Handy Book of Meteorology |
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Side 34
The surface of the globe is always divided into a day and night hemisphere ,
separated by a great circle which revolves with the sun from east to west in
twenty - four hours . Hence these two hemispheres are in direct contrast to each
other in ...
The surface of the globe is always divided into a day and night hemisphere ,
separated by a great circle which revolves with the sun from east to west in
twenty - four hours . Hence these two hemispheres are in direct contrast to each
other in ...
Side 50
The crowding together of the isobarometric lines in the south and east of Asia is
caused by the vapour which the summer monsoon brings to these regions , and
which is there precipitated in a copious rainfall . The low pressures which prevail
...
The crowding together of the isobarometric lines in the south and east of Asia is
caused by the vapour which the summer monsoon brings to these regions , and
which is there precipitated in a copious rainfall . The low pressures which prevail
...
Side 51
... be regarded as a drain lowering the pressure of Eastern Asia . ... The sources
of this high mean pressure must be upper currents flowing towards it and over it
from the four regions of low pressure , — lying respectively to the east , the south
...
... be regarded as a drain lowering the pressure of Eastern Asia . ... The sources
of this high mean pressure must be upper currents flowing towards it and over it
from the four regions of low pressure , — lying respectively to the east , the south
...
Side 52
It is , however , probably correct , since there is no mountain barrier stretching
east and west across the continent damming up the dense cold air and
preventing it from flowing over the United States . The effect of the Mediterranean
and ...
It is , however , probably correct , since there is no mountain barrier stretching
east and west across the continent damming up the dense cold air and
preventing it from flowing over the United States . The effect of the Mediterranean
and ...
Side 67
... from the warmer east towards the place of greatest cold , as evidenced by the
daily fluctuations of the barometer , perhaps contributes in a small degree to the
same result . 142 . Within the tropics , and in temperate regions during winter —
in ...
... from the warmer east towards the place of greatest cold , as evidenced by the
daily fluctuations of the barometer , perhaps contributes in a small degree to the
same result . 142 . Within the tropics , and in temperate regions during winter —
in ...
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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 |