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
The islanders like the Msika to open with showers strong enough to bind
the land, but not so violent as to carry off the manure deposited by the
year’s decayed vegetation. After this the water should fall in heavy
ropy torrents, with occasional breaks of sunshine and fine weather; when
this lasts thirty days, and is succeeded by frequent showers, good crops
are expected. The downfall is heavier in the interior of the island than
about the city, which, situated upon a point, escapes many a drenching.
It must, however, be borne in mind that the phenomena of the rains, like
those of the sea and air, are essentially irregular. In some seasons
there will be only half-a-dozen rainy afternoons; in others as many
rainy mornings. There are years of great drought, and there are seasons
when the sun does not appear for six weeks in succession. Usually heavy
rain is not expected after 11 A.M., and showers are rare after 2 P.M. As
I subsequently remarked in the east African interior—the Fluminenses of
the Brazil still preserve the tradition—there is a curious regularity
and periodicity in the hours of downfall, often extending over many
days. This phenomenon may have done much towards creating the ‘rain-
doctor.’
During the Msika the horizon is obscured, dangerously indeed for ships:
the wind veers round to every point of the compass; the sky is murky and
overcast; huge purple nimbi, like moving mountains, float majestically
against the wind, showing strong counter-currents in the upper aërial
regions. From afar the island appears smothered in blue mist, and often
the cloudrock splits into two portions, one of which makes for the
coast. Even during the rare days of sunshine the distances, owing to the
continuous humidity, are rarely clear, and the exhalations make
refraction extensive. A high tension of vapour is the rule. For the
first three hours after sunrise the land is often obscured by ‘smokes,’
a white misty fog, often deepening to a drizzling rain; this lasts until
10 A.M., about which time the sea-breeze begins to blow.
Public-domain text, read in full here on John Shaqi.
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