Handy Book of MeteorologyWilliam Blackwood, 1868 - 371 sider |
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Side 3
... 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 study of the science . 7. The ...
... 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 study of the science . 7. The ...
Side 33
... regions . It may , however , be detected by taking the means of a series of hourly ob- servations conducted for some time . The results show two maxima occurring from 9 to 11 A.M. and from 9 to 11 P.M. , and two minima occurring from 3 ...
... regions . It may , however , be detected by taking the means of a series of hourly ob- servations conducted for some time . The results show two maxima occurring from 9 to 11 A.M. and from 9 to 11 P.M. , and two minima occurring from 3 ...
Side 36
... regions of the atmosphere from the wave of heat which has been going on for some hours . But as the vapour becomes more equally diffused and the air more saturated , evaporation proceeds more languidly ; the air becomes also more ...
... regions of the atmosphere from the wave of heat which has been going on for some hours . But as the vapour becomes more equally diffused and the air more saturated , evaporation proceeds more languidly ; the air becomes also more ...
Side 38
... regions where the daily variation is great ; but they may also be , nay , frequently are , applied in cases where they are not applicable , thus leading to a good deal of confusion . mean . 74. The legitimate use of these corrections is ...
... regions where the daily variation is great ; but they may also be , nay , frequently are , applied in cases where they are not applicable , thus leading to a good deal of confusion . mean . 74. The legitimate use of these corrections is ...
Side 39
... regions of the atmosphere in the same direction . Hence , in so far as the dry air of the atmosphere is concerned , the atmospheric pressure will be least in the summer and greatest in the winter of each hemisphere . But the production ...
... regions of the atmosphere in the same direction . Hence , in so far as the dry air of the atmosphere is concerned , the atmospheric pressure will be least in the summer and greatest in the winter of each hemisphere . But the production ...
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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