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Side 3
This memorable discovery , in disclosing , by the elevations and depressions of
the barometric column , what was passing in the more elevated regions of the
atmosphere , largely extended our knowledge of this element . It should be
further ...
This memorable discovery , in disclosing , by the elevations and depressions of
the barometric column , what was passing in the more elevated regions of the
atmosphere , largely extended our knowledge of this element . It should be
further ...
Side 10
... the region of calms , the parts of the oceans swept by devastating storms at
particular seasons , and the laws of storms , has saved innumerable lives and
much property ; and by pointing out the quickest routes to be followed , has
shortened ...
... the region of calms , the parts of the oceans swept by devastating storms at
particular seasons , and the laws of storms , has saved innumerable lives and
much property ; and by pointing out the quickest routes to be followed , has
shortened ...
Side 33
This horary oscillation of the barometer is masked in Great Britain by the frequent
fluctuations to which the atmosphere is subjected in these regions . It may ,
however , be detected by taking the means of a series of hourly observations ...
This horary oscillation of the barometer is masked in Great Britain by the frequent
fluctuations to which the atmosphere is subjected in these regions . It may ,
however , be detected by taking the means of a series of hourly observations ...
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 38
Such corrections , when found , serve an important end , especially in tropical
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 ...
Such corrections , when found , serve an important end , especially in tropical
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 ...
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advancing 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 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 storm 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 | Harvard University |
| Digitalisert | 25. mar 2008 |
| Lengde | 371 sider |
| Eksporter sitat | BiBTeX EndNote RefMan |