Correct: B)
Explanation: The CB (cumulonimbus) is the most dangerous cloud: severe turbulence, lightning, hail, wind shear, icing.
Correct: D)
Explanation: Thunderstorms = slack pressure gradient (low pressure gradient) + strong surface heating (instability) + high humidity.
Correct: B)
Explanation: Visibility 1–5 km with water droplets = mist (BR). Fog = visibility < 1 km.
Correct: C)
Explanation: Radiation fog: light wind (2 kt), small temperature/dew point spread (1°C), some cloud acceptable. Option (C) has too large a temp/dew point spread.
Correct: C)
Explanation: ISA lapse rate = -2°C/1000 ft. Difference: 8600 - 5600 = 3000 ft. Temperature: 5°C - (3 × 2) = -1°C.
Correct: C)
Explanation: QFE = atmospheric pressure measured at aerodrome level (station). The altimeter reads 0 on the ground.
]
Correct: D)
Explanation: The arrow points towards the wind's origin. One long barb = 10 kt, one short barb = 5 kt. Total = 15 kt from the NE.
Correct: A)
Explanation: 280° = WNW, 15 kt mean, G25 = gusts to 25 kt.
Correct: C)
Explanation: In a METAR, cloud base is given in feet AGL (above aerodrome level).
Correct: A)
Explanation: Buys-Ballot's law: standing with your back to the wind in the northern hemisphere, the low-pressure area is to your left. Wind from the left = low pressure to the left, high pressure to the right.
Source : BAZL/OFAC Série 1 - Branches Communes Synoptic chart:
] T = depression centre. A = warm sector (between warm front and cold front). B = behind the cold front (cold air mass). C = ahead of the warm front (cool air mass). Cold front: blue triangles. Warm front: red semicircles.
Correct: B)
Explanation: Point C lies ahead of the warm front, meaning the depression centre and its associated frontal system are approaching. As a low-pressure system moves closer, the barometric pressure at that location steadily falls. Option A is wrong because an approaching depression always causes pressure changes. Option C (pressure rise) would apply to a location behind a cold front where cold dense air moves in. Option D (rapid irregular variations) is more typical of the immediate vicinity of thunderstorm activity, not the broad-scale approach of a warm front.
Source : BAZL/OFAC Série 1 - Branches Communes
Correct: B)
Explanation: An unstable cold front in summer forces warm, moist, unstable air upward vigorously, triggering strong convection and the development of cumuliform clouds including towering cumulus and cumulonimbus with showers and thunderstorms. Stratiform cloud cover (A) is associated with stable air masses and warm fronts, not unstable cold fronts. Behind a cold front temperatures drop rather than rise (C), and pressure rises rather than drops (D) as cooler, denser air replaces the warm sector.
Source : BAZL/OFAC Série 1 - Branches Communes
Correct: B)
Explanation: When stable warm humid air overrides a cold air mass (the classic warm front mechanism), the warm air ascends gently along the frontal surface, cooling progressively and forming widespread stratiform clouds — from high cirrus down through altostratus to nimbostratus — with continuous, steady precipitation and a lowering cloud base. Option A describes fair-weather conditions unrelated to frontal activity. Option C describes unstable convective weather typical of cold fronts, not warm fronts. Option D combines fog with drying aloft, which is internally contradictory and not a recognised frontal pattern.
Source : BAZL/OFAC Série 1 - Branches Communes
Correct: D)
Explanation: Maritime polar air (mP) originates over cold northern oceans, picking up moisture and becoming unstable as it moves over relatively warmer European land surfaces, producing convective showers year-round. Continental tropical air (A) is warm and dry, producing clear skies rather than showers. Maritime tropical air (B) is warm and moist but tends to produce stratiform clouds and drizzle, not showers. Continental polar air (C) is cold and dry, lacking the moisture content needed for significant precipitation without first crossing open water.
Source : BAZL/OFAC Série 1 - Branches Communes Synoptic chart Switzerland/Alps:
] Anticyclone (H) to the west, depression (T) to the north-east, isobars indicating NW flow over Switzerland.
Correct: C)
Explanation: A northwest flow situation (Nordwestlage) drives moist air against the northern slopes of the Alps, producing continuous orographic precipitation on the north side. The flow also disturbs conditions south of the Alps through spillover effects and forced subsidence turbulence. Option A describes a south-side precipitation event (Stau from the south), not a northwest situation. Option B misplaces the thunderstorms on the wrong side of the Alps. Option D reverses the pattern — clouds would cover the north side, not the south.
Source : BAZL/OFAC Série 1 - Branches Communes Low Level Significant Weather Chart (OGDD70)
] Fixed Time Prognostic Chart — Valid: 09 UTC, 22 JAN 2015 Issued by MeteoSwiss
| Zone | Cloud cover | Cloud base | Cloud top | Visibility | Turbulence | Icing | |------|-----------|-------------|---------------|------------|------------|---------| | A | BKN/OVC SC, AC | 3000 ft | FL080 | > 10 km | MOD below FL080 | MOD FL040-FL080 | | B | BKN/OVC ST, SC | 1500 ft | FL060 | 5-8 km, locally 3 km (BR) | MOD below FL060 | MOD FL030-FL060 | | C | SCT/BKN CU, SC | 4000 ft | FL100 | > 10 km | ISOL MOD | LGT FL050-FL100 |
0°C isotherm: FL040 (north) to FL060 (south). Surface wind: SW 15-25 kt.
