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- W2899187145 abstract "SUMMARY Geomorphologically, the Sar Uanle coast (0°29′48''S-42°25′30''E, 20 km South of Chisimaio) is successively composed of the reef edge (visible only at lowest syzygyal tides), a back-reef channel about 150 m wide, a rocky platform 40–70 m wide, a sandy beach 30–40 m wide, a dune 40 m wide and 7–10 m above mean sea level, a retrodunal plain and, finally, a rocky wall, an ancient pleistocenic coastline. According to a widely used classification, the climate in the Sar Uanle area is arid-tropical of the V 4 type, as is typical of the savannah belts, but modified along the coast where a marked thermic and hygrometric uniformity reigns throughout each and every year. Our data, collected during the course of five missions, substantially agree with those collected by FANTOLI (1965) at Chisimaio over a period of several years. The seasonal alternation is characterized by the two monsoons (NE- SW from December to March and SW-NE from April to November) with two intermediate periods of weak, irregular winds (Tanga Mbili) and two rainy periods (Gu—the heavier of the two—April-June and Oer, September-November). The temperature, relative humidity, atmospheric pressure, wind speed and direction, irradiation and precipitation were recorded during the course of each mission. All the variables show very weak excursions and very constant periodic fluctuations. In particular, the wind direction changes very regularly during the course of the day though changing in extent and bearing according to the time of year. The tide is constantly of the semidiurnal type, with a diurnal inequality of about 20–35% and inundates all the beach only during the extreme high spring tides. The tidal range does not usually exceedes 3.2 m." @default.
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- W2899187145 date "1977-01-01" @default.
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- W2899187145 title "RESEARCHES ON THE COAST OF SOMALIA. THE SHORE AND THE DUNE OF SAR UANLE" @default.
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- W2899187145 doi "https://doi.org/10.1080/03749444.1977.10736851" @default.
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