Private Pilot · Chapter 8 of 14

Weather Theory

12 free practice questions from the 259 in this chapter of StudyWren Aviation. Pick an answer and check it to see the explanation and its FAA source. Part of the free Private Pilot practice test.

Atmosphere PAR-08-002

In which layer of the atmosphere does nearly all weather occur?

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The answer is C: Troposphere

The troposphere extends from the surface to the tropopause and contains almost all of the atmosphere's water vapor, so clouds, precipitation, and most weather form there. The stratosphere above is very dry and has little weather.

Source: FAA-H-8083-28 Ch. 4 ACS PA.I.C

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Standard Atmosphere & Lapse Rates PAR-08-010

What are the standard sea-level temperature and pressure in the International Standard Atmosphere?

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The answer is A: 15°C and 29.92 inches of mercury

ISA sea-level conditions are 15°C (59°F) and 29.92 inches of mercury (1013.2 hPa). The 59 figure is the Fahrenheit value, not Celsius.

Source: FAA-H-8083-28 Ch. 4 ACS PA.I.C

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Pressure Systems & Wind PAR-08-031

How does the strength of the Coriolis force vary with latitude?

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The answer is A: It is zero at the equator and greatest at the poles

The Coriolis effect increases with latitude, from zero at the equator to a maximum at the poles, and it also increases with wind speed. This is why large rotating storm systems do not form right at the equator.

Source: FAA-H-8083-28 Ch. 10 ACS PA.I.C

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Global & Local Winds PAR-08-051

In winter, the temperature at an airport just east of the Rocky Mountains rises sharply within an hour as a gusty westerly wind descends the slopes. What is this wind?

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The answer is B: A Chinook (foehn) wind

Air that lost moisture on the windward side descends the lee slope and warms by compression at the dry adiabatic rate, arriving warm and dry. Chinooks can raise lee-side temperatures sharply in a short time and are often gusty and turbulent. A valley breeze flows upslope, not down.

Source: FAA-H-8083-28 Ch. 12, Ch. 16 ACS PA.I.C

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Moisture & Temperature/Dewpoint PAR-08-063

An airplane is parked outside on a clear, calm night. Under what condition will frost form on its wings?

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The answer is B: The wing surface cools to the dewpoint, which is below freezing

Frost forms by deposition: water vapor changes directly to ice on a surface that has cooled to a dewpoint that is below freezing. Rain freezing on contact produces glaze (clear) ice, not frost.

Source: FAA-H-8083-28 Ch. 6 ACS PA.I.C

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Atmospheric Stability PAR-08-087

When an entire layer of air is lifted and stretched vertically, how does its stability tend to change?

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The answer is C: Its stability decreases

As a layer is lifted and stretched, its top cools more than its bottom, steepening the lapse rate and decreasing stability. Sinking (subsidence) does the opposite and increases stability.

Source: FAA-H-8083-28 Ch. 13 ACS PA.I.C

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Clouds PAR-08-093

Before a summer cross-country, you see altocumulus castellanus (turret-shaped clouds at middle levels) in the morning sky. What do they indicate?

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The answer is C: Instability at middle levels that favors later convection

PHAK describes castellanus as clouds with a common base and separate, castle-like vertical development, and the Aviation Weather Handbook lists altocumulus among the visible forms of convection. Turrets at middle levels therefore show unstable air aloft, an early sign that convection, including thunderstorms, may build as the day warms.

Source: PHAK Ch. 12 FAA-H-8083-28 Ch. 13 ACS PA.I.C

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Precipitation PAR-08-107

While climbing in cloud, you begin encountering freezing rain. What does this indicate about the air above you?

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The answer is C: A layer of above-freezing air exists at a higher altitude

Freezing rain begins as rain (or melted snow) in a warmer layer aloft and becomes supercooled as it falls into below-freezing air. Its presence means there is a temperature inversion with above-freezing air higher up.

Source: FAA-H-8083-28 Ch. 14 ACS PA.I.C

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Air Masses PAR-08-135

An air mass labeled cP is

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The answer is B: continental polar: cold and dry

In an air-mass label the lowercase letter shows the moisture source (c = continental, dry; m = maritime, moist) and the capital letter the temperature source (P = polar, cold). cP air forms over cold northern land such as Canada, so it is cold and dry.

Source: FAA-H-8083-28 Ch. 11 ACS PA.I.C

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Thunderstorms PAR-08-161

You are watching a large cumulus cloud build near your route. Which observation signals that it has entered the mature stage?

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The answer is A: Precipitation starts reaching the ground from the cloud

The mature stage begins when precipitation falls out of the cloud base and reaches the surface, dragging air down into strong downdrafts alongside the remaining updrafts. Downdrafts throughout the cell indicate the dissipating stage.

Source: FAA-H-8083-28 Ch. 22 ACS PA.I.C

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Turbulence PAR-08-198

Relative to the jet stream core, where is clear air turbulence most frequently encountered?

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The answer is C: On the polar (low-pressure) side, especially near upper troughs

The strongest wind shear, and therefore CAT, tends to occur on the cold, low-pressure side of the jet core and where the jet curves sharply around deep upper troughs.

Source: FAA-H-8083-28 Ch. 19 ACS PA.I.C

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Weather & Temperature Effects on Flight PAR-08-233

You are flying VFR up a mountain valley toward a pass. Clouds are lowering over the ridges, and light precipitation is falling ahead. What hazard is developing?

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The answer is A: Mountain obscuration, with terrain hidden in cloud ahead

Low clouds and precipitation can hide ridges and passes, leaving no room to turn around in a narrowing valley. Mountain obscuration is a major cause of VFR flight into terrain; turn back early while visual references remain.

Source: FAA-H-8083-28 Ch. 18 ACS PA.I.C

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