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WorksheetsAtmosphere Multiple Choice Questions C10-C17
Total questions: 140
Worksheet time: 12mins
When super cooled water drops and ice particles coexist, the ice crystals grow at the expense of the water drops because
Saturation vapour pressure over water drops is less than over the ice crystals
Saturation vapour pressure over the ice crystals is less than over water drops
The ice crystals convert into water drops
The clouds whose tops extend well above the freezing level are called
Warm Clouds
Cold Clouds
Moderate Clouds
The clouds whose tops do not extend to the freezing level are called
Warm Clouds
Cold Clouds
Moderate Clouds
Coalescence Theory explains occurrence of rainfall from the
Warm Clouds
Cold Clouds
Both types of Clouds
Ice crystal Theory explains occurrence of rainfall from the
Warm Clouds
Cold Clouds
Both types of Clouds
Giant Nucleus Theory explains occurrence of rainfall over
Maritime areas
Inland areas
Hilly areas
Very heavy precipitation as showers over a short period is called
Flash floods
Cloud Burst
Orographic Rain
Rain shadow area is on the ………… of the mountain range
Top
Windward side
Leeward side
Sleet is a mixture of
Hail & Snow
Rain & Snow
Frozen Rain
Rainfall in the tropics is more in
Winters
Summers
Post monsoon
Rainfall in the tropics is more in the
Morning
Afternoon
Night
Rainfall in the temperate latitudes is more in
Winters
Summers
Spring
Over J&K and western Himalayas Rainfall is more in
Winters
Summers
Post monsoon
Rainfall over coastal areas is more in the
Evening
Afternoon
Night & early morning
Areas to the ………… of western Ghats of India are rain shadow areas
W
S
E
A sudden rise in the level of rivers or streams causing floods is called
Cloud Burst
Catchments flooding
Flash Floods
Artificial rain making is also termed as
Simulation
Cloud seeding
Nucleation
Fog can be dispersed for a short period by artificial stimulation
True
False
Showery precipitation occurs from
NS
AC
CB
A day is called Rainy day when rainfall in 24 hr is ....mm or more
1.5
2
2.5
Hoar frost occurs on airframe in clear air when the temperature of airframe is
below the frost point
frost point
just above the frost point
In clouds at temperatures below 0∘C an aircraft may encounter icing of the type
only Glazed
only Rime
intermediate between these two
Opaque Rime ice is
Light porous
Solid
Mixture of porous and solid
Rime is formed by freezing of ……… supercooled water droplets on airframe when aircraft is flying through clouds
Small
Large
Medium
Glazed ice is formed by freezing of ……… supercooled water droplets on airframe when aircraft is flying through clouds
Small
Large
Medium
The ……… ice poses serious aviation hazard
Rime
Hoar Frost
Glazed
Airframe icing occurs below 0∘C . Its probability of occurrence decreases progressively below 20∘C , as at lower temperatures the proportion of supercooled water drops in a cloud
Increases
Decreases
Does not change
CI, CS and CC clouds consist mostly ice crystals. Icing hazard is therefore
Maximum
Medium
Negligible
AS, NS consist of supercooled water drops and ice crystals in varying proportion…….. icing is possible.
Maximum
Light or moderate
In AC clouds …………. icing is likely in mountainous areas
Severe
Light to moderate
Negligible
In TCU icing may range from light to severe type at least up to ……… level.
-40 °C level
30 °C level
-20 °C level
In CB icing may range from light to severe type up to 20°C level. Below this temperature severe icing is
not significant
significant
maximum
Liquid water content is an important factor in icing. As the maximum water concentration is around ……., maximum ice formation in clouds may also be expected around that level.
-25°C level
-20°C level
-15°C level
Carburetor icing occurs when air from intake passes through a venturi (choke) and causes expansional cooling and vaporization of fuel. Serious icing can occur at extreme temperatures
13 °C
30°C to -10°C
20 °C
………… occurs in a moist cloudless air on an aircraft surface having temp. below 0° C, due to sublimation of water vapour onto feathery ice crystals.
Rime
Glazed
Hoar Frost
…………… occurs in St, Sc, Ac, Cu, Ns at temperature 10 to 40° C and in Cb at temperature 20 to 40°C
Rime
Glazed
Hoar Frost
In clouds … occurs when a wide range of water drop sizes are present at temperatures between 0°C and 40°C
Rime
Glazed
Mixture of rime and clear ice
……… occurs in AS, NS, SC and towering CU or CB between 0° C and 20° C, in warm front below 0° C, especially if the aircraft has rapidly descended from a colder region
Glazed
Fume
Mixture of Rime and Clear ice
When fog freezes on parked aircraft it produces..
Hoar Frost
Clear ice
Icing ………… the stalling speed appreciably
Decreases
Increases
Does not increase/decrease
The condition necessary for the formation of a thunderstorm are:
Steep lapse rate, strong winds
Shallow lapse rate, adequate supply of moisture
Steps lapse rate ,adequate supply of moisture and trigger action.
