Handy Book of MeteorologyWilliam Blackwood, 1868 - 371 sider |
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Side 49
... region , an ascending current takes place . But as moist air ascends into the upper regions of the atmosphere , it is cooled below the point of saturation , con- densation follows , and rain is precipitated . In the act of condensation ...
... region , an ascending current takes place . But as moist air ascends into the upper regions of the atmosphere , it is cooled below the point of saturation , con- densation follows , and rain is precipitated . In the act of condensation ...
Side 50
... region of calms and of constant rains , which will be re- ferred to further on . 103. The crowding together of the isobarometric lines in the south and east of Asia is caused by the vapour which the summer monsoon brings to these regions ...
... region of calms and of constant rains , which will be re- ferred to further on . 103. The crowding together of the isobarometric lines in the south and east of Asia is caused by the vapour which the summer monsoon brings to these regions ...
Side 51
... region to upwards of 30.400 inches . It is here that at this season the greatest degree of terrestrial cold known to ... regions of low pressure , -lying respectively to the east , the south , the south - east , and the west . 106. This ...
... region to upwards of 30.400 inches . It is here that at this season the greatest degree of terrestrial cold known to ... regions of low pressure , -lying respectively to the east , the south , the south - east , and the west . 106. This ...
Side 52
... region is given only hypothetically . It is , however , probably correct , since there is no mountain barrier ... regions of South Africa and South America . The influence which this peculiar distribution of atmospheric pressure ...
... region is given only hypothetically . It is , however , probably correct , since there is no mountain barrier ... regions of South Africa and South America . The influence which this peculiar distribution of atmospheric pressure ...
Side 53
... region is due to the saturated state of its atmosphere and to the copious rainfall resulting from it . The flow of the ... regions -the one north and the other south of the equator - passing completely round the globe as broad belts of ...
... region is due to the saturated state of its atmosphere and to the copious rainfall resulting from it . The flow of the ... regions -the one north and the other south of the equator - passing completely round the globe as broad belts of ...
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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