WorksheetsADDITIONAL QUESTION
Total questions: 75
Worksheet time: 38mins
The main cause of occurrence of weather over the earth surface is
Changing pressure
Advection of moist air
Variation in insolation
Movement of air mass
Thermal lows are generally located over
Polar region
Equatorial region
Temperate region
Movement region
The main cause of ground inversion is
Release of latent heat
Incident Solar radiation
Convection
Terrestrial radiation on calm and clear night
Above the friction layer winds mostly blow parallel to isobars due to balance of
Coriolis force and Geostrophic force
Coriolis force and Pressure gradient force
Coriolis force and Centripetal force
Coriolis fond and Centripetal force
Wind at 1 km height is 330/20 kt whereas surface wind is 260/05 kt because of
Subsidence
Convection
Friction
Thunderstorm
The amount of water vapour which air can hold depends on
Dew point temperature
Wet bulb temperature
Dry bulb temperature
Virtual temperature
In General circulation over the globe the Equatorial Low Pressure Belt is at the junction of which cells?
Hadley Cells
Polar cell
Ferrell and Hadley Cells
Ferrell Cell
The dew point temperature
is higher if air contains more water vapour
changes by cooling or warming
is equal to the air temperature during mist
is always higher than Wet Bulb temperature for unsaturated air
What controls the movement of most TS?
jet stream
wind at 400 hPa
wind at 700-500 hPa
wind at 30,000 ft
Isohyets are the line of equal
Humidity
Sunshine
Rainfall amount
Density
How much in advance of departure a pilot must notify the Aeronautical Met Station (AMS) requiring Met Forecast for a National flight?
3 hr
6 hr
12 hr
18 to 24 hr
An a/c cruising at FL500 in July from Chennai to Trivandrum will generally experience
Weak S'ly wind
Subtropical W'ly wind
Tropical E'ly wind
Tropical air stream
The sun is highest at noon, but two/three hours later the earth receives more radiation. Hence maximum temperature is around 1500 hr. It is due to
Angular Momentum
Thermal cooling
Thermal Inertia
Rotation of the Earth
Which of the following Indian month corresponds to Grishma Ritu
Jyeshtha and Aasadha
Shravana
Phalguna
Paush
Due to Coriolis force an E'ly wind blowing over the equator will
get deflected to the left
become W'ly
weaken
remain unchanged
The surface wind at coastal stations on West coast of India during late night/early morning in Pre-monsoon season is
E'ly
W'ly
S'ly
N'ly
Convective clouds develop at a place when the atmosphere is
absolutely stable
conditionally stable
neutrally stable
none of the above
In a SPECI report the QNH 1005.8 hPa is reported as
1016 hPa
1015.8 hPa
1005 hPa
1016.8 hPa
Stability of atmosphere is determined by
Inversion
DALR
ELR
SALR
The characteristics features, good visibility and turbulence, are of
high pressure area
stable air mass
unstable air
cold Polar air mass
Extreme turbulence in a TS can be assessed from
heavy ice accretion
frequent lightning
Hail
appearance of Anvil
Jet streams are strongest when temperature gradient are greatest
True
False
While planning to land during TS, which is the most expected serious aviation hazard
Hail storm
Downdraught
WS and Turbulence
Heavy rain
An and area the cloud which is capable of causing Dust Storm is
CI
CU
CB
NS
If after the issue of a SPECI, conditions continue to be below the prescribed limit then the next routine report will be a
METAR
SPECIAL
SPECI
could be METAR or SPECI
Fronts are characteristics of
Tropical cyclones
Monsoon depression
TS
Extra Tropical Depressions
In India in a VOLMET broadcast
SIGMET is included
METAR, SPECI, SIGMET and TAF are included
only SPECI is included
only TAF are included
In a SPECI the lowest layer of clouds, regardless of amount, is reported as
FEW, SCT, BKN or OVC
SCT, BKN or OVC
BKN or OVC
FEW, SCT, or OVC
The atmospheric pressure at an aerodrome is equal to the MSL pressure then
QNH > QFE
QNH = QFE
QNH < QFE
None of the above
An a/c at FL180 in July from Kolkata to Mumbai will generally experience
W'ly wind
E'ly wind
N'ly wind
S'ly wind
Isoqionic are the line of constant
Height
Insolation
Geopotential heights
Density
The minimum notice required to be given to an Aerodrome Met Office (AMO) by an aircraft operator needing Met data for a National flight is
3 hr
6 hr
12 hr
18 to 24 hr
In the METAR surface visibility in TS is
800 m
1200 m
4050 m
0300 m
The upper air report from an a/c other than weather reconnaissance a/c has the identification code as
WINTEM
VOLMET
RAWIN
CODAR
TAF AMD covers validity period
the remaining validity period of original TAF
half the validity period of the TAF
the validity starting 2 hr prior to the period of original TAF
full validity period of the TAF
RVR is a measure of
Atmospheric transmissivity and background illumination
Atmospheric transparency, intensity of R/W lights and background illumination
Intensity of background illumination
Atmospheric transmissivity, intensity of R/W lights
SPECI is issued when the visibility changes from
800 to 1500 m
8 km to 6 km
300 m to 400 m
300 m to 150 m
During pre-monsoon the pressure gradient in the S parts of East coast of India is from
N to S along the coast
S to N along the coast
E to W across the coast
W to E across the coast
During SW monsoon the wind at FL400 over Bengaluru is generally
Strong Ely
Strong Wly
Fluctuates between Ely and Wly
Weak Sly
The lapse rate of temperature in a low level inversion is
Positive
negative
insignificant
6.5º C
Which of the following Indian month corresponds to Rainy Season Varsha Ritu
Kwar
Kartik
Magha
Shravana Bhadapad
The Code Name for an aviation forecast in figure code for a specific area is
ROFOR
ARFOR
TAFOR
GAMET
SIGMET message is
Occurring or expected, enroute weather, which may affect safety of the air operation.
