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Side 2
In this way many valuable facts were ascertained and passed current from hand
to hand , so that there is perhaps no science of which more of the leading facts
and inferences have been so long incorporated into popular language . 4 .
In this way many valuable facts were ascertained and passed current from hand
to hand , so that there is perhaps no science of which more of the leading facts
and inferences have been so long incorporated into popular language . 4 .
Side 67
Within the tropics , and in temperate regions during winter - in other words ,
where the daily range of temperature is small — the maximum temperature
occurs about an hour and a half after the sun has passed the meridian at noon .
Within the tropics , and in temperate regions during winter - in other words ,
where the daily range of temperature is small — the maximum temperature
occurs about an hour and a half after the sun has passed the meridian at noon .
Side 112
... Scotland was passed . Was the low temperature of the sea on the British coast
from the Wash to Berwick , caused by a cold current from the Baltic Sea ( where
the temperature 112 THE DISTRIBUTION OF TERRESTRIAL TEMPERATURE .
... Scotland was passed . Was the low temperature of the sea on the British coast
from the Wash to Berwick , caused by a cold current from the Baltic Sea ( where
the temperature 112 THE DISTRIBUTION OF TERRESTRIAL TEMPERATURE .
Side 151
... the cold passed more quickly and completely through undrained than through
drained land . 4 . When the temperature of the air was higher than that of the soil ,
drained land received more benefit from the higher temperature than undrained ...
... the cold passed more quickly and completely through undrained than through
drained land . 4 . When the temperature of the air was higher than that of the soil ,
drained land received more benefit from the higher temperature than undrained ...
Side 186
sea , and are therefore moist ; but diminished if they have previously passed over
large tracts of land , particularly mountain - ranges , and are therefore dry . Since
the quantity of rain is evidently much modified by the temperature of the earth ...
sea , and are therefore moist ; but diminished if they have previously passed over
large tracts of land , particularly mountain - ranges , and are therefore dry . Since
the quantity of rain is evidently much modified by the temperature of the earth ...
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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 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 storm summer surface Table temperature thermometers tion tube upper vapour vols weather whole wind winter
Populære avsnitt
Side 396 - MACKENZIE. Studies in Roman Law. With Comparative Views of the Laws of France, England, and Scotland. By Lord MACKENZIE, one of the Judges of the Court of Session in Scotland.
Side 396 - KINGLAKE'S CRIMEAN WAR. The Invasion of the Crimea : its Origin, and an Account of its Progress down to the Death of Lord Raglan.
Side 397 - Burton.— The History of Scotland, from the Revolution to the Extinction of the last Jacobite Insurrection (1689—1748).
Bibliografisk informasjon
| Tittel | Handy Book of Meteorology |
| Forfatter | Alexander Buchan |
| Utgave | 2 |
| Utgiver | W. Blackwood and Sons, 1868 |
| Original fra | Harvard University |
| Digitalisert | 25. mar 2008 |
| Lengde | 371 sider |
| Eksporter sitat | BiBTeX EndNote RefMan |