Handy Book of Meteorology |
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Side 7
The law of the diffusion of vapour through the air , its influence on the barometric
pressure , and its relations to the other constituents of the atmosphere , are
among the least satisfactorily determined questions in meteorology . Since this ...
The law of the diffusion of vapour through the air , its influence on the barometric
pressure , and its relations to the other constituents of the atmosphere , are
among the least satisfactorily determined questions in meteorology . Since this ...
Side 29
Now , since at the equator gravity diminishes least rapidly with the height , the air
of the atmosphere will at any given height weigh more there than anywhere else
on the globe at the same height as compared with what it would do at sea - level
...
Now , since at the equator gravity diminishes least rapidly with the height , the air
of the atmosphere will at any given height weigh more there than anywhere else
on the globe at the same height as compared with what it would do at sea - level
...
Side 34
109 · Thus the greatest maximum occurs at Calcutta at 9 . 30 A . M . , and the
greatest minimum at 4 . 30 P . M . ; the least maximun at 10 . 30 p . m . , and the
smallest minimum at 3 . 30 A . M . Hence the two maxima occur when the
temperature ...
109 · Thus the greatest maximum occurs at Calcutta at 9 . 30 A . M . , and the
greatest minimum at 4 . 30 P . M . ; the least maximun at 10 . 30 p . m . , and the
smallest minimum at 3 . 30 A . M . Hence the two maxima occur when the
temperature ...
Side 35
... when the deposition of dew is greatest , and before sunrise , 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 ...
... when the deposition of dew is greatest , and before sunrise , 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 ...
Side 36
... at those places where the influence of temperature is most felt and its effects on
the daily barometric pressure least disturbed by large evaporating surfaces , or
by moist winds . Thus the smaller maximum and minimum are apparent in the ...
... at those places where the influence of temperature is most felt and its effects on
the daily barometric pressure least disturbed by large evaporating surfaces , or
by moist winds . Thus the smaller maximum and minimum are apparent in the ...
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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 |