutjeharms,et al.  Agulhas leakage dynamics affects decadal variability in Atlantic overturning circulation , 2008, Nature.

[19]  W. Collins,et al.  Global climate projections , 2007 .

[20]  Andrei P. Sokolov,et al.  A model intercomparison of changes in the Atlantic thermohaline circulation in response to increasing atmospheric CO2 concentration , 2005 .

[21]  Eric Blayo,et al.  AGRIF: Adaptive grid refinement in Fortran , 2008, Comput. Geosci..

[22]  Graham D. Quartly,et al.  Eddies around Madagascar — The retroflection re-considered , 2006 .

[23]  Johann R. E. Lutjeharms,et al.  Eddies and dipoles around South Madagascar: formation, pathways and large-scale impact , 2004 .

[24]  J. Sheinbaum,et al.  The mesoscale variability in the Caribbean Sea. Part I: Simulations and characteristics with an embedded model , 2008 .

[25]  Arne Biastoch,et al.  Modes of the southern extension of the East Madagascar Current , 2009 .

[26]  A. Gordon Oceanography: The brawniest retroflection , 2003, Nature.

[27]  A. Biastoch,et al.  The Role of Mesoscale Eddies in the Source Regions of the Agulhas Current , 1999 .

[28]  Charlie N. Barron,et al.  The Cape Cauldron: A regime of turbulent inter-ocean exchange , 2003 .

[29]  Thierry Penduff,et al.  Mesoscale Eddies in the Labrador Sea and Their Contribution to Convection and Restratification , 2008 .

[30]  R. Zahn,et al.  345,000-year-long multi-proxy records off South Africa document variable contributions of Northern versus Southern Component Water to the Deep South Atlantic , 2008 .

[31]  S. Speich,et al.  Role of bathymetry in Agulhas Current configuration and behaviour , 2006 .

[32]  Tim N. Palmer,et al.  Physical Climate Processes and Feedbacks , 2001 .

[33]  P. Leeuwen,et al.  Impact of Interbasin Exchange on the Atlantic Overturning Circulation , 1999 .

[34]  Johann R. E. Lutjeharms The Agulhas Current , 2006 .

[35]  Jean-Marc Molines,et al.  Causes of Interannual–Decadal Variability in the Meridional Overturning Circulation of the Midlatitude North Atlantic Ocean , 2008 .

[36]  M. Maqueda,et al.  Modelling the influence of snow accumulation and snow-ice formation on the seasonal cycle of the Antarctic sea-ice cover , 1999 .

[37]  G. Madec NEMO ocean engine , 2008 .

[38]  W. D. Ruijter,et al.  Stability of the Atlantic Overturning Circulation: Competition between Bering Strait Freshwater Flux and Agulhas Heat and Salt Sources , 2001 .

[39]  A. Biastoch,et al.  Mesoscale perturbations control inter‐ocean exchange south of Africa , 2008 .

[40]  P. Leeuwen,et al.  Generation and Evolution of Natal Pulses: Solitary Meanders in the Agulhas Current , 1999 .

[41]  Scott C. Doney,et al.  Evaluation of ocean carbon cycle models with data‐based metrics , 2004 .