Author(s)

Joël Amouin^1,2*, Kouassi Yves Kouadio^1*, Modeste Kacou¹, Sandrine Djakouré¹, Samuel Ta¹

¹Laboratory of Matter, Environmental and Solar Energy Sciences (LASMES), Ocean-Atmosphere Interaction Group, University F.H.B. of Cocody Abidjan, Abidjan, Côte d’Ivoire.
²Abidjan Meteorological Center of the Agency for the Safety of Air Navigation in Africa and Madagascar (ASECNA), Abidjan, Côte d’Ivoire.

Rain flooding during June on the West Africa coastal area is analyzed by using the 95th and 75th percentiles, which represent extreme and intense rainfall events respectively. Thus, the contribution of these events that reaches around 50% shows their impact on the rainfall in June. Atmospheric and oceanic factors influence the rain flooding. Indeed, the extreme events are associated with easterly waves propagating from 20°E, while those of intense events are initiated around 5°E. The impact of oceanic conditions exhibits the warming of the equatorial rail and the Atlantic cold tongue, the warming of the whole ocean basin and a north-south dipole of SST anomalies. The West African monsoon that reaches Abidjan corresponds to a low-level atmospheric flow, whose upward motion extends in latitude from the ocean to the continent. An increase of disturbance contributes to enhancing these events. This is confirmed by the inflow on to the continent of oceanic moisture coming from the ventilation by evaporation of warm water. In addition, the coupled ocean-atmosphere simulations are one of the best candidates that could help to better explain these dramatic events. This study is useful because of showing solutions that could help in adoption of policies for the risks management related to these events.

West Africa Coast, Rain Flooding, Threshold, Atmospheric and Ocean Surface Conditions

Amouin, J. , Kouadio, K. , Kacou, M. , Djakouré, S. and Ta, S. (2021) Diagnosis of the Causes of the Rain Flooding in June in the West Africa Coastal Area. Atmospheric and Climate Sciences, 11, 11-31. doi: 10.4236/acs.2021.111002.