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Scientists
have studied cloud types and have realized that rain
clouds are formed and shaped according to definite
systems and certain steps connected with certain types
of wind and clouds.
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One
kind of rain cloud is the cumulonimbus cloud. Meteorologists
have studied how cumulonimbus clouds are formed and how
they produce rain, hail, and lightning.
They
have found that cumulonimbus clouds go through the following
steps to produce rain:
1)
The clouds are pushed by the wind: Cumulonimbus clouds
begin to form when wind pushes some small pieces of clouds
(cumulus clouds) to an area where these clouds converge
(see figures 17 and 18).
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Figure
17:
Satellite photo showing the clouds moving towards
the convergence areas B, C, and D. The arrows
indicate the directions of the wind. (The Use of
Satellite Pictures in Weather Analysis and Forecasting,
Anderson and others, p. 188.)
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Figure
18:
Small pieces of clouds (cumulus clouds) moving towards
a convergence zone near the horizon, where we can
see a large cumulonimbus cloud. (Clouds and Storms,
Ludlam, plate 7.4.)
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2)
Joining: Then the small clouds join together forming
a larger cloud (see figures 18 and 19).
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Figure
19:
(A) Isolated small pieces of clouds (cumulus clouds).
(B) When the small clouds join together, updrafts
within the larger cloud increase, so the cloud is
stacked up. Water drops are indicated by ·.
(The Atmosphere, Anthes and others, p. 269.)
(Click on the image to enlarge it.)
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3)
Stacking: When the small clouds join together, updrafts
within the larger cloud increase. The updrafts near
the center of the cloud are stronger than those near the
edges. These updrafts cause the cloud body to grow
vertically, so the cloud is stacked up (see figures 19 (B),
20, and 21). This vertical growth causes the cloud
body to stretch into cooler regions of the atmosphere, where
drops of water and hail formulate and begin to grow larger
and larger. When these drops of water and hail become
too heavy for the updrafts to support them, they begin to
fall from the cloud as rain, hail, etc.
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Figure
20:
A cumulonimbus cloud. After the cloud is stacked
up, rain comes out of it. (Weather and Climate,
Bodin, p.123.)
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Figure
21:
A cumulonimbus cloud. (A Colour Guide to Clouds,
Scorer and Wexler, p. 23.)
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God
has said in the Quran:
Have
you not seen how God makes the clouds move gently, then
joins them together, then makes them into a stack, and then
you see the rain come out of it.... (Quran, 24:43)
Meteorologists
have only recently come to know these details of cloud formation,
structure, and function by using advanced equipment like
planes, satellites, computers, balloons, and other equipment,
to study wind and its direction, to measure humidity and
its variations, and to determine the levels and variations
of atmospheric pressure.
The
preceding verse, after mentioning clouds and rain, speaks
about hail and lightning:
....And
He sends down hail from mountains (clouds) in the sky, and
He strikes with it whomever He wills, and turns it from
whomever He wills. The vivid flash of its lightning nearly
blinds the sight. (Quran, 24:43)
Meteorologists
have found that these cumulonimbus clouds, that shower hail,
reach a height of 25,000 to 30,000 ft (4.7 to 5.7 miles),
like mountains, as the Quran said, “...And He sends down
hail from mountains (clouds) in the sky...” (see figure
21 above).
This
verse may raise a question. Why does the verse say
“its lightning” in a reference to the hail?
Does this mean that hail is the major factor in producing
lightning? Let us see what the book entitled Meteorology
Today says about this. It says that a cloud becomes
electrified as hail falls through a region in the cloud
of supercooled droplets and ice crystals. As liquid droplets collide with a hailstone,
they freeze on contact and release latent heat. This
keeps the surface of the hailstone warmer than that of the
surrounding ice crystals. When the hailstone comes
in contact with an ice crystal, an important phenomenon
occurs: electrons flow from the colder object toward the
warmer object. Hence, the hailstone becomes negatively
charged. The same effect occurs when supercooled droplets
come in contact with a hailstone and tiny splinters of positively
charged ice break off. These lighter positively charged
particles are then carried to the upper part of the cloud
by updrafts. The hail, left with a negative charge,
falls towards the bottom of the cloud, thus the lower part
of the cloud becomes negatively charged. These negative
charges are then discharged as lightning.We conclude from
this that hail is the major factor in producing lightning.
This
information on lightning was discovered recently.
Until 1600 AD, Aristotle’s ideas on meteorology were dominant.
For example, he said that the atmosphere contains two kinds
of exhalation, moist and dry. He also said that thunder
is the sound of the collision of the dry exhalation with
the neighboring clouds, and lightning is the inflaming and
burning of the dry exhalation with a thin and faint fire.
These are some of the ideas on meteorology that were dominant
at the time of the Quran’s revelation, fourteen centuries
ago.
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