
Currents run for six whole
months, each way. If a vessel happens to be at the northern extremity of this
islands it is
no great matter, for then it is only carried to Cochin, on the coast of India, or
thereabouts, about a 150 leagues distance, or to some of the islands on that coast. But if
they cannot make the islands of Ceylon, they are carried to Sumatra, a distance of about
500 leagues; and if ill-luck has it that these currents carry them away at the close of
the monsoons, and before they make land anywhere, they are caught in the other current, as
often happens, they are infallibly lost, as I have seen in a number of cases, when they
were expecting to make land every night, and were without water and provisions. If the
current carries them to the west, they are borne straight to the Arabian coast, which is
much further off than that of Sumatra, but most often they are dead before they get
there".
Francois Pyrard, Maldives, 1602 -
1607.
The
currents of the Maldives are notorious for their strength. For this reasons early traders
in the Indian Ocean were extremely cautious when in the Maldives region. Many ships
by-passed the Maldives to the North and South when they had no reason to visit, others
took on local pilots to steer them through the maze of reefs and their treacherous
currents.
The exposure of the Maldives to the
vast Indian Ocean ensures that an immense body of water is constantly flowing across the
plateau on which these Atolls are built. Ocean currents are largely influenced by the
direction of the trade winds and are of great strength. Currents in the channels near
Male' have been recorded at 4 knots or more. Inside the Atoll, current speed are more
settled and leisurely dives are more than norm. Tidal currents, which flow according to
the height of the tide and the direction of the prevailing winds, are said to be much
weaker than oceanic currents, though they cause velocity variations in the flow.
Early Arab navigators studied the
patterns of these oceanic and tidal currents to help them determine their position. When
in the vicinity of the Maldives they observed changes in current direction and surface
patterns as the ocean's waters confronted the great underwater barriers of the Maldive
archipelago.
On the eastern side of Male' Atoll,
currents predominantly flow into the Atoll when the North-East monsoon is firmly
set and
flow outside during the South-West monsoon. The opposite applies to the western side of
the Atoll. This is by no means the rule, as changes in wind direction and tides can offset
the influence of the oceanic currents. If the winds ease off for a few days, then currents
are more likely to flow both in and out of the channels.
During the seasonal transition months
of April and November, when the wind direction and oceanic currents are less predictable,
current is more likely to be influenced by the tides and similarly flow both in and out of
the channels.
At Atoll passages, current streams
can be quite irregular due to the islands, reefs and sandy shoals. Most Dhoani
captains
show great skill in reading the direction of the current and take great pride in their
knowledge of the ocean. If you ask: "Oi Othee Kon Thaakah" (which direction is
the current going?), they will usually wave their hand and say: "Mi Athah" (this
way), or "Eh Athah" (that way)
Usually they can tell the current
direction by the tiny wave patterns on the surface. If there is no wind, the current forms
ripples that bend around stationary objects, like the reef, in the direction of flow. The
captains can also tell current direction by the shape of the ripples and the movement of
the Dhoani. If the current is flowing against the wind, then the surface appears more
choppy than if the current is flowing in the same direction as the wind. If there is very
little, or no current, and the captains don't know its direction, they will usually guess
one way or the other, otherwise lose face. For this reason, it is always advisable for the
dive master to enter the water and check if in doubt. It is better to be sure, and dive on
the best point, than miss the point altogether.

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