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CPL Test Series
Question Bank
Questions for ADIABATIC AND STABILITY1
Answer the following questions
Test Mode
Training Mode
1. A layer of air can be
Conditional; unstable when unsaturated and stable when saturated
Conditional; unstable when saturated and stable when unsaturated
All of the above
Neutrally stable when saturated and unstable when unsaturated
2. The DALR is
Variable with latitude
Variable with time
Variable with temperature
Fixed
3. The stability in a layer is increasing if
warm and moist air is advected in the lower part
warm air is advected in the lower part and cold air in the upper part
cold and dry air is advected in the upper part
warm air is advected in the upper part and cold air in the lower part
4. Why does air cool as it rises?
It contracts
The air is colder at higher latitudes
It expands
The air is colder at higher altitudes
5. In unstable air, surface visibility is most likely to be restricted by
low stratus
haze
drizzle
showers of rain or snow
6. The rate of cooling of ascending saturated air is less than the rate of cooling of ascending unsaturated air because:
water vapour absorbs the incoming heat from the sun
moist air is heavier than dry air
heat is released during the condensation process
water vapour doesn’t cool as rapidly as dry air
7. From which of the following can the stability of the atmosphere be determined?
DALR
surface temperature
ELR
surface pressure
8. ELR is 1°C/100m
Absolute instability
Absolute stability
Conditional stability
Neutral when dry
9. What happens to the temperature of a saturated air mass when descending?
it heats up more than dry because of compression
it heats up less than dry because of evaporation
it heats up more than dry because of expansion
it heats up less than dry because of latent heat released during condensation
10. During an adiabatic process heat is
lost
neither added nor lost
neither added nor lost
added but the result is an overall loss
11. What happens to stability of the atmosphere in an isothermal layer? (Temp constant with height)
Absolutely stable
Unstable
Conditionally stable
Conditionally unstable
12. In an air mass with no clouds the surface temperature is 15°C and 13°C at 1000m. This layer of air is
conditionally unstable
stable
a layer of heavy turbulence
unstable
13. A parcel of air cooling by more than 1°C/100m is said to be?
Unstable
Conditionally unstable
Conditionally stable
Stable
14. In still air a lapse rate of 1.2°C/100m refers to
ALR
DALR
ELR
SALR
15. If the ELR is 0.65°C/100m
Atmosphere is conditionally stable
Atmosphere is stable when dry
Atmosphere is absolutely unstable
Atmosphere is absolutely stable
16. Which of the following gives conditionally unstable conditions when saturated?
1°C/100m
0.49°C/100m
0.65°C/100m
None of the above
17. When warm air is advected in the lower part of a cold layer of air
stability will remain the same
stability will be conditional
stability decreases in the layer
stability increases in the layer
18. What happens to the temperature of a saturated air mass when forced to descend?
it heats up less than dry because of evaporation
it heats up less than dry because of latent heat released during condensation
it heats up more than dry because of expansion
it heats up more than dry because of sublimation
19. What is the effect of a strong low level inversion?
Windshear
Calm conditions
Good visibility
Unstable conditions
20. A mass of unsaturated air is forced to rise till just under the condensation level. It then settles back to its original position
Temp. stays the same
Temp. is less than before
It depends on QFE
Temp. is greater than before
21. In an unstable layer there are cumuliform clouds. The vertical extent of these clouds depends on the
thickness of the unstable layer
air pressure at the surface
wind direction
pressure at different levels
22. The temperature at the surface is 15°C, the temperature at 1000m is 13°C.Is the atmosphere
Conditionally unstable
Unstable
Cannot tell
Stable
23. What happens to the stability of the atmosphere in an inversion? (Temp increasing with height) Absolutely stable
Absolutely stable
Conditionally stable
Conditionally unstable
Unstable
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