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Side vi
The subject of STORMS is more specially discussed , as being , from the practical
application of the results of the inquiry to the prediction of storms , and
consequently to the saving of life and property , a question the importance of
which it ...
The subject of STORMS is more specially discussed , as being , from the practical
application of the results of the inquiry to the prediction of storms , and
consequently to the saving of life and property , a question the importance of
which it ...
Side 16
If the mercury be not pure the density will be different , and consequently the
length of the column will not be the same as that of a barometer in which pure
mercury has been used ; and , moreover , impurities will soon appear in the
mercury ...
If the mercury be not pure the density will be different , and consequently the
length of the column will not be the same as that of a barometer in which pure
mercury has been used ; and , moreover , impurities will soon appear in the
mercury ...
Side 23
This stalk terminates a little below the upper level of the mercury , a , and its
upper end is therefore exposed to no more downward pressure than that of the
mercury above it ; consequently there is an excess of upward pressure from the ...
This stalk terminates a little below the upper level of the mercury , a , and its
upper end is therefore exposed to no more downward pressure than that of the
mercury above it ; consequently there is an excess of upward pressure from the ...
Side 30
... pushed the air up 31 feet above places at a height of 874 feet ; and the
atmospheric pressure being thus increased by the weight of the 31 feet raised
above them , and consequently pressing on them , the correction for height
becomes less .
... pushed the air up 31 feet above places at a height of 874 feet ; and the
atmospheric pressure being thus increased by the weight of the 31 feet raised
above them , and consequently pressing on them , the correction for height
becomes less .
Side 32
But in reducing to sea - level the mean barometric observations made at high
situations during a number of years , and where consequently the mean
temperature of the air is closely approximated to , the more accurate methods of
reducing ...
But in reducing to sea - level the mean barometric observations made at high
situations during a number of years , and where consequently the mean
temperature of the air is closely approximated to , the more accurate methods of
reducing ...
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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
Populære avsnitt
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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 |