id	author	title	date	pages	extension	mime	words	sentences	flesch	summary	cache	txt
63122	Greely, A. W. (Adolphus Washington)	Geography of the Air			.txt	text/plain	4736	191	52	resulting mean diminution of pressure, and the movement of the air from places of high to places of low pressure, the lower air ascending believes that air flowing into the cyclone from a "high" at the ground through a difference of temperature of the air from the equator to the largely the result of greater density due to low temperature, as is atmospheric pressure, temperature, and wind direction over the whole Marvin, whose successful experiments on wind pressures and velocities the square of the velocity of the wind, expressed in miles per hour; wind in pounds per square foot and of the velocity in miles per hour. hour too high, and for an indicated velocity of 90 miles the lower temperatures, the observations of Regnault as to the pressure of The work of Professor Hazen in charting tornadoes and in determining Geography of the Air. Great attention had previously been given to this subject by	./cache/63122.txt	./txt/63122.txt