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CHAPTER VI.
TRADE-WINDS—STORMS—THEIR EFFECTS—MONSOONS—THEIR VALUE—LAND AND SEA BREEZES—EXPERIMENTS HURRICANES—THOSE OF 1831—ROTATORY STORMS—THEIR TERRIBLE EFFECTS—CHINA SEAS—HURRICANE IN 1837—WHIRLWINDS—WEIGHT OF ATMOSPHERE—VALUE OF ATMOSPHERIC CIRCULATION—HEIGHT OF ATMOSPHERE.

BEFORE proceeding to speak of the power and the dreadful effects of wind, it is necessary to say a word or two about the trade-winds.

It is supposed that the "trades" derived their name from the fact of their being favourable to navigation, and, therefore, to trade. They consist of two belts of wind, one on each side of the equator, which blow always in the same direction.

In the last chapter it was explained that the heated atmosphere at the equator rises, and that the cooler atmosphere from the poles rushes in to supply its place. That which rushes from the south pole is, of course, a south wind, that from the north pole a north wind; but, owing to the Earth's motion on its axis from west to east, the