The new air world : $b The science of meteorology simplifiedMoore, Willis L. (Willis Luther)
Science
The new air world : $b The science of meteorology simplified
Moore, Willis L. (Willis Luther)
Meteorology
Because of the vast extent of the Eurasian (Europe and Asia)
continent the difference between continental and marine climates is
more marked than in the Western Hemisphere. Huntington and Cushing,
in their splendid work on “Principles of Human Geography”,[3] make
a comparison between the southern Lofoten Islands, off the coast
of Norway, and Verkhoyansk in Siberia, which probably furnish the
greatest contrast to be found anywhere between places of the same
latitude. Although both are inside the Arctic Circle, the influence
of the Atlantic Ocean with its warm-water currents coming all the way
from the tropics (Chart 13) protects the Lofoten Islands from the
extreme cold that otherwise would come to them; vegetation remains
green and cattle are pastured every month in the year. But the ocean
retains nearly the same temperature in summer as in winter, and
as a result the Islands are too cold to grow trees or many crops.
Verkhoyansk is so different that one can scarcely believe that both
places are in the same latitude. At the Siberian town the winter
temperature falls to 70° or 80° below zero every winter, and has
been known to register 90° below zero. It is said that steel skates
often will not “take hold” but slip sideways as well as forward on
the surface of the excessively cold ice. This doubtless is due to
the fact that under ordinary winter cold the weight of the skater
melts a thin film of water under the edge of the skate, which freezes
instantly when the skate passes and relieves the pressure. But here
the cold is so intense that the weight of no skater is sufficient
to lubricate his movements with water molecules. Remarkable to
relate, the summer at Verkhoyansk is warmer than in the islands
off the Norwegian coast, due to the rapidity with which the land
surface warms up under the action of the solar rays in the midst of
a continental area remote from water, 75° to 80° frequently being
recorded during the long summer days. The ground never thaws for more
than a foot or so, but a number of crops are successfully grown.
Public-domain text, read in full here on John Shaqi.
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