ATPL meteorology 050: practice questions and syllabus
Meteorology is ATPL paper 050, the one with the most questions in the exam. The syllabus has ten topics, from the atmosphere and wind to fronts, climatology, flight hazards and meteorological information. With 2,209 questions, it is the largest module of our ATPL bank.
- explained questions in the bank
- 2,209
- in the EASA paper
- 84 q. · 120 min
- pass mark per paper (EASA)
- 75 %
What the syllabus covers
The topics of the EASA syllabus for this subject, with what each one lists.
050 01The atmosphere
composition and vertical division, temperature, pressure, density, International Standard Atmosphere (ISA), altimetry.
050 02Wind
definition and measurement, primary cause, general circulation, local winds, mountain waves, turbulence, jet streams.
050 03Thermodynamics
humidity, changes of state of water, adiabatic processes.
050 04Clouds and fog
cloud formation and description, fog, mist, haze.
050 05Precipitation
development and types of precipitation.
050 06Air masses and fronts
air masses, fronts.
050 07Pressure systems
principal pressure areas, anticyclones, non-frontal depressions, tropical revolving storms.
050 08Climatology
climatic zones, tropical climatology, typical weather situations in the mid-latitudes, local winds and associated weather.
050 09Flight hazards
icing, turbulence, wind shear, thunderstorms, tornadoes, inversions, stratospheric conditions, hazards in mountainous areas, visibility-reducing phenomena.
050 10Meteorological information
observations, weather charts, information for flight planning, meteorological services.
Source: EASA, Easy Access Rules for Aircrew (AMC to Part-FCL)
The illustrated course
To understand before you answer: 14 chapters and 157 key points, 157 of them with a diagram or an illustration. The first chapter, « The atmosphere, radiation and the standard atmosphere », is free to read.
- The atmosphere, radiation and the standard atmosphere
- Pressure, isobaric surfaces and altimetry
- Wind, from the surface to jet streams
- Humidity, thermodynamics and stability
- Clouds and precipitation
- Visibility, mist and fog
- Air masses, fronts and disturbances
- Pressure systems
- General circulation and climatology
- Terrain, breezes and local winds
- Icing
- Thunderstorms and convective phenomena
- Turbulence, CAT and wind shear
- Weather messages and charts
3 questions to practise
Taken from the site's English bank and checked one by one. Read the question, choose your answer, then open the explanation. Like every explanation on the site, they may contain errors.
Question 1 · 050 01 The atmosphere
QNH is defined as
- Apressure at MSL in the standard atmosphere
- BQFE reduced to MSL using the values of the standard atmosphere
- CQFE reduced to MSL using the values of the actual atmosphere
- Dpressure at MSL in the actual atmosphere
Show the answer+
Answer: B. QFE reduced to MSL using the values of the standard atmosphere
QNH is defined as QFE (station pressure) reduced to mean sea level using standard atmosphere values.
Question 2 · 050 02 Wind
The most frequent wind direction in a valley caused by thermal effects is toward the :
- Avalley during daylight as much as at night.
- Bvalley during daylight hours.
- Cmountain during daylight hours.
- Dmountain at night.
Show the answer+
Answer: C. mountain during daylight hours.
Thermally driven valley winds blow up toward the mountain (upslope, anabatic) during daylight hours, as heated air rises along the slopes.
Question 3 · 050 04 Clouds and fog
Which of the following types of clouds are evidence of unstable air conditions?
- ASC, NS.
- BCU, CB.
- CCI, SC.
- DST, CS.
Show the answer+
Answer: B. CU, CB.
Cumulus and cumulonimbus (CU, CB) clouds are evidence of unstable atmospheric conditions.
7 more free questions, no sign-up: Free ATPL meteorology questions
How to approach this subject
Practise decoding METAR, TAF and SIGMET, then learn the reference figures: an isothermal layer at −56.5 °C from 11 to 20 km in the standard atmosphere, a TREND valid for 2 hours, about 27 ft per hPa near the ground, a warm front where warm air slides over cold air and a cold front where cold air pushes under warm air. For wind, Buys Ballot's law (back to the wind, low pressure on your left, in the northern hemisphere) is the anchor.
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