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Dew, Frost and Fog
Atmospheric Sciences 101
Autumn 2020
Dew
• Condensation on the surface when temperature
falls to the dew point temperature
• Often occurs on cold, clear nights in areas open
to the sky.
• On such nights, the surface emits infrared
radiation to space, cooling surface to the dew
point
Temperature drops, dew point remains constant until dew forms
Dew
• Often associated with periods when high
pressure is positioned overhead
• Highs are associated with clear skies and
calm or weak winds.
• Why are weak winds good for dew? Less
mixing of warmer air from above!
Clear Skies Allow Infrared
Radiation Cooling from the
Surface
Winds can mix warmer, drier
air down to the surface
Car’s in the open often get
covered with dew
Cars in a carport gather little
dew
Why?
Dew Protection: Roof Lessens Infrared
Cooling to Space
More Dew Facts
• More dew after a moist period or in moist
areas. Why? Higher dew point!
• Dew releases latent heat of condensation
and reduces temperature drops after it starts
to form
Frost
Frosty Facts
• Frost forms by the process of deposition, with
water vapor going directly to ice (frost)
• Frost forms when air temperature drops to the
dew point, when the dew point is at or below
0C (a.k.a. frost point)
• Frost tends is most frequent in low-lying
areas, since cold air is denser than warm air
and flows to low spots.
Frost is a problem for orchards
in eastern Washington
• Damages sensitive buds
• Ways to attack the
problem:
– Fans
– Heaters
– Spraying water
FOG
Fog is a cloud intersecting the
ground
• Can be made of liquid water droplets or ice
crystals (ice fog)
• Can get fog in three ways:
– Cooling air to the dew or frost points
– Adding moisture to the air (increasing dew point)
– Mixing different air masses that are not saturated, but
are when mixed
Types of Fog
• Radiation
• Advection
• Upslope
• Frontal
• Steam fog
Radiation Fog
• Associated with clear or nearly
clear conditions, light winds,
moist layer near the ground
• Earth radiates infrared radiation
to space and cools the surface
• Light turbulence mixes cool air
from surface into lower
atmosphere, which cools to the
dew point
Radiation Fog
• Light winds (2-7 knots) ideal. Why?
Just the right amount of mixing. Too
strong winds mixes too much dry warm
air to the surface.
• Like trying to cool a big house with a
small AC
Fog often associated with high
pressure (which is associated
with clear skies, light winds)
Radiation Fog is the Major Fog
Here in the Northwest
How deep?
Radiation fog can range from a few inches
(ground fog) to a few hundred meters in depth
If winds are very light: Ground
Fog
Fog
from
space
When is the foggiest time of the
year here in the Northwest
away from the Pacific?
Early fall.
Why?
The Answer
Early Fall
– Lengthening nights
– Still clear or partly cloudy
– Surface is moister than in mid-summer
– Atmosphere is relatively stable
(atmosphere is still warm, surface
cooling)
Radiation
Fog Can
Fill the
Interior
Valley of
CA
Tule Fog
Advection Fog
advection: the horizontal
transfer of any atmospheric
property by the wind
Advection Fog
• Occurs when warm, moist air moves over a
cooler surface
• Frequently observed along the West Coast
in summer. There is cold water just
offshore during late spring into fall.
• When warm, moist air from the Pacific goes
over cool coastal water, can get saturation
and fog.
Sea
Surface
Temps
Why is the Pacific Ocean cool along
the coast?
Upwelling of colder subsurface water
Mark Twain Quote
“The coldest
winter I ever spent
was a summer in
San Francisco.”
Also Along the Northeast Coast
• Coastal New
England has fog
due to cold water
along the coast
and the warm
Gulf Stream to
the south
• Warm, moist air
moves northward
Advection fog over snow:
warmer air over a colder
surface
Upslope Fog
Upslope Fog
• Air moving up a slope cools adiabatically
resulting in saturation and fog
• Bad for skiers.
Upslope Fog: Snoqualmie Pass
Frontal Fog: Particularly
north of warm fronts
Frontal Fog
• Precipitation falls into cool air, adding
moisture and bringing the air to saturation.
• Often found north of surface warm fronts.
