Handy Book of MeteorologyWilliam Blackwood, 1868 - 371 sider |
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Resultat 1-5 av 54
Side x
... passing the place , absolutely of no use ; and it cannot be used in determining the amplitude of the barometer fluctuations accompanying storms and other weather - changes . By this mode of publishing daily ob- servations , a ...
... passing the place , absolutely of no use ; and it cannot be used in determining the amplitude of the barometer fluctuations accompanying storms and other weather - changes . By this mode of publishing daily ob- servations , a ...
Side 2
... passed current from hand to hand , so that there is per- haps no science of which more of the leading facts and infer- ences have been so long incorporated into popular language . 4. Aristotle was the first who collected , in his work ...
... passed current from hand to hand , so that there is per- haps no science of which more of the leading facts and infer- ences have been so long incorporated into popular language . 4. Aristotle was the first who collected , in his work ...
Side 3
... passing in the more elevated regions of the atmosphere , largely extended our knowledge of this element . It should be further remarked that the value of the barometer as an indicator of the weather gave an addi- tional impetus to the ...
... passing in the more elevated regions of the atmosphere , largely extended our knowledge of this element . It should be further remarked that the value of the barometer as an indicator of the weather gave an addi- tional impetus to the ...
Side 53
... passing completely round the globe as broad belts of high pressure . They enclose between them the low pressure of the tropics , through the centre of which runs a narrower belt of ITS DISTRIBUTION OVER THE GLOBE . 53.
... passing completely round the globe as broad belts of high pressure . They enclose between them the low pressure of the tropics , through the centre of which runs a narrower belt of ITS DISTRIBUTION OVER THE GLOBE . 53.
Side 67
... passed the meridian at noon . But in temperate climates during summer the maximum does not take place till from 2 P.M. to 31 P.M. 143. To this general law of the time of its occurrence there are two interesting exceptions . At many ...
... passed the meridian at noon . But in temperate climates during summer the maximum does not take place till from 2 P.M. to 31 P.M. 143. To this general law of the time of its occurrence there are two interesting exceptions . At many ...
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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