Visibility and Fog Flashcards

1
Q

Describe runway visual range

A

The distance over which a pilot of an aircraft on the centreline of the runway can see the runway surface markings delineating or identifying its centre line.

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2
Q

How is the runway visual range obtained?

A

Sensors positioned near the threshold (for the touchdown zone) and at the midway point and stop-end of the runway.

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3
Q

How does an increase in altitude affect one’s visibility?

A
  • The brightness of the sky decreases with height. This factor becomes more apparent at high altitudes such as the Tropopause.
  • At high altitudes, the lack of dust, haze and cloud will make it harder for the eye to focus.
  • The eye will focus between close and long distances, for that reason, it is difficult to see and locate objects such as other aircraft flying at altitude.
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4
Q

List the requirements in order for radiation fog to form?

A
  • High relative humidity (little cooling needed to saturate the surface air).
  • Clear sky (so T.R. can readily escape).
  • Light wind (mixing within the surface air layer is assured).
  • Generally stable atmosphere (so that mixing and cooling are confined to a shallow layer).
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5
Q

Discuss why light wind is a factor that affects the extent of fog?

A
  • Necessary to maintain radiation fog.

- Prevents them from lifting into stratocumulus clouds.

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6
Q

Discuss why subsidence is a factor that affects the extent of fog?

A

Subsidence that accompanies an anti-cyclone is likely to produce stability of air, thus preventing the fog bank from lifting off the surface.

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7
Q

Discuss why clear skies are a factor that affects the extent of fog?

A

Associated with anticyclones prevent T.R. from escaping.

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8
Q

When does radiation fog usually form?

A

Night

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9
Q

Is it possible for radiation fog to form after sunrise, if so how?

A
  • Yes
  • When the RH is high (but a lack of mixing at right prevented its formation).
  • The mixing from solar input after sunrise and demand for latent heat as some surface moisture evaporates may cause radiation fog to form after sunrise.
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10
Q

Regarding radiation fog, how can mixing intensify?

A

After sunrise, the particles in the friction layer warm-up and move around more.

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11
Q

What will happen to the fog bank when mixing intensifies?

A

Top of the fog bank will experience this turbulence, causing the height of the fog bank to increase.

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12
Q

What will initially happen when there is solar input into the fog? What does the process require?

A
  • Encourages droplets at and near the top to evaporate.

- Requires latent heat, which is drawn from wherever it is available, including from the air above the bank.

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13
Q

What will cause the steepening of the ELR regarding radiation fog? (dispersal of radiation fog)

A
  • Solar radiation has a limited ability to penetrate moisture and also has some warming effect of the water content within the fog bank.
  • These factors combined causes a steepening of the ELR.
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14
Q

What causes a cloud to form with regards to ELR and radiation fog? (dispersal of radiation fog)

A
  • Fog will lift the surface in places, causing a few holes to appear and direct solar input onto the surface which further steepens the ELR.
  • This causes a layer of cloud to form, taking the form of low stratus but can turn into stratocumulus.
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15
Q

How does surface air cooling occur regarding advection fog?

A
  • Whereas radiation fog involves the relatively rapid cooling of the surface.
  • Advection fog requires a surface that is already cold so that when moist air is transported over it, the air can cool to temperatures lower than dewpoint.
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16
Q

Can advection fog form only on land?

A

No, it can form both on water and land.

17
Q

How long can advection fog last for?

A

Days, perhaps even weeks.

18
Q

How does dispersal of advection fog occur?

A
  • Change in direction or strength of the wind.

- Less moist air being advected into the region when there is advection fog