Correct: D)
Explanation: Condensation (gas to liquid) is exothermic — it releases latent heat that was absorbed during evaporation. This released heat is a key energy source for thunderstorm development and cloud growth. Sublimation (A, solid to gas), evaporation (B, liquid to gas), and melting (C, solid to liquid) all absorb heat from the environment. Only condensation and deposition release energy.
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- A) 1
- B) 2
- C) 4
- D) 3
Correct: D)
Explanation: Position 3 on the leeward side of the ridge experiences the strongest downdraughts as airflow descends and accelerates in the lee-side subsidence and rotor zone. Positions 1 and 4 on the windward slope have updrafts. Position 2 near the crest is transitional. Lee-side downdraughts are a significant hazard for gliders crossing ridges.
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- A) Rapid and regular variations.
- B) A fall.
- C) A rise.
- D) No change.
Correct: C)
Explanation: The chart shows an anticyclone approaching point B. As a high-pressure system moves closer, local barometric pressure rises. Option A (rapid variations) is associated with convective activity. Option B (fall) would apply if a depression were approaching. Option D (no change) is unlikely with a moving pressure system.
Correct: C)
Explanation: Flight levels use standard pressure (1013.25 hPa). Flying from higher QNH (1020) to lower QNH (1005), the aircraft enters progressively lower-pressure air where pressure surfaces sit at lower true altitudes. The rule "high to low, look out below" applies — true altitude decreases while the flight level remains constant. Option D reverses the relationship.
Correct: C)
Explanation: When temperature rises from 18°C to 28°C, the saturation vapour pressure increases substantially while actual moisture stays constant. The ratio (relative humidity) therefore decreases. Options A and D wrongly claim an increase. Option B ignores the fundamental temperature dependence of relative humidity.
Correct: A)
Explanation: Cooling from below weakens the temperature gradient — the bottom cools while the top stays warm, reducing the lapse rate and increasing stability. This favours stratiform cloud and fog, not convection. Option B is wrong because cooling increases relative humidity. Option D contradicts the stable conditions. Option C has no direct relationship.
Correct: D)
Explanation: GAFOR validity (06:00-12:00 UTC) in CEST (UTC+2): block 1 = 08-10 LT, block 2 = 10-12 LT, block 3 = 12-14 LT. "DDO": D (difficult), D (difficult), O (open). At 13:00 LT (= 11:00 UTC), block 3 applies = O (open). Options A, B, C misidentify the time block or condition.
Correct: D)
Explanation: Rising air enters lower-pressure layers, expanding adiabatically — volume increases. This expansion converts internal energy into work, cooling the air at approximately 1°C/100 m (DALR). Options A and B incorrectly say volume decreases. Option C incorrectly says temperature increases.
Correct: D)
Explanation: Drizzle consists of tiny droplets falling at light intensity from low stratus, causing only minor visibility reduction and no structural damage. Hail (C) causes severe structural damage. Heavy snowfall (A) drastically reduces visibility and causes icing. Rain showers (B) involve turbulence and reduced visibility. Drizzle is the least threatening.
Correct: C)
Explanation: Freezing rain requires warm air aloft (above 0°C) overriding a shallow sub-zero surface layer — the hallmark of a winter warm front. Rain from the warm layer passes through the freezing layer and supercools. Summer (A, D) rarely has sub-zero surfaces. Cold fronts (B, D) undercut warm air rather than overriding it, preventing the necessary warm-over-cold layering.
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- A) Wind from NNE, 120 kt
- B) Wind from NNE, 70 kt
- C) Wind from SSW, 70 kt
- D) Wind from SSW, 120 kt
Correct: C)
Explanation: The symbol shows wind from SSW with one pennant (50 kt) and two long barbs (20 kt) = 70 kt total. Wind barbs point FROM the wind source. Options A and B incorrectly identify the direction as NNE. Option D overstates the speed.
Correct: C)
Explanation: Advection fog forms when warm, moist air is transported horizontally over a colder surface, cooling from below to the dew point. Radiation fog (A) forms on calm clear nights from radiative cooling. Orographic fog (B) forms from terrain-forced lifting. Sea spray (D) is not a fog type.
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- A) Westerly wind situation
- B) Bise situation
- C) South Foehn situation
- D) North Foehn situation
Correct: C)
Explanation: The sketch shows South Foehn (Sudföhn): air driven from the south over the Alps, losing moisture on the Italian side, then descending warm and dry on the northern slopes. Option A (westerly) involves Atlantic air. Option B (Bise) is a cold northeast wind. Option D (North Foehn) has the flow reversed, descending on the southern side.
Correct: C)
Explanation: QFE is the atmospheric pressure at the aerodrome reference point. Setting QFE causes the altimeter to read zero on the ground and height above the aerodrome (AAL) in flight. QNH (A) shows altitude above MSL. QFF (B) is a meteorological reduction not used for altimetry. QNE (D) is the standard pressure for flight levels.
Correct: A)
Explanation: "29004KT 220V340": 290° = WNW direction, 04 = 4 knots speed, varying between 220° (SW) and 340° (NNW). Options B and C misread 290° as ESE (which would be ~110°). Option D has the correct mean direction but wrong variability range.
