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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 15, issue 4 | Copyright
Ann. Geophys., 15, 471-475, 1997
https://doi.org/10.1007/s00585-997-0471-x
© European Geosciences Union 1997

  30 Apr 1997

30 Apr 1997

Impact of warm ENSO events on atmospheric circulation and convection over the tropical Atlantic and West Africa

S. Janicot S. Janicot
  • Météo-France, Laboratoire de Météorologie Dynamique du CNRS, Palaiseau, France

Abstract. Empirical studies have shown that warm El Nino/Southern Oscillation (ENSO) episodes are associated during northern summer with, first, a southward location of the intertropical convergence zone (ITCZ) over the tropical Atlantic, and, second, a weakened convection over West Africa where the ITCZ is near its mean latitude. A modelling experiment presented here is used to help explain this apparent contradiction. In simulated ENSO conditions, the ITCZ is located southwards over the tropical Atlantic. Over West Africa the intertropical front is also displaced southwards, but more slightly; the ITCZ is located at its climatological latitude and the vertical development of convective clouds over West and Central Africa is reduced due to dynamical subsidence in the upper levels.

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