Question Bank

DGCA Question Bank

4,298 questions with answers and explanations · growing weekly

Showing 25 of 4,298 questions
1
Aviation Meteorology · Aviation Meteorology (Advanced)

The lowest layer of the atmosphere is the:

A.Troposphere
B.Tropopause
C.Stratosphere
2
Aviation Meteorology · Aviation Meteorology (Advanced)

The height of the tropopause at the Equator is approximately:

A.10–12 km
B.16–18 km
C.12–14 km
3
Aviation Meteorology · Aviation Meteorology (Advanced)

The height of the tropopause at the Poles is approximately:

A.12–14 km
B.12–13 km
C.8–10 km
4
Aviation Meteorology · Aviation Meteorology (Advanced)

The higher the surface temperature, the ____ the tropopause:

A.Higher
B.Lower
C.Same
5
Aviation Meteorology · Aviation Meteorology (Advanced)

The height of the tropopause:

A.Is constant
B.Varies with altitude
C.Varies with latitude
6
Aviation Meteorology · Aviation Meteorology (Advanced)

Above 8 km, the lower temperatures are found over the:

A.Equator
B.Mid-latitudes
C.Poles
7
Aviation Meteorology · Aviation Meteorology (Advanced)

The atmosphere is heated mainly by:

A.Solar radiation directly
B.Heat from the earth's surface
C.Radiation from space
8
Aviation Meteorology · Aviation Meteorology (Advanced)

The stratosphere is:

A.Unstable
B.Neutral
C.Stable
9
Aviation Meteorology · Aviation Meteorology (Advanced)

The tropopause is discontinuous (has breaks) at about:

A.30° latitude
B.40° latitude
C.60° latitude
10
Aviation Meteorology · Aviation Meteorology (Advanced)

Most of the atmospheric mass is contained in the:

A.Troposphere
B.Stratosphere
C.Heterosphere
11
Aviation Meteorology · Aviation Meteorology (Advanced)

The stratosphere extends from the tropopause up to about:

A.50 km
B.60 km
C.40 km
12
Aviation Meteorology · Aviation Meteorology (Advanced)

The atmospheric layer characterised by a temperature inversion and great stability is the:

A.Troposphere
B.Tropopause
C.Stratosphere
13
Aviation Meteorology · Aviation Meteorology (Advanced)

Mother-of-pearl (nacreous) clouds occur in the:

A.Mesosphere
B.Thermosphere
C.Stratosphere
14
Aviation Meteorology · Aviation Meteorology (Advanced)

In the ISA, the temperature at 17 km is:

A.−56.5°C
B.−65.5°C
C.−35.5°C
15
Aviation Meteorology · Aviation Meteorology (Advanced)

By weight, the approximate ratio of O₂ to N₂ in the atmosphere is:

A.1:3
B.1:4
C.1:5
16
Aviation Meteorology · Aviation Meteorology (Advanced)

By volume, the approximate ratio of O₂ to N₂ in the atmosphere is:

A.1:3
B.1:4
C.1:5
17
Aviation Meteorology · Aviation Meteorology (Advanced)

By volume, the proportion of CO₂ in the atmosphere is about:

A.3%
B.0.3%
C.0.03%
18
Aviation Meteorology · Aviation Meteorology (Advanced)

In the ISA, the mean sea level temperature is:

A.15°C
B.10°C
C.25°C
19
Aviation Meteorology · Aviation Meteorology (Advanced)

The maximum concentration of ozone is at a height of about:

A.10–15 km
B.20–25 km
C.30–35 km
20
Aviation Meteorology · Aviation Meteorology (Advanced)

Supplemental oxygen is required when flying above about:

A.5000 ft
B.7000 ft
C.10 000 ft
21
Aviation Meteorology · Aviation Meteorology (Advanced)

CO₂ and water vapour keep the atmosphere:

A.Warm
B.Cold
C.No effect
22
Aviation Meteorology · Aviation Meteorology (Advanced)

Noctilucent clouds occur in the:

A.Thermosphere
B.Mesosphere
C.Stratosphere
23
Aviation Meteorology · Aviation Meteorology (Advanced)

If the temperature at 2 km is +5°C, the ISA deviation (Actual − ISA) is:

A.−5°C
B.+2°C
C.+3°C
24
Aviation Meteorology · Aviation Meteorology (Advanced)

If the MSL pressure is 1002.25 hPa, the deviation from the ISA MSL pressure is:

A.−11 hPa
B.+10 hPa
C.+12 hPa
25
Aviation Meteorology · Aviation Meteorology (Advanced)

If the temperature at 19 km is −60°C, the ISA deviation is:

A.−4.5°C
B.−5.5°C
C.−3.5°C