Correct: C)
Explanation: When a cold front encounters warm unstable air in European summer, forced lifting triggers vigorous convection and cumulonimbus (thunderstorm) cloud development. Stratiform clouds (A) require stable air. Temperature falls, not rises (B), after cold front passage. Pressure rises, not drops (D), as dense cold air replaces the warm sector.
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- A) Gradual temperature increase, tailwind, isolated thunderstorms.
- B) Gradual temperature decrease, headwind, isolated thunderstorms.
- C) Gradual temperature increase, headwind, no thunderstorms.
- D) Gradual temperature decrease, tailwind, isolated thunderstorms.
Correct: B)
Explanation: Flying from LOWK (Klagenfurt) northward to EDDP (Leipzig), temperatures decrease with latitude, the synoptic pattern indicates headwind conditions, and summer convective activity produces isolated thunderstorms. Option A wrongly predicts warming and tailwind. Option C denies thunderstorm risk. Option D identifies a tailwind, which contradicts the chart.
Correct: D)
Explanation: Cumulonimbus (Cb) clouds produce the heaviest showers, hail, and thunderstorms. They extend from near the surface to the tropopause with enormous water and ice content. Nimbostratus (A) produces steady rain, not heavy showers. Altostratus (B) produces light precipitation. Cirrocumulus (C) does not produce significant precipitation.
Correct: B)
Explanation: Geostrophic wind blows parallel to isobars with low pressure to the left in the Northern Hemisphere. With low pressure north and high south, the pressure gradient points north, Coriolis deflects right, producing westward flow. The balloon is carried west. Options A, C, D misapply the Buys-Ballot law.
Correct: B)
Explanation: When terrain mechanically forces air upward into moist, unstable layers, the resulting convective storms are orographic thunderstorms — driven by topographic lifting rather than frontal forcing (A, D) or purely thermal heating (C). They are common over mountain ranges in summer and can be persistent because the terrain continuously feeds the lift.
Correct: C)
Explanation: Advection fog forms when warm, moist air moves horizontally over a colder surface and cools from below to the dew point. Cold air over warm water (A) produces steam fog. Evaporation from warm ground into cold air (B) describes mixing fog. Cooling on a cloudy night (D) prevents the radiative cooling needed for fog because clouds block radiation.
Correct: A)
Explanation: Advection fog results from horizontal transport of warm, moist air across a cold surface, which cools the air from below to its dew point. Option B describes mixing fog. Option C describes radiation fog. Option D (cold air over warm ground) would warm the air, decreasing humidity and preventing fog.
Correct: B)
Explanation: During cold front passage, pressure briefly falls (pre-frontal trough) then rises sharply as cold dense air moves in — the classic V-shaped barograph trace. Options A and D describe monotonic trends. Option C suggests no weather activity. Only option B captures the characteristic fall-then-rise signature.
Correct: A)
Explanation: The polar front is the semi-permanent boundary separating warm subtropical air from cold polar air across mid-latitudes, where extratropical cyclones form. A cold front (B) is the advancing edge of cold air within a cyclone. A warm front (D) is the advancing warm air boundary. An occlusion (C) forms when a cold front overtakes a warm front. None of these are the large-scale climatological boundary.
Correct: C)
Explanation: Summer highs produce widely spaced isobars (weak gradients, light synoptic winds), allowing locally driven thermal circulations (valley breezes, sea breezes, slope winds) to develop. Option A contradicts itself (close isobars do not produce calm winds). Options B and D describe strong wind patterns associated with lows.
Correct: B)
Explanation: Winter highs produce subsidence inversions trapping cold moist air near the surface, creating widespread high fog (Hochnebel) and stratus with light winds. Option A (frontal weather) belongs to lows. Option C (thunderstorms) requires instability absent in winter highs. Option D describes summer high-pressure conditions.
Correct: B)
Explanation: The most dangerous icing occurs between 0°C and -12°C where supercooled liquid water droplets are most abundant and largest. Below -20°C (D), most water has frozen to ice crystals that bounce off. Range A extends above freezing where icing cannot occur. Range C is mostly above freezing.
Correct: A)
Explanation: Clear ice (glaze) forms from large supercooled droplets that flow back along the surface before freezing, creating a smooth, dense, transparent, very heavy layer that is extremely difficult to remove. Rime ice (D) forms from small droplets freezing instantly on contact. Mixed ice (B) combines both. Hoar frost (C) forms by vapour deposition, not droplet impact.
Correct: A)
Explanation: Thermal thunderstorms need conditional instability (becomes unstable once air reaches saturation), high surface temperature (strong trigger), and high humidity (latent heat fuel). Absolutely stable atmospheres (B, C) suppress convection. Low temperature and humidity (D) deny the storm its trigger and energy source.
Correct: D)
Explanation: The cumulus (developing) stage features exclusively updrafts building the cloud vertically — no downdrafts or precipitation have developed yet. The mature stage (A) has both updrafts and downdrafts. The dissipating stage (C) is downdraft-dominated. "Upwind stage" (B) is not a recognised meteorological term.