The Philosophy of StormsC.C. Little and J. Brown, 1841 - 552 pagina's |
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afternoon Alcmene annulus appears ascending column atmosphere Barbadoes barom barometer blowing borders breeze Brunswick tornado calm Cape Hatteras cause central line centre changed round Châtenay cloud cold commenced condensation cone continued descend dew point diameter diminished pressure direction distance earth Espy facts fall feet fell force Franklin Institute hail half past heat 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 reached Redfield region remarkable 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 water-spout weather whirlwind wind blew wind changed