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The China Sea directory - Sabrizain.org

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CHAP. III.] WINDS AND WEATHER. 153<br />

directly on shore ;<br />

north-westers, with few exceptions, are the only winds<br />

that blow with violence. Westward of the outlying islands the winds are<br />

from S.S.E. to S.W. <strong>The</strong> rainy season ends in August.<br />

South of the Equator.—From October to April the N.W. monsoon<br />

of the Indian Ocean prevails on the west coast of Sumatra south of<br />

the equator, and is ushered in by thunderstorms and heavy rain. Land<br />

and sea breezes are occasionally experienced, and bad weather with rain<br />

and heavy squalls occur at night. Near the equator the winds are<br />

variable with frequent calms.<br />

During the period from May to September the S.E. trade wind prevails<br />

on the west coast south of the equator, and blows from S.S.13. to S.S.W.<br />

with fine weather. In this season N.W. winds with bad weather are<br />

occasionally experienced at full and change of the moon. Land and sea<br />

breezes occasionally blow in May and September.<br />

Cyclones, occur in the South Indian Ocean between the months of<br />

November and April, but none are recorded as being met with on the west<br />

coast of Sumatra. <strong>The</strong> nearest approach is one noted in November 187l,<br />

at about 100 miles S.W. of the Pagi islands. In July the same year (a<br />

most unusual period) one is recorded at 300 miles westward of Siberut<br />

strait, thence taking the usual westerly direction. No others are recorded<br />

within 500 miles of the coast. <strong>The</strong>y are not unknown at the Keeling<br />

islands.* See page 226.<br />

CURRENTS.—On the west coast of Sumatra the current is influenced<br />

greatly by the winds, and seldom runs to the northward, in either<br />

monsoon, except when the wind is blowing strong from southward. When<br />

N.W. winds prevail, the current runs with the wind to the S.E., and it<br />

generally sets in this direction along the coast in both monsoons particu-<br />

larly in north latitude, but seldom exceeds 12 to 18 miles a day. To the<br />

northward of the equator, when the current is setting to the southward<br />

betwixt the coast and the islands, it is frequently at the same time running<br />

to the northward in the open sea, far outside of them.<br />

In October, November,, and December, it is often tedious getting to the<br />

northward, particularly from the equator to Aehi head, for baffling N.W.<br />

winds and southerly currents are often found to extend a considerable dis-<br />

tance from the coast in these months, particularly in the channels among the<br />

large islands in the offing, where the current sets to the South and S.W.<br />

but in June and July, between Analabu and Achi head, the current has<br />

been found to set to the N.W. from 20 to 30 miles per day.<br />

To the southward of the equator, when at times the southerly winds<br />

blow with considerable strength from June to October, a drain of current<br />

is impelled to the northward, at which time it is difficult to work to the<br />

southward along the coast.<br />

* See A'lmiraltj- wind and cureent charts.

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