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Dew , Frost and Fog

Dew , Frost and Fog. Dew. Condensation on surface when temperature falls to the dew point temperature Often occurs on cold, clear nights in areas open to the sky? Why surface emits infrared radiation to space, cooling surface Dew forms when temperature drops to the dew point. Dew.

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Dew , Frost and Fog

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  1. Dew, Frost and Fog

  2. Dew • Condensation on surface when temperature falls to the dew point temperature • Often occurs on cold, clear nights in areas open to the sky? • Why surface emits infrared radiation to space, cooling surface • Dew forms when temperature drops to the dew point

  3. Dew • Often associated with periods when high pressure (a.k.a., an anticyclone) 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!

  4. Car’s in the open can get covered with dewCars in a carport gather little dewWhy?

  5. Dew Protection: Roof Lessens Infrared Cooling to Space

  6. More Dew Facts • More dew after a moist period or in moist areas. Higher dew point! • Dew releases latent heat of condensation and reduces temperature drops after it starts to form

  7. Frost

  8. 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 (a.k.a. frost point) is at or below 0C • Frost tends is most frequent in low-lying areas, since cold air is denser than warm air.

  9. Frost is a problem for orchards in eastern Washington • Damages sensitive buds • Ways to attack the problem: • Fans • Heaters • Spraying water

  10. FOG

  11. 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 too different air masses that are not saturated, but are when mixed

  12. Types of Fog • Radiation • Advection • Upslope • Frontal • Steam fog

  13. 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 mixing cooling into lower atmosphere, where the cools to the dew point

  14. Radiation Fog • Light winds (2-7 knots) ideal. Why? Just the right amount of mixing. • The major fog here in the Northwest

  15. Radiation Fog

  16. If winds are very light: Ground Fog

  17. How deep? • Radiation fog can range from a few inches (ground fog) to a few hundred meters in depth (with moderate wind)

  18. Often associated with high pressure

  19. When is the foggiest time of the year here in the Northwest away from the Pacific?Why?

  20. The Answer • Early Fall • Long night • Still clear or partly cloud nights • Surface is moister • Atmosphere is relatively stable

  21. Radiation Fog Can Fill the InteriorValley of CATule Fog

  22. Advection Fog

  23. Advection Fogadvection: the transfer of heat or matter by the flow of a fluid, especially horizontally in the atmosphere or the sea.advection: the horizontal transfer of any atmospheric property by the wind • Occurs when warm, moist air moves over a cooler surface • For the west coast. We have cold water along the West Coast during late spring into fall. • When warm, moist air from the Pacific goes over cool coastal water, can get saturation and fog.

  24. Why is the Pacific Coast cool?Upwelling of colder subsurface water

  25. Mark Twain Quote  “The coldest winter I ever spent was a summer in San Francisco.”

  26. Advection Fog • Coastal New England due to cold water along the coast and the warm Gulf Stream to the south

  27. Advection fog over snow

  28. Upslope Fog

  29. Upslope Fog • Air moving up a slope cools adiabatically producing saturation and fog • Bad for skiers.

  30. Upslope Fog: Snoqualmie Pass

  31. FRONTAL FOG

  32. Frontal Fog

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