Rainfall Mechanisms for the Dominant Rainfall Mode over Zimbabwe Relative to ENSO andor IODZM

Abstract EN

Zimbabwe’s homogeneous precipitation regions are investigated by means of principal component analysis (PCA) with regard to the underlying processes related to ENSO and/or Indian Ocean Dipole zonal mode (IODZM).

Station standardized precipitation index rather than direct rainfall values represent the data matrix used in the PCA.

The results indicate that the country’s rainfall is highly homogeneous and is dominantly described by the first principal mode (PC1).

This leading PC can be used to represent the major rainfall patterns affecting the country, both spatially and temporarily.

The current practice of subdividing the country into the two seasonal rainfall forecast zones becomes irrelevant.

Partial correlation analysis shows that PC1 is linked more to the IODZM than to the traditional ENSO which predominantly demonstrates insignificant association with PC1.

The pure IODZM composite is linked to the most intense rainfall suppression mechanisms, while the pure El Niño composite is linked to rainfall enhancing mechanisms.