Steam Fog
Steam Fog
• Often associated with very cold air passing
over warm water
• A difference of 15-20F or more is needed
between the water and air temperatures.
Where are the foggiest
locations in the U.S.?
Average Number of Days with Dense Fog
Foggiest Place in U.S.: Cape Disappointment
106 days per year of heavy fog (<=.25 mile
visibility)
Other neat fog facts
• Fog tends to burn off from the edges
• Fog accumulates in valleys and low areas
• During the day, fog can lift into stratus
Local Fog Issues
• SEA TAC
is fogged
in more
than
Boeing
Field
• MUCH
less fog in
Portland
Reason: SeaTac is on a hill
SEA
BFI
Fog Stratus
Troutdale
Portland has a lot of dry, easterly wind during winter: bad for fog
Fog and Black Ice
Roadway Icing: Often called “Black
Ice”
Dozens of people in WA state are killed by
roadway icing each year. Many hundreds injured.
Biggest Threat: Fog Moving Over
Cold Road
• A typical scenario starts with a clear, cold
night with light winds in which the surface
rapidly cools.
• A light frost occurs on the roadway, with
nearby fog forming over a moist surface.
• The fog drifts over the road, and as it passes
over the road a thick coating of ice is
deposited.
Be Worried…Very Worried
Roadway Icing 101: Temperature
Facts
• Air temperatures are generally
measured at 2 meters (roughly 6 ft)
above the surface.
• Car thermometers measure
temperatures a few feet above the road.
• Temperatures at the surface can be
cooler than air temperature a few
feet above the surface during winter
nights
Surface Temperature
• On cold nights the ground temperature can be
2-6F colder than the official air temperature or
your car thermometer temperature.
• Thus, once the air temperature drops below
roughly 36-37F, you should be careful.
Is ”Black Ice” Really Black?
No, it is nearly clear.
Roadway Icing is Particularly
Bad on Bridges
Why bridges so problematic?
Insulating air under the bridge
No conduction of heat from ground
into bridge

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DewFrostFog101A2020.pptx

  • 1. Dew, Frost and Fog Atmospheric Sciences 101 Autumn 2020
  • 2. Dew • Condensation on the surface when temperature falls to the dew point temperature • Often occurs on cold, clear nights in areas open to the sky. • On such nights, the surface emits infrared radiation to space, cooling surface to the dew point
  • 3.
  • 4.
  • 5. Temperature drops, dew point remains constant until dew forms
  • 6. Dew • Often associated with periods when high pressure is positioned overhead • Highs are associated with clear skies and calm or weak winds. • Why are weak winds good for dew? Less mixing of warmer air from above!
  • 7. Clear Skies Allow Infrared Radiation Cooling from the Surface
  • 8. Winds can mix warmer, drier air down to the surface
  • 9. Car’s in the open often get covered with dew Cars in a carport gather little dew Why?
  • 10.
  • 11.
  • 12. Dew Protection: Roof Lessens Infrared Cooling to Space
  • 13. More Dew Facts • More dew after a moist period or in moist areas. Why? Higher dew point! • Dew releases latent heat of condensation and reduces temperature drops after it starts to form
  • 14. Frost
  • 15.
  • 16. Frosty Facts • Frost forms by the process of deposition, with water vapor going directly to ice (frost) • Frost forms when air temperature drops to the dew point, when the dew point is at or below 0C (a.k.a. frost point) • Frost tends is most frequent in low-lying areas, since cold air is denser than warm air and flows to low spots.
  • 17. Frost is a problem for orchards in eastern Washington • Damages sensitive buds • Ways to attack the problem: – Fans – Heaters – Spraying water
  • 18. FOG
  • 19. Fog is a cloud intersecting the ground • Can be made of liquid water droplets or ice crystals (ice fog) • Can get fog in three ways: – Cooling air to the dew or frost points – Adding moisture to the air (increasing dew point) – Mixing different air masses that are not saturated, but are when mixed
  • 20. Types of Fog • Radiation • Advection • Upslope • Frontal • Steam fog
  • 21. Radiation Fog • Associated with clear or nearly clear conditions, light winds, moist layer near the ground • Earth radiates infrared radiation to space and cools the surface • Light turbulence mixes cool air from surface into lower atmosphere, which cools to the dew point
  • 22.
