Reading the WeatherLongstreth, T. Morris (Thomas Morris)
Science
Reading the Weather
Longstreth, T. Morris (Thomas Morris)
Weather forecasting
In lesser fashion the Appalachians protect the Atlantic seaboard. They
withstand the impact of the cold waves to a great extent, although they
are not high enough to divert the flow of cold air entirely toward the
south and it is not desirable that they should. As things are the cold
strikes Alabama before it hits New Jersey, and is often more severe there.
Comparative cold is often registered by the green color of the sky. A
fiery red continues the prevailing heat.
The day that is ushered in by a fog, in summer, will likely be warm,
providing the fog lifts by ten o'clock.
The temperature of a night with even a thin covering of clouds will be a
good deal higher than if the sky is clear. In the British Isles the whole
difference between freezing and no freezing lies with the fairness of the
heavens. Everywhere frost will not form while the sky is covered, although
the temperature may be below the freezing point. In summer radiation on a
still clear night may be so rapid that frost may follow a temperature of
fifty degrees at nightfall.
The temperature at the surface of the earth may easily deceive, as a
colder or warmer stratum of air may overlie that immediately next to the
ground. I have seen water particles fall when the temperature was as low
as 16 degrees above zero, showing that the stratum of cold air was very
thin. Our sleet storms in which immense damage is done to trees and
telegraph wires occurs from just such a situation,--a cold, shallow layer
of air close to the earth, with the warm moisture-bearing air flowing over
it. The reverse of this situation is not uncommon--the sight of a
snowstorm proceeding merrily along with the ground temperature at 35 or
even 40 degrees.
Coming warmth may be noticed by the increase in size of snow flakes, with
finally hail and rain. Coming cold is foreshadowed by hail mixed with the
rain and lastly snow flakes which have a tendency to decrease in size.
Colors of the clouds predict temperature changes, but it takes much
practice to distinguish the cold, hard grays from the soft, warm ones. A
warm sky is always less uniform in color than a cold one. The colors of
winter sunsets are, as a rule, much brighter than those of summer skies.
The stars seem brighter on a night that is to be cold. If they twinkle it
is because of rushing air currents, and if the wind is from the northwest
the result may be a subsequent lowering of temperatures.
The whole question of whether it will be colder and how much is vital to
the camper and if the signs of change are taken along with the look of the
clouds and the direction of the wind he need never be wrong as to the
direction the mercury is going, and will soon be able to guess the
distance pretty fairly.
RAIN AND SNOW
Public-domain text, read in full here on John Shaqi.
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