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Relationships between intraseasonal rainfall variability of coastal Tanzania and ENSO

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Summary

The influence of ENSO on intraseasonal variability over the Tanzanian coast during the short (OND) and long (MAM) rainy seasons is examined. In particular, variability in the rainfall onset, peak and end dates as well as dry spells are considered. In general, El Niño appears to be associated with above average rainfall while La Niña is associated with below average rainfall over the northern Tanzanian coast during OND, and to lesser extent MAM. Over the southern coast, the ENSO impacts are less coherent and this region appears to be a transition zone between the opposite signed impacts over equatorial East and southern Africa. The increased north coast rainfall during El Niño years is generally due to a longer than normal rainfall season associated with early onset while reduced rainfall during La Niña years tends to be associated with a late onset, and thus a shorter than average rainfall season. Wet conditions during El Niño years were associated with enhanced convection and low-level easterly anomalies over the equatorial western Indian Ocean implying enhanced advection of moisture from the Indian Ocean while the reverse is true for La Niña years. Hovmöller plots for OLR and zonal wind at 850 hPa and 200 hPa show eastward, westward propagating and stationary features over the Indian Ocean. It was observed that the propagating features were absent during strong El Niño years. Based on the Hovmöller results, it is observed that the convective oscillations over the Tanzanian coast have some of the characteristic features of intraseasonal oscillations occurring elsewhere in the tropics.

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Authors and Affiliations

  1. Department of Oceanography, University of Cape Town, Rondebosch, South Africa

    A. L. Kijazi & C. J. C. Reason

  2. Tanzania Meteorological Agency, Dar es Salaam, Tanzania

    A. L. Kijazi

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  1. A. L. Kijazi
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  2. C. J. C. Reason
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Kijazi, A., Reason, C. Relationships between intraseasonal rainfall variability of coastal Tanzania and ENSO. Theor. Appl. Climatol. 82, 153–176 (2005). https://doi.org/10.1007/s00704-005-0129-0

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  • DOI: https://doi.org/10.1007/s00704-005-0129-0

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