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Atlas Final Web Version 6_14

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The north-easterly movement of the ICTZ across Ethiopia means that the kremt season is<br />

longest in the south-west of the country and shortest in the north-east.<br />

Belg (Mar-May)<br />

The belg rains result from a weather system that develops to the north of the ITCZ between<br />

the successful cultivation of belg season sweet potatoes – a key hunger season crop.<br />

Gu (April-May) & Deyr (October-November) 2<br />

These are the main season rains for the pastoral areas in the south and south-east of the country.<br />

In terms of weather system they can be thought of as early and late kremt rains respectively.<br />

January and May.<br />

These rains are<br />

associated<br />

offshore<br />

with<br />

winds<br />

originating in the<br />

Arabian Sea. Belg<br />

rainfall peaks in April.<br />

The map for April<br />

clearly shows the<br />

belg rains falling on<br />

the north-east and<br />

Harerge Highlands.<br />

Rainfall in January<br />

and February (which<br />

can be thought of as<br />

early belg rainfall) is important in certain parts of the country. Coastal rains in these months<br />

are important for pastoral areas bordering northern Somalia, Djibouti and Eritrea (heys rains in<br />

Somali, dadac in Afar). In SNNPR rainfall in January-February (the sapia rains) is important for<br />

200<br />

150<br />

100<br />

50<br />

0<br />

400<br />

350<br />

200<br />

100<br />

0<br />

100<br />

80<br />

60<br />

40<br />

20<br />

0<br />

Belg<br />

J F M A M J J A S O N D<br />

J F M A M J J A S O N D<br />

Gu<br />

J F M A M J J A S O N D<br />

The gu rains start as<br />

the ITCZ passes over<br />

southern<br />

Ethiopia,<br />

and are brought to<br />

an end by relatively<br />

dry winds blowing<br />

north-east<br />

along<br />

the African coast<br />

from May onwards<br />

(see map for June,<br />

which shows a<br />

‘corridor’ of dryness<br />

along the coast) 3 .<br />

The<br />

southward<br />

movement of the<br />

ITCZ in the second half of the year brings renewed rainfall (deyr rains) between October and<br />

November.<br />

Kremt<br />

Kremt<br />

Deyr<br />

The ITCZ and coastal weather<br />

systems from the Arabian<br />

seas combine to create both<br />

bimodal and unimodal<br />

patterns of rainfall.<br />

The north-east and east have<br />

a bi-modal pattern (belg and<br />

kremt). The south-west of the<br />

country has one long rainy<br />

season (kremt). The southeast<br />

has a bi-modal gu and<br />

deyr pattern. The gu and<br />

deyr graphic shows clearly<br />

how gu and deyr correspond<br />

respectively to the beginning<br />

and end of the kremt.<br />

2 Amharic and Somali names are used to describe the seasons in this graphic. The Afar and Oromifa names are given in the text<br />

box on page 15.<br />

3 These winds are associated with low pressure over Asia created by the heat of the northern hemisphere summer. They blow<br />

from May-September.<br />

Seasonality & Livelihoods<br />

The Livelihoods <strong>Atlas</strong> for Ethiopia The Livelihoods Integration Unit 13

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