The Boy Travellers in the Far East, Part Second: Adventures of Two Youths in a Journey to Siam and Java; With Descriptions of Cochin-China, Cambodia, Sumatra and the Malay Archipelago — John Shaqi
The Boy Travellers in the Far East, Part Second: Adventures of Two Youths in a Journey to Siam and Java; With Descriptions of Cochin-China, Cambodia, Sumatra and the Malay ArchipelagoKnox, Thomas Wallace
General
The Boy Travellers in the Far East, Part Second: Adventures of Two Youths in a Journey to Siam and Java; With Descriptions of Cochin-China, Cambodia, Sumatra and the Malay Archipelago
Knox, Thomas Wallace
East Indies -- Description and travel -- Juvenile literature; Java (Indonesia) -- Description and travel -- Juvenile literature; Thailand -- Description and travel -- Juvenile literature
"In studying about the trade-winds and the monsoons, I find that they do
not blow directly north or directly south, as we might suppose they
would if they came in to fill up the vacancy caused by the rising of the
heated air. North of the equator the trade-winds blow from the
north-east, and south of it they are from the south-east. The
inclination to the east is caused by the rotary motion of the earth from
east to west. The earth slips from under the wind while turning on its
axis, and it is really the earth that makes the slope of the wind, and
not the wind itself. Something like it may be seen when a boat crosses a
river. The boatman may try to pull straight across, but if he does so
the current carries him down, and he is unable to land opposite his
starting-point. The only way he can do so is by going obliquely against
the stream.
"The monsoons get their direction in the same way as the trade-winds get
theirs; with this difference, that the south-west monsoon starts near
the equator, and not in the southern hemisphere, like the south-east
trade-wind. The rotary motion of the earth is greater at the equator
than it is in the northern latitudes, and so the wind gets a westerly
inclination instead of an easterly one, as in the case of the
trade-wind. Some of the scientific men say that the north-east monsoon
is not a monsoon at all, but only the north-east trade-wind taking its
regular course, which has been disturbed by the more powerful wind from
the south-west."
"Very good," remarked the Doctor, when Frank read what he had written.
"I am a little fearful, however, that it will not be understood by
everybody, and so we will drop the dry subject and think of something
easier."
The boys admitted that the topic was a dry one, but nevertheless it was
interesting; and they thought they would not be doing their duty in
their journey if they failed to comprehend the great winds that so
materially help or hinder the movements of ships in Asiatic waters.
On their third day from Hong-kong the boys heard with delight that land
was visible. At first it was like a dark cloud on the horizon; but, as
they approached it, the scene changed, and the cloud was resolved into a
tropical shore, backed by a line of hills in the distance. The steamer
headed for a little promontory, and by-and-by a light-house was revealed
that marked the entrance of the river which they were to ascend.
A boat came out from the mouth of the river, and a pilot boarded the
steamer. He was a weather-beaten Frenchman, who had lived more than
twenty years in Cochin China, and was thoroughly familiar with the
channel of the river, or rather of its various channels. The Mekong
empties into the China Sea, very much as the Mississippi discharges into
the Gulf of Mexico; it has several mouths, and the whole lower part of
its course is divided into canals and bayous, that are very convenient
for the natives in the matter of local navigation.
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