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The China Sea directory - Sabrizain.org

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4 MAI/ACCA STRAIT. [chap. I.<br />

the wind. This, however, is not always the case, for at times the current<br />

is found to run obliquely and even contrary to the wind.*<br />

Between the western entrance of Malacca strait and Aroa islands the<br />

general set of the current is to the north-west all the year round, but<br />

near the Malay coast regular tides mostly prevail, except occasionally<br />

during the north-east monsoon, when the current sets to the south-east<br />

along the Malay coast. During the south-west monsoon the current runs<br />

to the westward along the coast of Pedir, whilst it is setting to the<br />

north-eastward between Fulo Rondo and Salang (Junkseylon) island ; at<br />

limes, when the monsoon is light, and veers to the westward, the current<br />

between Pulo Rondo and Junkseylon sets to the southward. Between<br />

Diamond point and the eastern entrance of the strait a tidal influence<br />

prevails close inshore.<br />

From Aroa islands to Carimon islands regular tides prevail throughout<br />

the strait ; the flood sets to the south-east, and the ebb to the north-west,<br />

from 2 to 3^ miles an hour ; the ebb running longer and stronger than<br />

the flood. Near Aroa islands the flood is often weak, and during neaps<br />

there is a constant current setting north-westward.<br />

Near cape Rachada, where the strait suddenly becomes narrowed to 20<br />

miles, the tides run strong, and with eddies during springs. In the ofl[ing<br />

between Water islands and Carimon islands the tides set fair through the<br />

strait, except near Pulo Pisang, when the flood sometimes sets a vessel<br />

towards Carimon islands.<br />

<strong>The</strong> flood setting south-eastward past Carimon islands, meets the flood<br />

setting from the <strong>China</strong> sea through Singapore strait, between the north<br />

end of Little Carimon and Tree island ; after this junction the flood<br />

^usually sets to the southward through Durian strait, but sometimes to the<br />

Jiorthward towards Old Strait. See page 107.<br />

In most parts of Malacca strait the streams run from 2 to 3 hours after<br />

high and low water by the shore. <strong>The</strong> greatest rise and fall is 15 feet.<br />

GENERAL DIRECTIONS.—<strong>The</strong> navigation of Malacca strait<br />

is, with ordinary caution, not dangerous, the channels are mostly spacious<br />

and have good anchorage, but due attention to the set of the currents and<br />

tides is requisite. <strong>The</strong> sailing passage is much facilitated by keeping under<br />

-way at night, for steady breezes then often prevail, calms and faint airs<br />

being experienced during the day ; passages are thus made without<br />

anchoring more than once or twice. <strong>The</strong> passage to the north-west is<br />

generally made in less time than the one to the south-east. Vessels which<br />

* In July and August, a south-westerly current rnnniog in the teeth of the monsoon<br />

at the rate of one to two knots per hour, between Aehi head and Great Nicobar, has<br />

.been reported by several vessels. H.M.S. Rifleman in August 1878, experienced a set<br />

of 2 knots an hour, the wind being S.E., and with a force of 2 to 3.

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