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Side
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
... 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 . Let H be the height in feet of a column of air at the given
temperature ...
... 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 . Let H be the height in feet of a column of air at the given
temperature ...
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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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 |