Hail is most likely to fall from a cloud
Having layers
Composed of Ice crystals
Having strong vertical development
Norwesters are
The western disturbances which affect NW India
Severe thunderstorms which occur over NE India during hot weather period
Severe thunderstorms which occur over Peninsula during hot weather period
Dust Storm usually occurs over NW India during
Post-monsoon
Winter
Pre-Monsoon
A 'mature' thunderstorm has
updraft only
downdraft only
updrafts and downdrafts
Aircraft icing is most favoured in the cloud which have temperatures ranging between
20°C and 40°C
0°C and -20°C
below 40 ° C
A short duration, showery precipitation is associated with
ST
AS
CB
Hail is
Solid precipitation which commonly occurs over the mountainous regions in winter.
Frozen or partly frozen rain falling from sheet type of clouds
Solid precipitation falling from a deep convective cloud
The most hazardous cloud for aviation is
CB
CU
NS
The life of a Cb cell is usually
7 to 8 hrs
30 to 45 min
3 to 4 hr
Generally the severest activity of a, heat type, TS is for
2 hrs
30 to 45 min
3 to 4 hr
Norwesters occur during
Jan-Feb
Mar-May
June-Sep
Oct Dec
Norwesters occur during
Winter
Hot weather
Monsoon
Post Monsoon
Norwesters affect
N India
Bengal, Bihar, Orissa and Assam
Central India
The trigger action may take place due ro
Clear night sky no wind
Orographic lifting
high pressure
Norwesters normally occur during
Mornings
Afternoons
Nights
Norwesters originates over
Chota - Nagpur hills
Deccan Plato
Andhi (blinding storms) occur generally over
S India
N India
NE India
Wind speed in Light DS is
25 kt
30 kt
up to 21 kt
The diameter of Microburst is
less than 4 km
less than 2 km
less than 6 km
The diameter of Macroburst is
< 4 km
4 km or more
> 8 km
For detecting precipitation a Radar wavelength in the range ... is suitable
30 to 200 mm
400–500 mm
600–700 mm
For airborne radars wavelength generally used
20 mm
40 mm
60 mm
The wavelength of TS detection X band radar is
10 mm
20 mm
30 mm
The wavelength of storm detection S band radar is
50 mm
100 mm
200 mm
Over plains TS mostly occur during the
afternoon
night
early morning
Over valley and foot hills TS generally occur during
afternoon
night & early morning
Over the sea TS are more frequent
afternoon
night
early morning
The life of Mesoscale Convective Complex TS is
2–3 hr
3–4 hr
6 to 24 hr
Loud peals of thunder, frequent flashes of lightning, moderate or heavy showers accompanied by light hail with maximum wind speed 15–40 kt is classified as
Light TS
Moderate TS
Severe TS
For a severe TS one of the requirements is strong wind shear
Horizontal
Vertical
Slant
Severe TS cells are tilted
in vertical
to the South
to the North
When flying through an active TS, lightning strikes are mostly likely
Above 5000 ft and under the anvil
In the clear air below the cloud in rain
In the temperature band between +10 C and -10 C
At or above 10000 ft
Hazards of the mature stage of TS Cell include lightning, turbulence and
Microburst, windshear and anvil
Icing, microburst and WS
Icing, drizzle and microburst
WS, hail and fog
Hail grows by
freezing as it leaves the cloud
up and down forces in CU cloud
collision with ice crystals
collision with supercooled water drops
The airmass which originates at sea in low Latitudes is called
Polar maritime
Tropical continental
Tropical maritime
The air mass which originates over equatorial region is
Warm & Dry
Warm & Moist
Cold & Dry
If the advancing cold front is colder than the cool air mass of the warm front, the advancing cold front undercuts and lifts both the warm and cool air masses of the warm front. This is
Warm Occlusion
Cold Occlusion
The airmass which originated over land area located in polar region:
Warm & Dry
Warm & Moist
Cold & Dry
If a warm air mass overtakes a cold air mass, it is called
Cold Front
Warm Front
Occluded Front
At warm front
Warm air overtakes the cold air
Cold air undercuts the warm air
The conditions are always unstable at
Cold front
Warm front
Sometimes line squall occurs about 100–300 km ahead of
Warm front
Cold front
Precipitation occurs over a belt of 30–50 km on both side of front
Cold front
Warm front
Cold front moves at ...... the speed of a warm front moves
Same
Double
Half
Line Squalls occur ......... of Cold front
Ahead
Behind
At the front
CB, roll-type clouds, SC, AC with embedded CB are associated
Cold front
Warm front
The surface of discontinuity between the Polar Easterlies and the temperate Westerlies is called
Equatorial Front
Tropopause
Polar Front
The air mass which originates from sea area located in lower latitudes is
Warm and dry
Warm and moist
Cold and moist
WDs approach India as
Cols
Occluded fronts
Highs