Aerodrome forecast in plain language
Special Reports to local ATC unit and concerned operators
Trend type of landing forecast passed to operators
Which of the following Indian month corresponds to Winter Shishira Ritu
Kwar
Pausha
Magha and Phalguna
Shravana
The variable surface wind speed refresh is
< 03 KT
04 KT or less
≥ 02 KT
Calm
Which of the following Indian month corresponds to Sharad Ritu (Post monsoon)
Jyeshtha
Asauj and Kartika
Phalguna
Shravana
TAF VECC 2200300Z 24000KT 3000 FU SCT100 BECMG 0406 6000 SCT030 BKN100 TEMPO 0708 2000 TSRA SCT23CB OVC80~ The above TAF forecasts TS and RA between
0400 and 0600 UTC
0400 and 0600 IST
0700 and 0800 UTC
0400 and 0800 IST
The hailstorms occur from
Both warm and cold clouds
cold clouds only
warm clouds only
NS clouds
SPECI is issued when the height of base of the lowest cloud layer > 5/8 changes to or passes
500m, 300m, 150m, 50m, 25m
450m, 300m, 150m, 50m, 30m
400m, 300m, 150m, 90m, 30m
450m, 300m, 150m, 60m, 30 m
Fog is produced in Fronts by
evaporation and precipitation
frequent Rain
Over the earth deserts are located in the regions of
Equatorial trough
Subtropical high
Polar Front
ITCZ
The air can hold more moisture at MSL over the
Temperate latitudes
20° Latitude
Equator
Poles
With altitude in an isothermal atmosphere the density of the air
does not change
increases with height
first decreases and then decrease
decreases
The Fronts associated with W'ly over NW India in winters are mostly
Warm Occlusion
Cold Occlusion
Cold Fronts
Warm Fronts
In a Cold Occlusion the
Cold air of Cold Front is not the coldest
Cold air of Cold Front is the coldest
Cold air of Warm Front is the coldest
A day is called Rainy Day when the amount of Rainfall in a day is
7.5 mm or more
10 mm or more
2.5 mm or more
at least 1.0 mm
A cold front is defined as the
advancing cold airmass undercutting the warm airmass
warm airmass over riding the cold airmass
retreating cold pool of air
leading cold gust front
In a METAR the third layer of clouds is reported when amount is
3/8 or more SCT, BKN or OVC
5/8 or less SCT, BKN
5/8 or more BKN or OVC
3/8 or more FEW, SCT
SPECI is issued an issued RVR when it changes or passes
150m
200m
400m
900m
Above which datum the cloud base is reported at airports?
above mean sea level
above the aerodrome level
above standard pressure level
above pressure level in ISA
For International Flight documentation, the following data is provided:
SIGWX charts between FL 250 and FL 600
SIGWX charts between FL 250 and FL 600 and forecast 250 hPa wind and Temp. data
SIGWX charts and Upper wind and temperature charts
WAFC generated SIGWX forecast chart only
When visibility is 800 m to 5000 m, in a METAR it is reported in steps of:
100 m
200 m
500 m
1000 m
The Polar Front is:
Continuous
Not continuous
A transition Zone between Polar and Arctic Westerlies
Boundary between Arctic and Polar Air Masses
Most of the weather occurring in India is due to:
Fronts
Cyclones
TS
Monsoon Trough
The Doppler Weather Radar works on the Principles of
Frequency amplification
Change in frequency of return echo
Comparison of drop sizes
Wavelength modification
Flight forecast in "Chart from of documentation" supplied in India consists of
Synoptic charts 03 and 12 UTC and U/A charts for 00 and 12 UTC
Latest surface synoptic chart and upper air charts
SIGWX chart and upper air charts for 150, 300 and 390 hPa
SIGWX chart and prognostic charts for 300,250 and 200 hPa
SIGMET message contains weather information which is
Actual and not a forecast
Forecast only
Both actual and forecast
Actual only
Veering of geostrophic wind at a station with height indicates
Warm air advection
Cold air advection
Subsidence of cold air
Convection of warm air
The wind Born is a
warm Anabatic wind
cold Katabatic wind
violent W'ly wind
light maritime E'ly wind
Will a SPECI be issued when the mean speed has changed by
< 09 kt
10 kt or more
less than 10 kt
> 08 kt
Highest annual rainfall over the earth occurs the regions?
Temperate regions
Tropical regions
Polar regions
Equatorial regions
The most hazardous area for aviation in a cyclone is
about 400 km from eye
eye of the cyclone
wall cloud around the eye
allover the cyclone
The ITCZ
is a region of calm winds and layer type of clouds
affects only N hemisphere in winters
usually lies along the Equatorial Trough
affects S hemisphere in monsoon
The strong W'ly winds which blow in both the hemispheres between 35° and 60° Lat are called:
Roaring Forties
Trades
Jetstreams
Polar W'ly
Cold core low pressure system
intensifies with height
weakens with height
does not change with height
veers with height
