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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 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 53
... which determines the region of calms and constant rains , is peculiar in this ,
that it does not lie parallel to the equator , as might have been expected , but
slanting from Tamatave in Madagascar , 18° S . lat . , to the coast of Sumatra , in 5
° S ...
... which determines the region of calms and constant rains , is peculiar in this ,
that it does not lie parallel to the equator , as might have been expected , but
slanting from Tamatave in Madagascar , 18° S . lat . , to the coast of Sumatra , in 5
° S ...
Side 67
At many places in tropical countries it occurs about noon , or sometimes a little
earlier , when the temperature at the coast is lowered by the seabreeze , which
begins to blow before noon , and during the rainy season the temperature at this
...
At many places in tropical countries it occurs about noon , or sometimes a little
earlier , when the temperature at the coast is lowered by the seabreeze , which
begins to blow before noon , and during the rainy season the temperature at this
...
Side 97
The mean daily range of the temperature of the sea has been ascertained off the
Scottish coast from Captain Thomas ' s observations , already referred to . On a
mean of the year it is as follows :Mean of daily Minima . 48° . 43 | Maximum at 4 P
...
The mean daily range of the temperature of the sea has been ascertained off the
Scottish coast from Captain Thomas ' s observations , already referred to . On a
mean of the year it is as follows :Mean of daily Minima . 48° . 43 | Maximum at 4 P
...
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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 |