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Jozani biodiversity inventory report 2002 - Coastal Forests of Kenya ...

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tropics depends mainly on the movements <strong>of</strong> the air masses that cover the globe. The heavy rains<br />

from March to May are brought about when the Intertropical Convergence Zone (ITCZ) is to the<br />

north <strong>of</strong> the equator; hence Tanzania receives the convection currents causing rain. The short<br />

rains in October are due to the ITCZ moving southwards from the Tropic <strong>of</strong> Capricorn. There are<br />

no rainfall records from <strong>Jozani</strong> and only recently has a rain gauge been installed at the station,<br />

however data recording is still not satisfactory. Rainfall data from Zanzibar is presented showing<br />

mean monthly rainfall for a period <strong>of</strong> 13 years (Figure 1). Zanzibar receives rain almost all year<br />

round and no month completely lacks rainfall. East Africa coastal islands receive the highest<br />

rainfall, with Pemba receiving the highest rain (2000mm/year) while Zanzibar receive on the<br />

average 1565mm/year (UNEP, 2001). In <strong>Jozani</strong> area the locals refer to the heavy rains as<br />

"masika" and the short rains as "vuli". Unreliable rainfall between the two main seasons is known<br />

as "chororo.<br />

Mean monthly rainfall (mm)<br />

450<br />

400<br />

350<br />

300<br />

250<br />

200<br />

150<br />

100<br />

50<br />

0<br />

65<br />

48<br />

139<br />

399<br />

211<br />

72<br />

40 44 52<br />

73<br />

210<br />

165<br />

January<br />

February<br />

March<br />

April<br />

May<br />

June<br />

July<br />

August<br />

September<br />

October<br />

November<br />

December<br />

Month<br />

Figure 1: Mean monthly rainfall for Kisauni Airport Zanzibar for a period <strong>of</strong> 13 years<br />

(Source: TANRIC, UDSM)<br />

2.8 Hydrology<br />

The Quaternary geomorphology forms part <strong>of</strong> Zanzibar's corridor aquifer complex. <strong>Jozani</strong> area is<br />

<strong>report</strong>ed to be the lowest in Zanzibar and the water table is generally high, <strong>of</strong>ten emerging above<br />

the ground surface forming springs and marshes. High water tables are also evident in areas with<br />

ground water forest. Some creeks in Charawe, Chwaka and Kichanga extend inland sometimes<br />

8

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