Handy Book of Meteorology |
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Side 6
... the barometric measurement of heights , the tradewinds , evaporation , and
natural and artificial climates . While in all these departments he contributed
largely to our knowledge , his attention was most successfully turned to the
investigation ...
... the barometric measurement of heights , the tradewinds , evaporation , and
natural and artificial climates . While in all these departments he contributed
largely to our knowledge , his attention was most successfully turned to the
investigation ...
Side 34
Hence these two hemispheres are in direct contrast to each other in respect of
heat , and consequently evaporation , which depends on the temperature . The
hemisphere exposed to the sun is warm , and the hemisphere turned in the other
...
Hence these two hemispheres are in direct contrast to each other in respect of
heat , and consequently evaporation , which depends on the temperature . The
hemisphere exposed to the sun is warm , and the hemisphere turned in the other
...
Side 35
Vapour tends to diffuse itself equally through the air ; but , as the particles of air
offer an obstruction to the watery particles , the vapour is accumulated or pent up
in the lower stratum of the atmosphere about 9 or 10 A . M . , when evaporation is
...
Vapour tends to diffuse itself equally through the air ; but , as the particles of air
offer an obstruction to the watery particles , the vapour is accumulated or pent up
in the lower stratum of the atmosphere about 9 or 10 A . M . , when evaporation is
...
Side 36
But as the vapour becomes more equally diffused and the air more saturated ,
evaporation proceeds more languidly ; the air becomes also more expanded by
the heat , and flows away to meet the diurnal wave of cold advancing from the ...
But as the vapour becomes more equally diffused and the air more saturated ,
evaporation proceeds more languidly ; the air becomes also more expanded by
the heat , and flows away to meet the diurnal wave of cold advancing from the ...
Side 39
But the production of aqueous vapour by evaporation being most active in
summer , the pressure on the barometer will be increased from this cause . As the
aqueous vapour is transferred to the colder hemisphere it will be there
condensed ...
But the production of aqueous vapour by evaporation being most active in
summer , the pressure on the barometer will be increased from this cause . As the
aqueous vapour is transferred to the colder hemisphere it will be there
condensed ...
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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 |