1. Role of the Gulf Stream and Kuroshio-Oyashio Systems in Large- Scale Atmosphere-Ocean Interaction: A Review Young-oh Kwon et al.

2. Outline Intorduction Processes affecting the SST variability in the WBCs WBCs and the basin-scale climate variability Performance of climate models on simulation of WBC variability Outstanding issue

3. Introduction There are “exceptionally” strong atmosphere- ocean interaction over West Boundary Current region. – Mean and Variances(SSTA) – Interannual and longer time scale – Heat transport Atmosphere response to WBC STTAs with several issues

4. Processes affecting the SST in WBC region

5. Interesting issues The Connection between frontal-scale boundary layer ocean-atmosphere interaction and the basin-scale variability. Potential changes in WBC ocean duce to global warming. The relationship between the Meridional overturning circulation and Gulf Stream in North Atlantic. Interbasin connection between the KOE and GS variability.

6. Processes affecting the SST variability in the WBCs Shift of oceanic fronts Oceanic advection Surface heat fluxes Ekman transport Reemergence mechanism Remote wind stress curl forcing communicated via oceanic Rossby wave Tropical atmosphere teleconnections

7. Shift of oceanic front Decadal SST variability is particularly strong along the SubArctic Frontal Zones.

8. Oceanic advection In the WBCs on interannual and longer time scales is determined mainly by anomalous geostrophic advection, which tends to dominate over Ekman advection and Q net.

9. Surface heat flux Q net in the WBC

10. Ekman Transport Ekman transport responds quickly to changes in surface wind and can generate SSTA. To reinforce the Q net in mid-latitudes because stronger westerlies cool the ocean by the sensible and latent heat fluxes and by southward Ekman transport. The cross-frontal cold Ekman advection lowers the near-surface stratification on the warmer side of the front and enhance vertical mixing.

11. Reemergence mechanism

12. Remote wind stress curl forcing communicated via oceanic Rossby wave

13. Tropical Teleconnection

14. WBCs and the basin-scale climate variability Decadal SST variability in the WBCs Oceanic dynamics and decadal variability Surface heat flux damping and implications Decadal variability in atmosphere-ocean coupled general circulation models

15. Decadal SST variability in the WBCs

16. Oceanic dynamics and decadal variability As the Rossby waves propagate westward, they integrate the stochastic forcing to increase the variance and dominant period of dynamic ocean properties until reaching a maximum near the WBC. The spatial resonance mechanisms could generate a decadal peak in the ocean by stochastic atmosphere.

17. Surface heat flux damping and implications

18. Decadal variability in atmosphere- ocean coupled general circulation models Coupled climate models generally indicate that ocean-atmosphere interaction in WBC regions is a key factor in generating extropical decadal variability. Although earlier studies suggested that North Atlantic decadal variability in SST was primarily reflecting a passive response to the atmospheric forcing.

19. Performance of climate models on simulation of WBC variability High-resolution ocean simulations Simulation of the Kuroshio and Gulf Stream at non-eddy-permitting resolution Atmospheric simulations

20. High-resolution ocean simulations For KOE: – KE’s path variability can be tied largely to wind forcing. For GS: – Interaction between DWBC.

21. Simulation of the Kuroshio and Gulf Stream at non-eddy-permitting resolution

23. Outstanding issues How are the frontal-scale and basin-scale atmosphere-ocean interactions related? What is the large scale atmospheric circulation/wind stress curl response to the WBC SSTA Global warming and the WBCs Relation between the Gulf Stream and the MOC Connection between GS and KOE variability