Climate Dynamics

, Volume 36, Issue 5, pp 989–1003

Impacts of interruption of the Agulhas leakage on the tropical Atlantic in coupled ocean–atmosphere simulations


    • Royal Netherlands Meteorological Institute (KNMI)
  • Edmo J. D. Campos
    • Oceanographic InstituteUniversity of São Paulo (IOUSP)
  • Sybren Drijfhout
    • Royal Netherlands Meteorological Institute (KNMI)
  • Wilco Hazeleger
    • Royal Netherlands Meteorological Institute (KNMI)
  • Camiel Severijns
    • Royal Netherlands Meteorological Institute (KNMI)

DOI: 10.1007/s00382-009-0692-7

Cite this article as:
Haarsma, R.J., Campos, E.J.D., Drijfhout, S. et al. Clim Dyn (2011) 36: 989. doi:10.1007/s00382-009-0692-7


In this paper we use a coupled ocean–atmosphere model to investigate the impact of the interruption of Agulhas leakage of Indian ocean water on the tropical Atlantic, a region where strong coupled ocean–atmosphere interactions occur. The effect of a shut down of leakage of Indian ocean water is isolated from the effect of a collapse of the MOC. In our experiments, the ocean model is forced with boundary conditions in the southeastern corner of the domain that correspond to no interocean exchange of Indian ocean water into the Atlantic. The southern boundary condition is taken from the Levitus data and ensures an MOC in the Atlantic. Within this configuration, instead of warm and salty Indian ocean water temperature (cold) and salinity (fresh) anomalies of southern ocean origin propagate into the South Atlantic and eventually reach the equatorial region, mainly in the thermocline. This set up mimics the closure of the “warm water path” in favor of the “cold water path”. As part of the atmospheric response, there is a northward shift of the intertropical convergence zone (ITCZ). The changes in trade winds lead to reduced Ekman pumping in the equatorial region. This leads to a freshening and warming of the surface waters along the equator. Especially in the Cold Tongue region, the cold and fresh subsurface anomalies do not reach the surface due to the reduced upwelling. The anomaly signals are transported by the equatorial undercurrent and spread away from the equator within the thermocline. Part of the anomaly eventually reaches the Tropical North Atlantic, where it affects the Guinea Dome. Surprisingly, the main effect at the surface is small on the equator and relatively large at the Guinea Dome. In the atmosphere, the northward shift of the ITCZ is associated with a band of negative precipitation anomalies and higher salinities over the Tropical South Atlantic. An important implication of these results is that the modified water characteristics due to a shut down of the Agulhas leakage remain largely unaffected when crossing the equatorial Atlantic and therefore can affect the deepwater formation in the North Atlantic. This supports the hypothesis that the Agulhas leakage is an important source region for climate change and decadal variability of the Atlantic.


Climate variabilityAtlantic oceanNumerical modellingAgulhas leakageOcean–atmosphere coupling

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© Springer-Verlag 2009