The Philosophy of Storms

afternoon annulus appear atmosphere Barbadoes barom barometer began blowing breeze Brunswick tornado calm caloric of elasticity Cape Hatteras cause central line centre changed round Châtenay cloud cold commenced condensation continued descend dew point direction distance earth Espy Espy's facts fall feet fell Franklin Institute Gulf stream hail half past heat heavy gale height Hollidaysburg hundred yards hurricane inches increased Island latent caloric light meteor Meteorology middle midnight miles moderate morning mountain move nearly night noon north east north west o'clock observations outwards passed phenomena Philadelphia produced Professor rain Redfield region rise says ship shower side snow south east south west specific gravity spout squalls storm strong gales surface temperature theory thermometer thunder tion tornado trees tricity upmoving upper current upward motion vapor veered velocity violent volcano vortex weather whirlwind whole wind blew wind changed wind N. E.