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Changes in the frequency and intensity of extremes over Northeast Africa

G Endalew

Climate of Northeastern Africa varies from humid to semi-arid with both abundant and scarce
moisture. Hence, flooding and drought are frequent phenomena which have a direct impact on the
agriculture, health, water and other socio-economic sectors of the region. Analysis for the expected
changes in the frequency and intensity of extreme rainfall induced by climate change in Ethiopia is
the aim of this study.
The Ethiopian area has been divided into three homogeneous rainfall regimes (Zone A-C).The
seasonal classification of the region, especially over Ethiopia, is from February to May, June to
September and October to January, called Belg, Kiremt and Bega, respectively. Here, more
emphasis is given to the Kiremt and Belg seasons.
Anomalous wet and dry decades were identified using ERA-40 data. The condition of the main rain
bearing systems during these decades has been assessed and from this result systems which favor
more for the extremes have been detected. Among the systems that control the weather activity in
the region are: Inter-tropical Convergence Zone (ITCZ), Tropical Easterly Jet (TEJ), East African
Low Level Jet (EALLJ), El Niño-Southern Oscillation (ENSO) as well as Mascarena, St. Helena,
Azores and Arabian High pressure systems. Then simulations from GFDL and CCCma were
There is large decadal variability in the occurrence of extreme rainfall events. During the Kiremt
season, 90-96% wet anomalies were mostly occurring in the 1958-1979 time range. The dry
anomalous decades were mostly found in 1980-2001 for both zone-A and -B. During Belg, all the
dry anomalies are in the third decade of March for zone-B. During April and May, most of the dry
anomalies are in the first decade. For zone-C, most of the dry anomalies are in the third decade of
The sources of moisture, the means of transport and the dynamic conditions should be satisfied to
have a wet anomaly. During the driest decades these conditions are not fulfilled. The future
scenario runs from GFDL and CCCma indicate that both models have a consistent trend. However,
as most models have limitations, even the seasonality is not well represented in both models.

Bibliografische gegevens

G Endalew. Changes in the frequency and intensity of extremes over Northeast Africa
KNMI number: WR-07-02, Year: 2007, Pages: 46

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