DGCA Meteorology: Precipitation Questions
32 exam-style Precipitation questions for the DGCA Meteorology paper (CPL · ATPL · PPL). The first 12 are free below with answers and explanations — sign up free to practise all of them with progress tracking.
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Q1
The hailstones occur from
- A cold clouds only
- B warm clouds only
- C NS clouds
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Correct answer: A. cold clouds only
Hail requires supercooled water freezing onto growing ice stones above the freezing level, so it originates only in cold clouds; warm clouds, entirely below the 0 degree C level, cannot generate hail.
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Q2
Rain shadow effect occurs on the:
- A Windward side of mountains
- B Leeward side of mountains
- C Equatorial side
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Correct answer: B. Leeward side of mountains
The leeward side gets dry air after mountains block rain on the windward side.
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Q3
Hail is typically produced by:
- A Stratus clouds
- B Clouds with large vertical development (e.g., Cumulonimbus)
- C Cirrus
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Correct answer: B. Clouds with large vertical development (e.g., Cumulonimbus)
Big cumulonimbus clouds have strong updrafts that form hail.
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Q4
Rainfall in the tropics is more in the
- A Night
- B Morning
- C Afternoon
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Correct answer: C. Afternoon
Over tropical land areas rainfall peaks in the afternoon, when maximum surface heating drives the deepest convection and thunderstorm development.
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Q5
Rainfall in the tropics is more in the
- A Afternoon
- B Morning
- C Night
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Correct answer: A. Afternoon
Tropical rainfall over land is greatest in the afternoon, when peak surface heating produces the strongest convection and shower or thunderstorm activity.
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Q6
Which cloud would you encounter the most intensive rain?
- A St
- B Ci
- C Ns
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Correct answer: C. Ns
Nimbostratus, a thick, deep precipitating layer cloud, gives the most intensive and prolonged rain of the three; stratus yields only drizzle and cirrus precipitation never reaches the ground.
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Q7
When supercooled water drops and ice particles co-exist the ice crystals grow at the expense of the water drops because
- A Saturation vapour pressure over water drops is less than over the ice crystals
- B Saturation vapour pressure over the ice crystals is less than over water drops
- C The ice crystals convert into water drops
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Correct answer: B. Saturation vapour pressure over the ice crystals is less than over water drops
At the same sub-zero temperature the saturation vapour pressure over ice is lower than over supercooled water, so vapour deposits onto the crystals while the drops evaporate, and the ice crystals grow at the expense of the water drops (the Bergeron process).
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Q8
The cloud whose tops extend well above the freezing level are called
- A Warm clouds
- B Cold clouds
- C Moderate clouds
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Correct answer: B. Cold clouds
Clouds whose tops extend well above the freezing level, and which therefore contain ice crystals and supercooled droplets, are called cold clouds.
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Q9
The clouds whose tops do not extend to the freezing level are called
- A Warm clouds
- B Cold clouds
- C Moderate clouds
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Correct answer: A. Warm clouds
Clouds lying entirely below the freezing level, containing only liquid water warmer than 0 degrees C, are called warm clouds.
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Q10
Coalescence Theory explains occurrence of rainfall from the
- A Warm clouds
- B Cold clouds
- C Both types of Clouds
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Correct answer: A. Warm clouds
The coalescence theory explains rainfall from warm clouds: droplets of different sizes, falling at different speeds, collide and merge until heavy enough to fall as rain, with no ice phase involved.
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Q11
Ice crystal Theory explains occurrence of rainfall from the
- A Warm clouds
- B Cold clouds
- C Both types of clouds
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Correct answer: B. Cold clouds
The ice-crystal (Bergeron) theory explains precipitation from cold clouds, where ice crystals coexisting with supercooled droplets grow rapidly at the droplets' expense until they fall.
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Q12
Giant Nucleus Theory explains occurrence of rainfall over
- A Maritime areas
- B Inland areas
- C Hilly areas
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Correct answer: A. Maritime areas
The giant nucleus theory attributes rainfall over maritime areas to giant salt nuclei thrown up by sea spray, on which unusually large droplets form and grow quickly by coalescence.
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