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The tenth IMSC, Beijing, China, 2007 - International Meetings on ...

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the Agro_ecological z<strong>on</strong>es of Zambia. <str<strong>on</strong>g>The</str<strong>on</strong>g> analysis shows that in Agro-ecological z<strong>on</strong>e 1, low<br />

intensity rainfall events are increaing and intense rainfall events are decreasing. In<br />

Agro-ecological z<strong>on</strong>e 2 low and moderate rain events are decreasing and intense rain events<br />

are increasing. <str<strong>on</strong>g>The</str<strong>on</strong>g> annual rain events in Agro-ecological z<strong>on</strong>e 1 are increasing at the rate of<br />

0.629 events/year and decreasing in Agro-ecological z<strong>on</strong>e 2 at the rate of 0.33 events/year.<br />

<str<strong>on</strong>g>The</str<strong>on</strong>g> annual rainfall amounts in Agro-ecological z<strong>on</strong>e 1 and 2 are decreasing at the rate of<br />

1.038 and 3.269 mm/ year respectively.<br />

Variability of Rainfall in C<strong>on</strong>necti<strong>on</strong> with the 3 - 5-Day Wave in Northern Africa in summer<br />

Speaker: David MONKAM<br />

David MONKAM<br />

Department of Physics, Faculty of Science, University of Douala, P.O.Box: 24157 Douala - Camero<strong>on</strong><br />

m<strong>on</strong>kam1@yahoo.fr<br />

A composite method is used to determine the spatial pattern of the westward propagating<br />

3 - 5-day waves and the associated rainfall anomalies in northern Africa in summer,<br />

throughout the period 1981-90. <str<strong>on</strong>g>The</str<strong>on</strong>g> rainfall anomalies increasing (decreasing) is associated<br />

with the cycl<strong>on</strong>ic (anticycl<strong>on</strong>ic) circulati<strong>on</strong> and negative (positive) geopotential height<br />

anomalies. <str<strong>on</strong>g>The</str<strong>on</strong>g> waves increase rainfall in the band of latitudes 7.5°- 15°, around the ZCIT<br />

mean positi<strong>on</strong> in summer, with a maximum near the Fouta-Djall<strong>on</strong> in Guinea and decrease<br />

rainfall north of 15° and south of 7.5°. <str<strong>on</strong>g>The</str<strong>on</strong>g> rainfall anomalies increasing or decreasing depends<br />

<strong>on</strong> the waves activities. For example in 1981 where the waves were active, the rainfall<br />

anomalies composited were positive in the whole studied area, with str<strong>on</strong>g values while in<br />

1982 and 1983 where they were weak, the rainfall anomalies composited were negative south<br />

of 10°.<br />

C<strong>on</strong>siderati<strong>on</strong> of Drought at the Aji-chai Basin<br />

Speaker: Davoud Naghizadeh<br />

Davoud Naghizadeh<br />

Head of Radjan Ab C<strong>on</strong>sulting Engineers Co.<br />

d_n_raz2006@yahoo.com<br />

Mr. Rostamzadeh<br />

(PHD Student of physical Geography, University of Tabriz, Iran)<br />

Masumeh KHalkhali<br />

(Master of physical Geography, University of Tabriz, Iran)<br />

Climatic change is <strong>on</strong>e of the natural characteristic of the atmospheric cycle that causes<br />

abnormality and fluctuati<strong>on</strong>s in the trend of climatic parameters such as precipitati<strong>on</strong> and heat.<br />

Atmospheric abnormalities are very intensive in the most parts of the world and resulting<br />

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