  • 23. Radiation Fog • Light winds (2-7 knots) ideal. Why? Just the right amount of mixing. Too strong winds mixes too much dry warm air to the surface. • Like trying to cool a big house with a small AC
  • 24. Fog often associated with high pressure (which is associated with clear skies, light winds)
  • 25. Radiation Fog is the Major Fog Here in the Northwest
  • 26. How deep? Radiation fog can range from a few inches (ground fog) to a few hundred meters in depth
  • 27. If winds are very light: Ground Fog
  • 29. When is the foggiest time of the year here in the Northwest away from the Pacific?
  • 31. The Answer Early Fall – Lengthening nights – Still clear or partly cloudy – Surface is moister than in mid-summer – Atmosphere is relatively stable (atmosphere is still warm, surface cooling)
  • 32.
  • 34. Advection Fog advection: the horizontal transfer of any atmospheric property by the wind
  • 35.
  • 36. Advection Fog • Occurs when warm, moist air moves over a cooler surface • Frequently observed along the West Coast in summer. There is cold water just offshore during late spring into fall. • When warm, moist air from the Pacific goes over cool coastal water, can get saturation and fog.
  • 37.
  • 39.
  • 40.
  • 41.
  • 42. Why is the Pacific Ocean cool along the coast? Upwelling of colder subsurface water
  • 43. Mark Twain Quote “The coldest winter I ever spent was a summer in San Francisco.”
  • 44. Also Along the Northeast Coast • Coastal New England has fog due to cold water along the coast and the warm Gulf Stream to the south • Warm, moist air moves northward
  • 45.
  • 46. Advection fog over snow: warmer air over a colder surface
  • 48. Upslope Fog • Air moving up a slope cools adiabatically resulting in saturation and fog • Bad for skiers.
  • 50.
  • 52. Frontal Fog • Precipitation falls into cool air, adding moisture and bringing the air to saturation. • Often found north of surface warm fronts.
  • 54.
  • 55. Steam Fog • Often associated with very cold air passing over warm water • A difference of 15-20F or more is needed between the water and air temperatures.
  • 56.
  • 57.
  • 58.
  • 59.
  • 60. Where are the foggiest locations in the U.S.?
  • 61. Average Number of Days with Dense Fog
  • 62. Foggiest Place in U.S.: Cape Disappointment 106 days per year of heavy fog (<=.25 mile visibility)
  • 63. Other neat fog facts • Fog tends to burn off from the edges • Fog accumulates in valleys and low areas • During the day, fog can lift into stratus
  • 64. Local Fog Issues • SEA TAC is fogged in more than Boeing Field • MUCH less fog in Portland
  • 65. Reason: SeaTac is on a hill SEA BFI Fog Stratus
  • 66. Troutdale Portland has a lot of dry, easterly wind during winter: bad for fog
  • 68. Roadway Icing: Often called “Black Ice” Dozens of people in WA state are killed by roadway icing each year. Many hundreds injured.
  • 69. Biggest Threat: Fog Moving Over Cold Road • A typical scenario starts with a clear, cold night with light winds in which the surface rapidly cools. • A light frost occurs on the roadway, with nearby fog forming over a moist surface. • The fog drifts over the road, and as it passes over the road a thick coating of ice is deposited.
  • 71. Roadway Icing 101: Temperature Facts • Air temperatures are generally measured at 2 meters (roughly 6 ft) above the surface. • Car thermometers measure temperatures a few feet above the road. • Temperatures at the surface can be cooler than air temperature a few feet above the surface during winter nights
  • 72. Surface Temperature • On cold nights the ground temperature can be 2-6F colder than the official air temperature or your car thermometer temperature. • Thus, once the air temperature drops below roughly 36-37F, you should be careful.
  • 73. Is ”Black Ice” Really Black? No, it is nearly clear.
  • 74. Roadway Icing is Particularly Bad on Bridges
  • 75. Why bridges so problematic? Insulating air under the bridge No conduction of heat from ground into bridge