303 Flashcards

1
Q

Define Fog

A

A suspension of either water droplets, ice crystals or both at the surface of the earth.

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2
Q

What condition must be occurring, and what are the 2 ways condensation can occur for fog to form

A

An inversion must be present
the air must be cooled to it’s dew point
water vapour must be added to the air to bring the dewpoint up to the temperature

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3
Q

3 factors that control the evolution of fog

A

Cooling of the air
addition of water vapour
mixing

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4
Q

What are the types of fog caused by cooling of the air

A

upslope fog is formed as a result of adiabatic cooling
radiation fog is formed as a result of radiation cooling
advection fog is formed as a result of advection cooling

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5
Q

what are the types of fog caused by adding water vapour to the air

A

Frontal fog (warm rain fog)
Steam fog, arctic steam fog
ice fog

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6
Q

radiation fog

A

-earth continues to re-radiate suns energy after sun sets, cooling the earth
-cool earth cools warmer air above it
-temperature decreases to dewpoint, saturation occurs
-relatively warm air over cold land surface
-forms on land on clear days, usually in the morning
requires
-clear night
-light winds (3-5kts)
-high RH
-condensation nuclei

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7
Q

Advection fog

A
  • Moist warm air moves over a relatively cold surface
  • moderate wind speed (13-17 kts)
  • high RH
  • Condensation nuclei
  • can form on land or water
  • will not dissipate over water during the day
  • if wind speeds are higher, clouds will form at the top of the turbulent layer, lower wind will mean a thinner layer of fog
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8
Q

Upslope fog

A
  • air is lifted adiabatically and cools by expansion to dew point
  • moderate wind speed (higher speed will cause cloud)
  • high RH
  • condensation nuclei
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9
Q

Pre-frontal fog

A

-warm rain falls through cold nearly saturated air
-evaporation takes place, supersaturation occurs, extra water vapour condenses.
-forms ahead of a warm front and in cold air after cold frontal passage
-warm air over cold air
-warm frontal precipitation
-high RH
-Condensation nuclei
-

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10
Q

Steam fog

A
  • water vapour is released from warm water to cooler air above
  • condensation occurs when dewpoint is raised to temperature
  • shallow unstable layer of air above water surface
  • happens in arctic when air moves from an ice covered surface to warmer water.
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11
Q

Ice Fog

A
  • Man made
  • very cold temps
  • strong surface inversion
  • formed from ice crystals caused by the addition of water vapour through fuel combustion
  • will build up if winds are light
  • -30c
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12
Q

2 factors that control the dissipation of fog

A
  • heating of the air

- decrease in water vapour

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13
Q

4 ways of heating the air

fog dissipation

A
  • solar radiation
  • advection over a warm surface
  • adiabatic heating
  • turbulent mixing
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14
Q

2 ways of decreasing water vapour

fog dissipation

A
  • turbulent mixing of fog with drier air above

- condensation of water vapour in the form of dew or hoar frost

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