Handy Book of Meteorology |
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Side 50
... which blow thither from an almost unbroken sheet of waters , which embraces
the South Pacific , the South Atlantic , and the Indian Ocean , and which meet
with little land to condense the vapour till they flow within the antarctic circle . 104
.
... which blow thither from an almost unbroken sheet of waters , which embraces
the South Pacific , the South Atlantic , and the Indian Ocean , and which meet
with little land to condense the vapour till they flow within the antarctic circle . 104
.
Side 54
through the centre of which runs a narrower belt of still lower pressure , towards
which the trade - winds blow . Since these belts of high pressure can only be
maintained by air flowing in upon them in the upper regions of the atmosphere , it
is ...
through the centre of which runs a narrower belt of still lower pressure , towards
which the trade - winds blow . Since these belts of high pressure can only be
maintained by air flowing in upon them in the upper regions of the atmosphere , it
is ...
Side 67
... 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 hour is
still further lowered by the clouds which then begin to overspread the sky .
... 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 hour is
still further lowered by the clouds which then begin to overspread the sky .
Side 123
As an atmosphere loaded with vapour obstructs both solar and terrestrial
radiation , moist winds blowing from the ocean are accompanied by a mild
temperature in winter , and a cool temperature in summer ; and dry winds coming
from ...
As an atmosphere loaded with vapour obstructs both solar and terrestrial
radiation , moist winds blowing from the ocean are accompanied by a mild
temperature in winter , and a cool temperature in summer ; and dry winds coming
from ...
Side 144
... the key to the climates of all parts of the globe in the different seasons of the
year ; for the direction of prevailing winds thus becomes known , and these are
warm or cold , and dry or wet , as determined by the regions from which they blow
.
... the key to the climates of all parts of the globe in the different seasons of the
year ; for the direction of prevailing winds thus becomes known , and these are
warm or cold , and dry or wet , as determined by the regions from which they blow
.
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Vanlige uttrykk og setninger
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 |