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Side 37
The daily variation is less in winter when the temperature is low , than it is in
summer , unless when rains in summer occur to diminish it . Thus , at St
Petersburg , the variation in January is only 0 . 009 inch , whereas in OF THE
ATMOSPHERE .
The daily variation is less in winter when the temperature is low , than it is in
summer , unless when rains in summer occur to diminish it . Thus , at St
Petersburg , the variation in January is only 0 . 009 inch , whereas in OF THE
ATMOSPHERE .
Side 38
In the generally wet climate of Great Britain there appears , from Glaisher ' s
Table for Greenwich , to be little difference between the winter and the summer
months . 73 . The mean pressure at Calcutta of the three Januarys ( 1861 - 63 ) ,
as ...
In the generally wet climate of Great Britain there appears , from Glaisher ' s
Table for Greenwich , to be little difference between the winter and the summer
months . 73 . The mean pressure at Calcutta of the three Januarys ( 1861 - 63 ) ,
as ...
Side 39
When it is summer in the one hemisphere , it is winter in the other . In the
hemisphere where summer prevails , the whole air , being warmer than in the
other hemisphere , expands both vertically and laterally . As a consequence of
the lateral ...
When it is summer in the one hemisphere , it is winter in the other . In the
hemisphere where summer prevails , the whole air , being warmer than in the
other hemisphere , expands both vertically and laterally . As a consequence of
the lateral ...
Side 40
978 inches in July ( winter ) , the difference being 0 . 234 inch . The large annual
variation at Calcutta is caused jointly by the great heat in July , and by the heavy
rains which accompany the south - west monsoons at this season ; while in ...
978 inches in July ( winter ) , the difference being 0 . 234 inch . The large annual
variation at Calcutta is caused jointly by the great heat in July , and by the heavy
rains which accompany the south - west monsoons at this season ; while in ...
Side 41
countries , and the large amount of moisture in the air in winter , and the heavy
rainfall , which , by setting free great quantities of latent heat , still further
augments and accelerates the outflow . 80 . The variations in mean pressure are
very ...
countries , and the large amount of moisture in the air in winter , and the heavy
rainfall , which , by setting free great quantities of latent heat , still further
augments and accelerates the outflow . 80 . The variations in mean pressure are
very ...
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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 |