Zanzibar; city, island, and coast. Vol. 1 (of 2)Burton, Richard Francis, Sir
History
Zanzibar; city, island, and coast. Vol. 1 (of 2)
Burton, Richard Francis, Sir
Africa, East -- Description and travel; Ethnology -- Tanzania -- Zanzibar; Zanzibar -- Description and travel
Presently appear the rains which have followed the northing sun. The
same observation was made by the Austrian mission on the White River in
N. lat. 4° 30′. On the coast we can distinctly trace their progress. In
1857 the downfall began in Feb. 15, at Usumbara (S. lat. 5°), where the
clouds are massed and condensed by a high plateau, leading to lofty,
snow-capped mountains. In 1854 I found that the rainy season opened at
Berberah of the Somal (N. lat. 10° 25′) on April 15; and in early June
they reach Bombay (N. lat. 18° 53′). Concerning the movement of the wet
season in inner intertropical Africa I have already written in the
Journal of the Royal Geographical Society (xxix. 207).
The heaviest rains at Zanzibar Island begin the wet season about mid-
April, and last 30 to 40 days; they do not end, however, till early
June. Some observers remark that the fall is greatest at low water and
during the ebb-tides of the Syzygies. It is, however, rare to have a
week of uninterrupted rain, as in eastern India and sometimes in the
Brazil. The discharge is exceedingly uncertain. Some years number 85
inches, others 108. During the first eight months of 1857 and the last
four months of 1858, we find a total of 120·21 inches. In 1859 it
reached 167, doubling the average of Bombay (76·55), and nearly trebling
that of Calcutta (56·83). We may compare these figures with those of
Europe and the United States. England has 31·97 inches; France, 25·00;
Central Germany, 20·00; Hungary, 16·93; Boston, 38·19 (about the same at
Beyrut in Syria); Philadelphia, 45·00; and St Louis, Mo., 31·97. Of
these 167 inches (1859), 104·25 fell during the Msika Mku. The number of
wet days ranges from 100 to 130 per annum. According to the people, rain
has diminished of late years; perhaps it is the result of felling
cocoas, and of disforesting the land for cloves. In 1857, the Great
Msika was preceded by a few days of oppressive heat, which ended (March
24) in a highly electrical storm, like those which usher in the rains of
western India, and suddenly the cool S.W. began to blow. For some time
we had daily showers, now from the N.E., then from the S.W., with high
winds and loud thunderings; the rains, however, did not show in earnest
before April 10.
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