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Biophysical Survey of Mafia Island Marine Reserves

Biophysical Survey of Mafia Island Marine Reserves

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II. STUDY SITES<br />

The <strong>Mafia</strong> <strong>Island</strong> <strong>Marine</strong> <strong>Reserves</strong> are located in <strong>Mafia</strong> District, Tanzania, to the North-<br />

west <strong>of</strong> <strong>Mafia</strong> <strong>Island</strong>. They are situated in the Western Indian Ocean in the shallow<br />

stretch <strong>of</strong> water that separates <strong>Mafia</strong> <strong>Island</strong> from the mainland <strong>of</strong> Tanzania,<br />

approximately 35km <strong>of</strong>f the Tanzanian coast. This area is located in the mouth <strong>of</strong> the<br />

Rufiji delta, and is therefore heavily influenced by the outflow from this major river<br />

system. It is also affected by the East African Current and both the north-eastern and<br />

south-western monsoons. The NE monsoon (Kaskazi) runs from November to March and<br />

brings strong northerly winds, which is followed later in the year by a period <strong>of</strong> heavy<br />

rains which run until May. The wind direction is then reversed with the coming <strong>of</strong> the SE<br />

monsoon (Kusi) which blows from June to October and brings steady winds and good<br />

weather. Another period <strong>of</strong> shorter rains also follows this monsoon. The East Africa<br />

current is a major influencing factor on the area, and runs approximately south to north.<br />

The current can flow at between 1 and 4 knots, depending on physical conditions, water<br />

depth and season.<br />

Tides are another important factor in the physical makeup <strong>of</strong> the reserves. Tides in this<br />

region are mixed semi-diurnal, and average spring tidal range is approximately 3-4m,<br />

varying throughout the year. Currents are heavily influenced around the reserves by tidal<br />

state, with slack water negating currents to a negligible amount, and other states<br />

magnifying them to a maximum <strong>of</strong> 2-3kts in some cases. There is some evidence to<br />

suggest that tides were exceptionally high throughout January and February 2009, to the<br />

extent that the islands were washed over in parts. These high tides are almost certainly<br />

responsible for the morphology <strong>of</strong> the steep beaches that characterise the two smallest<br />

islands. Low tides expose shallow reef flat and sea grass areas to view around both<br />

Shungimbili and Mbarakuni <strong>Island</strong>s.

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