Handy Book of MeteorologyWilliam Blackwood, 1868 - 371 sider |
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Side vi
... Pressure over the Globe , " and " The Relation of Atmospheric Pressure to the Tem- perature , " are wholly new , and the Chapter on " Winds is almost altogether new . The intimate connection of temperature with pressure is illustrated ...
... Pressure over the Globe , " and " The Relation of Atmospheric Pressure to the Tem- perature , " are wholly new , and the Chapter on " Winds is almost altogether new . The intimate connection of temperature with pressure is illustrated ...
Side xi
... PRESSURE OF THE ATMOSPHERE , 15 • • III . ATMOSPHERIC PRESSURE , ITS DISTRIBUTION OVER THE GLOBE , IV . TEMPERATURE , HOW OBSERVED AND CALCULATED , V. TEMPERATURE - SOLAR AND TERRESTRIAL RADIATION , VI . THE DISTRIBUTION OF TERRESTRIAL ...
... PRESSURE OF THE ATMOSPHERE , 15 • • III . ATMOSPHERIC PRESSURE , ITS DISTRIBUTION OVER THE GLOBE , IV . TEMPERATURE , HOW OBSERVED AND CALCULATED , V. TEMPERATURE - SOLAR AND TERRESTRIAL RADIATION , VI . THE DISTRIBUTION OF TERRESTRIAL ...
Side xii
... PRESSURE OF THE GLOBE FOR JULY . II . ISOBAROMETRIC LINES SHOWING THE MEAN ATMOSPHERIC PRESSURE OF THE GLOBE FOR JANUARY . III . ISOBAROMETRIC LINES SHOWING THE MEAN ANNUAL ATMOSPHERIC PRESSURE OF THE GLOBE . IV . ISOTHERMAL LINES ...
... PRESSURE OF THE GLOBE FOR JULY . II . ISOBAROMETRIC LINES SHOWING THE MEAN ATMOSPHERIC PRESSURE OF THE GLOBE FOR JANUARY . III . ISOBAROMETRIC LINES SHOWING THE MEAN ANNUAL ATMOSPHERIC PRESSURE OF THE GLOBE . IV . ISOTHERMAL LINES ...
Side 16
... pressure and its great elasticity , air becomes less dense as we ascend , the real height is very much greater , being , it is supposed , about 210 miles . 29. Other fluids may be used in the construction of baro- meters , which , being ...
... pressure and its great elasticity , air becomes less dense as we ascend , the real height is very much greater , being , it is supposed , about 210 miles . 29. Other fluids may be used in the construction of baro- meters , which , being ...
Side 23
... pressure than that of the mercury above it ; consequently there is an excess of upward pressure from the atmosphere which tends to raise the cistern . When the excess of upward pressure is exactly balanced by the weight of the cistern ...
... pressure than that of the mercury above it ; consequently there is an excess of upward pressure from the atmosphere which tends to raise the cistern . When the excess of upward pressure is exactly balanced by the weight of the cistern ...
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America antisolar point ascending Asia Atlantic atmospheric pressure average barometer blow Britain calm causes centre charts cirrus cirrus cloud cistern climate cloud coast cold colder column condensed continent Crown 8vo daily dew-point diminished direction dry air earth earth's surface east Edition electricity equator equatorial current Europe evaporation falls Fcap feet flow globe greater heat height hemisphere Hence high pressure higher hour humidity hygrometer Iceland inch of mercury inches increase Indian Ocean isobarometric lines January John Herschel July latitudes low pressure lower Mauritius maximum mean temperature mercury Meteorological meter miles moisture monsoon months northern northern hemisphere Norway observations occur ocean Orkney perature Plate polar current polarisation prevail Professor rain rainfall regions rises round Scotland season snow soil St Petersburg storm summer temperature terrestrial radiation thermometers tion tropics tube upper currents vapour vols weather wind winter Yakutsk