mate of all parts over which the winds
extend. The same monsoon blows over the eastern countries of the
continent, but the insular character of Japan and the proximity of the
warm current on both sides of the islands give to the winds which prevail
a character which they do not possess on the continent. During the greater
part of September the northern wind blows, which brings a colder
temperature, condensing the moisture contained in the atmosphere. This
month is therefore generally a rainy month. Gradually the atmosphere
becomes more dry, and the beautiful autumn and early winter follow in
course.
The winter is very different in the different parts. On the east coast the
temperature is very moderate. Even as far north as Tokyo the snow rarely
falls to a depth of more than a few inches, and then rapidly melts away.
Ice seldom forms to a thickness, even on protected waters, to permit
skating. In all this region, however, snow covers the high mountains.
On the west coast of the Main island the conditions are very different.
The winds of the continent take up the moisture of the Japan sea, and
carry it to the west coast, and then, coming in contact with high ranges
of mountains which run down the middle of the island, impart their
moisture in the form of rain in summer, and snow in winter. These
circumstances produce extraordinary falls of snow on the west coast. This
is particularly true of the provinces of Kaga, Noto, Etchu, Echigo, and
even farther north, especially in the mountainous regions. In the northern
part of these districts the snow is often as much as twenty feet deep
during the winter months. The inhabitants are obliged to live in the
second stories of their houses and often find it necessary to make steps
from their houses out to the top of the snow. One effect of these deep
snows is to cover up with a safe protection the shrubs and tender plants
which would otherwise be exposed to the chilling winds of winter. By this
means the tea-shrub and the camellia, which could not withstand the open
winter winds, are protected so as to grow luxuriantly.
The southern islands are materially warmer than the Main island. The
tropical current together with the warm sunshine due to their low
latitude, immerses them in a moist and warm atmosphere. Their productions
are of a sub-tropical character. Cotton, rice, tobacco, sugar, sweet
potatoes, oranges, yams, and other plants of a warm latitude, flourish in
Kyushu and S
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