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Side 11
In Europe , however , stormy weather is accompanied by a diminution in the
atmospheric pressure , the centre of which , after traversing more or less of the
Atlantic , arrives on the coast of Europe . The existence of this diminished
pressure is ...
In Europe , however , stormy weather is accompanied by a diminution in the
atmospheric pressure , the centre of which , after traversing more or less of the
Atlantic , arrives on the coast of Europe . The existence of this diminished
pressure is ...
Side 29
The amount of this correction is determined by the height of the place above the
sea ; the atmospheric pressure and temperature at the time ; and the distance
from the centre of gravity of the earth , which is known from the latitude and height
...
The amount of this correction is determined by the height of the place above the
sea ; the atmospheric pressure and temperature at the time ; and the distance
from the centre of gravity of the earth , which is known from the latitude and height
...
Side 45
In the centre of Africa , from which there are no observations , and where ,
consequently , the lines are hypothetical , they are made dotted lines . 90 . MEAN
ATMOSPHERIC PRESSURE FOR JULY . — It will be seen from Plate I . ,
representing ...
In the centre of Africa , from which there are no observations , and where ,
consequently , the lines are hypothetical , they are made dotted lines . 90 . MEAN
ATMOSPHERIC PRESSURE FOR JULY . — It will be seen from Plate I . ,
representing ...
Side 46
The observations showing this depression near its centre are scanty ; but as the
North American observations show clearly a decreasing pressure from the coast
towards the interior of the continent till it falls to 29 . 686 inches at Great Salt Lake
...
The observations showing this depression near its centre are scanty ; but as the
North American observations show clearly a decreasing pressure from the coast
towards the interior of the continent till it falls to 29 . 686 inches at Great Salt Lake
...
Side 51
An extraordinary excess of atmospheric pressure extends over Central and
Northern Asia , rising in the centre of that region to upwards of 30 . 400 inches . It
is here that at this season the greatest degree of terrestrial cold known to exist
takes ...
An extraordinary excess of atmospheric pressure extends over Central and
Northern Asia , rising in the centre of that region to upwards of 30 . 400 inches . It
is here that at this season the greatest degree of terrestrial cold known to exist
takes ...
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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 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 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
Side 184 - That rises upward always higher, And onward drags a labouring breast, And topples round the dreary west, A looming bastion fringed with fire.
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 |