Nature of the Atmosphere (part 3) Flashcards

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1
Q

Is frost considered to be hazardous to flight? Why? (AC00-6)

A
  1. The rough surface of frost spoils the smooth flow of air over an airfoil, therefore causing a slowing of airflow
  2. This slowing of the air causes early airflow separation, resulting in a loss of lift
  3. Even a small amount of frost on airfoils may prevent an aircraft from becoming airborne at normal takeoff speed
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2
Q

What factors must be present for a thunderstorm to form? (AC00-6)

A
  1. Sufficient water vapor
  2. An unstable lapse rate
  3. An initial upward boost (lifting) to start the storm process in motion
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3
Q

What are the three stages of a thunderstorm? (AC00-6)

A
  1. Cumulus stage: Updrafts cause raindrops to increase in size
  2. Mature stage: Rain at earth’s surface; it falls through the updrafts; lightning; perhaps roll clouds
  3. Dissipating stage: Downdrafts while the rain begins to dissipate
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4
Q

What is a temperature inversion? (AC00-6)

A
  1. An inversion is an increase in temperature with height
  2. An inversion aloft permits warm rain to fall through cold air below, which could be critical to icing
  3. A ground-based inversion favors poor visibility by trapping fog and smoke into low levels of the atmosphere; the air is stable, with little or no turbulence
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5
Q

How does fog form? (AC00-6)

A
  1. Fog forms when the temperature and dewpoint of the air become identical (or nearly so)
  2. Cooling of the air to a little beyond its dewpoint produces radiation fog, advection fog, or upslope fog
  3. Adding moisture and thereby elevating the dewpoint produces frontal fog or steam fog
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6
Q

What causes radiation fog to form? (AC00-6)

A
  1. The ground cools the adjacent air to the dew point on calm, clear nights
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7
Q

What is advection fog, and where is it most likely to form? (AC00-6)

A
  1. Advection fog results from the transport of warm humid air over a cold surface (primarily along coastal areas during the winter)
  2. Unlike radiation fog, it may occur with winds and cloudy skies, at any time of the day or night
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8
Q

What is upslope fog? (AC00-6)

A
  1. Upslope fog forms as a result of moist, stable air being cooled as it moves up sloping terrain; Once the upslope wind ceases, the fog dissipates
  2. Upslope fog is often quite dense and extends to high altitudes
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9
Q

Define the term wind shear, and state the areas in which it is likely to occur? (AC00-6)

A
  1. Wind shear is defined as the rate of change of wind velocity (direction and/or speed); conventionally expressed as vertical or horizontal wind shear
  2. It may occur at any level in the atmosphere but three areas are of special concern: low-level temperature inversion, frontal zone or thunderstorm, and Clear air turbulence (CAT) at high levels associated with a jet stream or strong circulation
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10
Q

Why is wind shear an operational concern to pilots? (AC00-6)

A
  1. Unexpected changes in wind speed and direction can be very hazardous to aircraft operations at low altitudes on approach and departure from airports
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11
Q

What types of weather information will you examine to determine if wind shear conditions might affect your flight? (AC 00-54)

A
  1. PIREPs
  2. METARs
  3. SIGMETS, and convective SIGMETS
  4. Terminal forecasts
  5. LLWAS (low level windshear alert system) reports—installed at 110 airports in the U.S.
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