Maximum WDs occur in
Summers
Post monsoon
Winters
Ahead of a warm front the surface wind
Backs and weakens
Veers and strengthens
Backs and strengthens
On approach of a warm front temperature
Fall
Rise
Remain same
CI, CS, AS, NS, ST in sequence are associated with the front
Warm
Cold
Occluded
During the passage of a cold front winds
Suddenly become squally
Back and weaken
Veer and are of moderate strength
Visibility is poor in a warm front
Ahead
Ahead and during
After and during
Fog occurs in cold front
Ahead
During
After
WD is an .......... front
Cold
Warm
Occluded
FZRA and FZFG occur .......... of a warm front
Ahead
During
After
Precipitation ceases after the passage of a front
Cold
Warm
Occluded
During the approach of a warm front wind
Backs
Veers
Does not change
A WD has two or more closed isobars, at 2 hPa interval, it is termed as
Troughs in Westerlies
Western Depression
Western Cyclone
A WD originate over
Baluchistan
Caspian Sea
Mediterranean, Caspian and Black Seas
Induced lows develop to the ........... of a WD
N
S
NE
The arbitrary lower limit of jet core velocity has been assigned by WMO as
60 kt
60 m/s
70 m/s
Jet stream has
one maxima
one or more maxima
only two maxima
The vertical wind shear in a jet stream is about
5 m/s/km
6 m/s/km
7 m/s/km
Compared to horizontal wind shear the vertical wind shear in a jet stream is
weaker
stronger
same
In a jet stream, the path of the maximum speed is known as
Core
Axis
Jet streak
The wind speed along the axis of a jet stream is always
Uniform
Not uniform
Axis
Along the axis of a jet stream there are centres of high speed winds, these are called
Jet streaks
Core
Axis
In a wavy jet the jet streaks are located over or near the
Ridge
Trough
Between trough and ridge
Subtropical Jet Stream (STJ) is
Westerly
Easterly
Southerly
The normal position of Subtropical Jet Stream is
30° N
27° N
35° N
The southern most position of STJ is in February is
22° N
20° N
18° N
The STJ affects India from
Jun to Jul
Nov to Apr
Sep to Oct
STJ has a layered structure. There are often two layers of maximum wind to the ...... of jet core
S
N
SW
The STJ strengthens
Northwards
Upstream
Downstream
At and near the STJ the temperature gradient is very
Small
Large
Moderate
Vertical wind shear in STJ is greater ………… the core
above
below
along
The TJ prevails over the Indian Peninsula from
May to Jun
Sep to Oct
Jun to Aug
The TJ is located over the Indian Peninsula, approximately at
13° N
17° N
18° N
The TJ is located over Indian, approximately at a height of
15–16 km
12–13 km
11–12 km
The TJ is strongest in
July–Aug
Sep–Oct
June
In the TJ the wind shears are much …… than the STJ
more
less
same
TJ is
Westerly
Easterly
Southerly
A jet stream can be recognized by
High level dust
High Pressure
Streaks of CI
Lenticular clouds
Flying at right angles to a jet stream with falling pressure you will experience
wind from left
Increasing head wind
Increasing tail wind
Wind from right
When and Where tropical jet stream occurs
All year along equator
In middle East in summers
In winters over Russia
In summers over SE Asia and Central Africa
For mountain waves to form there should be flow of air across the ridge, generally within …………… of the perpendicular to the ridge.
30°
45°
60°
For mountain waves to form the wind speed for small mountains should be atleast
15 m/s
10 m/s
7 m/s
For mountain waves to form the wind speed for large mountains should be atleast
15 m/s
10 m/s
7 m/s
For mountain waves to form the atmosphere should be ……. up to the ridge, where air stream strikes the ridge.
Unstable
Stable
Indifferent
For mountain waves to form the atmosphere should be ….. at higher levels above the ridge
Unstable
Stable
Indifferent
The worst kind of turbulence is encountered in the vicinity of rotor clouds
Rotar Clouds
Lenticular Clouds
Cap Clouds
In Mountain waves the Rotor clouds form in
Troughs
Ridges
Valleys
Clear air turbulence is often encountered
At the boundary of a jet stream
In the wake of a passing airplane
In the wake of a larger airplane at take off and landing
All of the above
Most CAT occurs on the ……. of a jet stream and in the vicinity of upper level frontal zones where temperature contrasts are strong.
Fringes
Within the core
Axis
CAT is the bumpiness experienced by aircraft at high altitudes ……. in either cloudfree conditions or in stratiform clouds
above 18,000 feet
below 18,000 feet
below 28,000 feet
When approaching an area where mountain waves have been reported, a pilot should expect:
Possible presence of roll clouds and lenticular clouds
Intense updrafts and downdrafts on the lee side of the mountains
Moderate to severe turbulence as far as 20 to 30 miles from the range on lee side
All of the above
