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Side 35
... when evaporation and the absolute quantity of vapour in the atmosphere is
least . 68 . Thus , taking both causes into consideration , the maximum in the
forenoon is brought about by the rapid evapora, tion arising from the dryness of
the air ...
... when evaporation and the absolute quantity of vapour in the atmosphere is
least . 68 . Thus , taking both causes into consideration , the maximum in the
forenoon is brought about by the rapid evapora, tion arising from the dryness of
the air ...
Side 36
tion arising from the dryness of the air and the increasing temperature , together
with the overflow of air in the upper regions of the atmosphere from the wave of
heat which has been going on for some hours . But as the vapour becomes more
...
tion arising from the dryness of the air and the increasing temperature , together
with the overflow of air in the upper regions of the atmosphere from the wave of
heat which has been going on for some hours . But as the vapour becomes more
...
Side 60
tion it is hung horizontally ; then as the temperature rises the whole column
moves along the scale , but when it begins S TORITVE NATURBILDUN Fig . 13 .
to fall the detached portion is left behind at the point to which it had been pushed
...
tion it is hung horizontally ; then as the temperature rises the whole column
moves along the scale , but when it begins S TORITVE NATURBILDUN Fig . 13 .
to fall the detached portion is left behind at the point to which it had been pushed
...
Side 307
tion , and the barometer is said not to be perceptibly affected by it . A low bank of
dark cloud is seen in the horizon , which rapidly increases , and before the
spectator is aware the storm bursts upon him , wrapping everything in midnight ...
tion , and the barometer is said not to be perceptibly affected by it . A low bank of
dark cloud is seen in the horizon , which rapidly increases , and before the
spectator is aware the storm bursts upon him , wrapping everything in midnight ...
Side 370
... tion of a " rainy day , " 401 . Sympiesometer , 44 . Synchronous or synoptic
charts indispensable in studying storins , 498 ; their construction , 499 . Ventnor
as a winter and spring resort , 157 . 370 INDEX .
... tion of a " rainy day , " 401 . Sympiesometer , 44 . Synchronous or synoptic
charts indispensable in studying storins , 498 ; their construction , 499 . Ventnor
as a winter and spring resort , 157 . 370 INDEX .
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America amount appear Asia Atlantic atmosphere atmospheric pressure average barometer becomes blow Britain calm causes centre changes charts climate cloud coast cold column compared consequently continued countries course daily diminished direction earth east Edition effect electricity Europe evaporation examined falls feet flow force frequently give given greater greatest heat height Hence higher hour Illustrations important inches increase indicate influence January July land least less light lines lower maximum mean mean temperature mercury Meteorological miles months nearly night northern observations occur ocean passed period Plate position pressure prevail Professor quantity radiation rain rainfall regarded regions relation rises round scale Scotland season seen side soil storms summer surface Table temperature thermometers tion tube upper vapour vols weather whole wind winter
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Bibliografisk informasjon
| Tittel | Handy Book of Meteorology |
| Forfatter | Alexander Buchan |
| Utgave | 2 |
| Utgiver | W. Blackwood and Sons, 1868 |
| Original fra | Oxford University |
| Digitalisert | 20. sep 2006 |
| Lengde | 371 sider |
| Eksporter sitat | BiBTeX EndNote RefMan |