Visibility And Fog Flashcards

1
Q

Define runway visual range (RVR)

A
  • Max distance a pilot 15ft above the runway in the touchdown area can see marker boards by day or runway lights by night.
  • Reported when RVR is below 1500m
  • Measured with Transmissometers
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2
Q

Explain the effect of altitude on visibility.

A
  • Reduction in aerosols with an increase in altitude
  • Visibility increases with an increase in altitude
  • Slant range also increases with altitude.
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3
Q

State the difference between fog, mist and haze.

A
  • Fog = low level cloud with visibility less than 1000m
  • Mist = low level cloud with visibility 1000m to 5000m
  • Haze = solid aerosols with visibility less than 5000m
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4
Q

Describe the principle of formation of radiation and advection fog with respect to required meteorological conditions.

A
  • Radiation fog forms over cold land with high RH.
  • Forms at night and early morning
  • Clear skies and moist air allow radiation to escape
  • Wind 2 to 8kts
  • Advection fog forms over cold sea or land
  • Warm moist air moves over cold surface
  • Wind 5 to 25kts
  • High RH so little cooling required to condense
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5
Q

Describe the principle of formation of radiation and advection fog with respect to factors affecting the extent of the fog.

A
  • Radiation fog forms in valleys because of katabatic effect
  • Occurs in anticyclones, ridges and cols due to subsidence
  • Seasonal changes in surface temperature
  • Direction of wind
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6
Q

Describe the principle of formation of radiation and advection fog with respect to factors affecting the timing of the fog.

A
  • Radiation fog forms in autumn and winter
  • Surface is cooler than air
  • Night and early morning due to lowest temperatures
  • Latest time is can form is 30 minutes after sunrise
  • Advection fog forms over land in winter and early spring
  • Over sea in late spring and early summer
  • Can occur anytime of year when air moves over sea with temperature below dew point
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7
Q

Describe the principle of formation of radiation and advection fog with respect to factors affecting the dispersal of the fog.

A
  • Radiation fog
  • By insolation causing convection, lifting the fog
  • Will also evaporate the lower layers
  • By stronger winds lifting the fog to form stratus cloud
  • Advection fog is affected by a change of air mass from wind direction change.
  • Winds greater than 15kt lift the fog to form St cloud
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