Correct: C)
Explanation: Area A features BKN/OVC stratocumulus and altocumulus with moderate icing between FL040 and FL080 and the 0°C isotherm at FL040, indicating mixed precipitation — rain and snow showers — within this zone. Option A incorrectly states no icing or turbulence in area C, whereas the chart shows isolated moderate turbulence and light icing there. Option B mischaracterises area B, which has stratiform clouds (ST, SC), not cumuliform. Option D makes an unsupported claim about warm fronts that cannot be verified from the chart data provided.
Source : BAZL/OFAC Série 1 - Branches Communes
Correct: A)
Explanation: During a sunny summer afternoon, the land heats faster than the sea, causing air to rise over land and drawing cooler air inland from the sea — this is the sea breeze. Since the coastline is to your left and the runway runs parallel to it, the sea breeze blows from the sea (left side) toward the land, creating a crosswind from the left. Options B and C (headwind/tailwind) would require the wind to blow along the runway, not from the coast. Option D would require the sea to be on the right side.
Source : BAZL/OFAC Série 1 - Branches Communes
Correct: B)
Explanation: Transition zones between air masses — i.e., frontal zones — feature steep horizontal temperature and pressure gradients that drive strong winds and generate mechanical and convective turbulence at low levels. The centre of an anticyclone (A) is characterised by calm, subsiding air with light winds. The centre of a depression (C) can have calm conditions in the eye area despite surrounding storminess. Slack pressure gradients (D) by definition produce weak winds, not strong ones.
Source : BAZL/OFAC Série 1 - Branches Communes
Correct: C)
Explanation: Relative humidity is the ratio of the actual water vapour content to the maximum the air can hold at that temperature. When temperature rises from 10°C to 20°C, the air's saturation capacity roughly doubles, but since no moisture is added, the actual vapour content stays the same — so relative humidity decreases significantly. Options A and D wrongly claim humidity increases, which would require either adding moisture or cooling the air. Option B is incorrect because relative humidity is temperature-dependent and cannot stay constant when temperature changes without a corresponding moisture change.
Source : BAZL/OFAC Série 1 - Branches Communes
Correct: C)
Explanation: The Swiss GAFOR divides the validity period (06:00–12:00 UTC) into three two-hour blocks. Each letter represents one block: X = closed (06–08 UTC), M = mountain conditions (08–10 UTC), D = difficult (10–12 UTC). On 1 June, summer time (CEST = UTC+2) applies, so 06–08 UTC = 08–10 LT. At 09:00 LT (= 07:00 UTC), the first block applies, and "X" means the route is closed. Option A and D incorrectly interpret the timing or the code. Option B confuses the category — "M" is not "critical."
]
- A) Wind from NE, 25 kt
- B) Wind from SW, 110 kt
- C) Wind from SW, 25 kt
- D) Wind from SW, 110 kt
Correct: C)
Explanation: Wind barb symbols point in the direction the wind blows from, with barbs on the upwind end indicating speed: a long barb equals 10 kt, a short barb equals 5 kt, and a pennant (triangle) equals 50 kt. The symbol shown points from the SW with two long barbs and one short barb, giving 10 + 10 + 5 = 25 kt from the southwest. Options B and D overstate the wind speed dramatically. Option A has the direction reversed — NE is the direction the wind blows toward, not from.
Correct: B)
Explanation: Radiation fog forms when the ground loses heat by longwave radiation to space on clear, calm nights, cooling the overlying air to the dew point. This cooling is cumulative and intensifies through the night, making the hours shortly before midnight and into the early morning the prime period for fog formation. Option A (afternoon) is when solar heating is strongest, preventing fog. Option C (after sunset) is usually too early for sufficient cooling. Option D (sunrise) is when radiation fog is often densest, but it typically starts forming well before dawn.
]
- A) North Foehn situation
- B) Westerly wind situation
- C) South Foehn situation
- D) Bise situation
Correct: D)
Explanation: The sketch depicts the Bise — a cold, dry northeast wind in Switzerland driven by a high-pressure system over northern or northeastern Europe and lower pressure to the south. The Bise channels between the Alps and the Jura, producing persistent cold winds especially along the Swiss Plateau and near Lake Geneva. Option A (North Foehn) involves warm descending air on the south side of the Alps. Option B (Westerly wind) is associated with Atlantic depressions. Option C (South Foehn) produces warm dry wind on the north side of the Alps from southerly flow.
Correct: C)
Explanation: QNH is the altimeter setting that causes the altimeter to display altitude above mean sea level (AMSL). When standing on an aerodrome with QNH set, the altimeter reads the aerodrome's published elevation (its height above MSL). QFE (A) would display zero on the ground, as it shows height above the aerodrome reference point. QNE (B) is the standard pressure setting (1013.25 hPa) used for flight levels. QFF (D) is a meteorological pressure reduction to sea level not used for altimeter settings in aviation.
Correct: D)
Explanation: In METAR format, the cloud group "BKN012" decodes as BKN (broken = 5–7 oktas of sky coverage) with a base at 012 hundreds of feet, meaning 1,200 ft AGL. Option A misreads the height as 12,000 ft by adding an extra zero. Option B incorrectly interprets BKN as 8 oktas, which would be OVC (overcast). Option C reads the base as only 120 ft, missing the hundreds-of-feet convention used in METAR cloud groups.