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You compare the readings of wet bulb and dry bulb thermometers to measure
scattering
32 degrees
30 degrees Celsius
prevailing westerlies
cumulonimbus
wind vane
relative humidity
convection current
Wind direction is measured with a
scattering
32 degrees
30 degrees Celsius
prevailing westerlies
cumulonimbus
wind vane
relative humidity
convection current
The sky looks blue because of
scattering
32 degrees
30 degrees Celsius
prevailing westerlies
cumulonimbus
wind vane
relative humidity
convection current
Hailstones form only in the type of clouds called
scattering
32 degrees
30 degrees Celsius
prevailing westerlies
cumulonimbus
wind vane
relative humidity
convection current
The upward movement of warm air and the downward movement of cool air is called a
scattering
32 degrees
30 degrees Celsius
prevailing westerlies
cumulonimbus
wind vane
relative humidity
convection current
Clouds form when air is cooled to
scattering
32 degrees
30 degrees Celsius
prevailing westerlies
cumulonimbus
wind vane
relative humidity
convection current
On the Fahrenheit scale, the freezing point of water is
scattering
32 degrees
30 degrees Celsius
prevailing westerlies
cumulonimbus
wind vane
relative humidity
convection current
In the Northern Hemisphere, global winds that blow from the south-west to the northeast are called
scattering
32 degrees
30 degrees Celsius
prevailing westerlies
cumulonimbus
wind vane
relative humidity
convection current
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