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Both ALTOCUMULUS (top) and ALTOSTRATUS (below left) clouds indicate precipitation in the next ten to 15 hours if wind is steady from between the northeast and the south.
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The secrets of weather forecasting
and preparedness.
By Matt Scanlon.
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The sky was clouding over to the east and one after
another the starts [the old man] knew were gone. It looked
now as though he were moving into a great canyon of clouds
and the wind had dropped. "There will be bad weather in
three or four days," he said. "But not tonight and not
tomorrow."
The Old Man and the Sea
Ernest Hemingway
In fact, nearly all but the largest TV stations simply grab
the forecasts provided by the National Weather Service
(NWS) and disguise them as their own. It would be foolish
to completely discount their advice, but just as all our
politics is inherently local, so is our weather. Individual
communities have peculiar rainfall patterns, unique wind
currents and other vagaries that defy a sweeping
declaration of "scattered showers." The only way to guess
with accuracy when it is going to rain or snow on your roof
is to train your eye. With a crash course in cloud types,
wind direction and speed, and what the frenzy of numbers in
a forecast really means, you'll have a leg up on
the national weather guessers... and a great excuse to
stare endlessly at the sky without ever being accused of
daydreaming.
The Anatomy of Clouds
Weather, for all its thousands of forms, storms and sunny
days, is actually just nature's way of distributing heat.
Every day, the sun heats the earth with energy equivalent
to burning nearly one billion tons of coal. The earth's
atmosphere, proportionally no thicker than the skin of an
apple, takes the brunt of the radiation. If this incredible
amount of energy were distributed evenly, pole to pole,
we'd have an endless array of sunny days. Of course, we'd
also have no rain, plants or life. Fortunately for us,
temperature imbalances occur, not only because half the
earth cools itself during the night, but because the poles
reflect more heat energy than they absorb. Since the planet
seeks balance, the excess heat in the tropics naturally
distributes itself north and south from the equator. That
distribution vehicle is wind, and in the face of constantly
changing temperatures, water vapor blown into the
atmosphere from oceans, lakes and rivers will often
condense into clouds.
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