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
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.
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
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
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
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
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