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Winds and Weather:
A
central area of high pressure dominates the South Atlantic,
and both the wind and current systems (see diagrams) circulate
in an anti-clockwise direction. The southeast trade winds
flow around this high which is generally centered between
20deg. to 28deg. S, and blows with consistency from S.S.E.
on the African side to almost east close to the North Brazilian
coastline.
In
summer the southeast trades are normally encountered a few
days sail NW of Cape Town, and are often heralded by a day
of light fluffy clouds. Line squalls followed by stronger
winds and sometimes heavy rain, are often encountered in
mid ocean, and towards the North Eastern Brazilian coastline.
If
headed to the Caribbean the Doldrum belt is narrow, with
torrential rain, and will be encountered close to the mouth
of the Amazon River.
Fog,
or sea fog, are very common in the Cape Town area and northwards,
in the autumn months with very limited visibility.
Further
North, towards the deserts of Namibia, fog often occurs
in any season, the worst conditions develop at night, when
the overlaying air is cooled, as it encounters the cold
Benguela Current.
Inshore,
in the summer months, the fog usually clears by noon.
Sea
and swell:
Moderate
to heavy swell from between SW and NW, depending on wind
strength and direction occurs off the Cape area. Very rough
and confused seas are common in winter, occurring anything
up to 25deg. S, right across the South Atlantic.
Heavy
seas are rare north of 25deg. S, but can develop during
violent squalls. North of latitude 10deg. S, the sea is
slight in summer between SE and SW.
Changes in direction and strength of the SE trades, can
cause landing and anchorage problems at the South Atlantic
islands.
About
3 days in any summer month "rollers" occur at St Helena,
Ascension and Fernando de Noronha islands making landing
almost impossible.
For
full details with photos, charts, diagrams, etc., see "Cape
to Caribbean Cruising Notes" by Tony Herrick http://www.cruiser.co.za/tony.asp
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