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Side 51
The highest atmospheric pressure does not occur at this point , but at a
considerable distance westward , near the sources of the Obi and Yenisei . The
non - coincidence of the areas of greatest cold and greatest pressure may be
explained by ...
The highest atmospheric pressure does not occur at this point , but at a
considerable distance westward , near the sources of the Obi and Yenisei . The
non - coincidence of the areas of greatest cold and greatest pressure may be
explained by ...
Side 59
The most important temperatures in their relation to climate and most other
inquiries are the highest which occur during the day and the lowest which occur
during the night ; and to record these , various thermometers have been devised ,
well ...
The most important temperatures in their relation to climate and most other
inquiries are the highest which occur during the day and the lowest which occur
during the night ; and to record these , various thermometers have been devised ,
well ...
Side 74
At the Scottish stations , the smallest differences between the 9 A . M . and 9 P . M
. and the maximum and minimum observations occur in the western and northern
islands , where the climate is eminently cloudy and rainy . An examination of ...
At the Scottish stations , the smallest differences between the 9 A . M . and 9 P . M
. and the maximum and minimum observations occur in the western and northern
islands , where the climate is eminently cloudy and rainy . An examination of ...
Side 76
that excessive cold rarely occurs . Ventnor ... afforded by the Undercliff , and in its
proximity to the sea , towards which its cold heavy air flows , and being there
counteracted by the higher temperature of the sea , low temperatures rarely occur
.
that excessive cold rarely occurs . Ventnor ... afforded by the Undercliff , and in its
proximity to the sea , towards which its cold heavy air flows , and being there
counteracted by the higher temperature of the sea , low temperatures rarely occur
.
Side 80
... to the thermometers , and their proximity to walls , trees , or other objects which
radiate their heat to the thermometers ; whereas with boxes louvre - boarded all
round , such variation does not occur , or if it does , only to a very slight degree .
... to the thermometers , and their proximity to walls , trees , or other objects which
radiate their heat to the thermometers ; whereas with boxes louvre - boarded all
round , such variation does not occur , or if it does , only to a very slight degree .
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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 important inches increase indicate influence January July known 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
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 |