rge extent of water before they reach the coasts of the United States.
During the whole of this travel, these thirsty winds are drinking their fill from the sea, and by the time they reach Portland or Boston, they are heavily laden with moisture, which they now begin to let down again upon the land.
Hence, those long, gloomy, rainy, rheumatic, easterly storms, that prevail along our coast in the fall and winter months.
The reader has now only to take up the west wind, as it leaves the Pacific Ocean, as a wet wind, and follow it across the American continent, and see how dry the mountains wring it before it reaches the Atlantic, to see why it should bring us fair weather.
The change was very curious to us at first, until we became a little used to it.
Another change was quite remarkable, and that was the great difference in temperature which we experienced with reference to latitude.
Here we were, in midwinter, or near it, off the south coast of Spain, in latitude 36°, nearly t