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Meteorology Notes

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* Forming Dew
Radiational cooling of the surface-
Outgoing longwave radiation emitted to space
Surfaces (grass,trees,cars) cool to the “dew” “point”
Air is cooled by “conduction” and reaches its dew point condensation of liquid droplets on surfaces
Dew Formation
More likely to form on nights with clear skies and calm winds
Objects near the ground will emit infradred radiation (clear nights) coldest air is located near the ground (calm winds)
Frost Formation
Radiational cooling of the Surface surfaces (grass,trees,cars) cool below frost point (below freezing).
Air temp reaches frost point (air becomes saturated)
(temp and dew point are equal) deposition of ice onto surfaces also known as hoarfrost or white frost exhibits “tree-like branching pattern.”
FROST IS NOT FROZEN DEW!
Frost forms on objects that are below freezing (vapor)
Frozen dew is dew (liquid) that freezes as temperatures drop
Haze…What Is It?
Dust or salt particles suspended in the air
Morning – Distant objects on the horizon are harder to see
RH is much higher, therefore, water vapor condenses more readily and fills the air
Afternoon – Distant objects on the horizon are easier to see
RH is much lower, therefore, water vapor doesn’t condense as it would in the morning
Hygoscopic – “Water-Seeking.” Ocean salt
Hydrophobic – “water-repelling.” Oils, wax, and gas
Wet haze – tiny liquid drops scatter light and appears dull grey or white
Dry haze – non-water particles appear orange or yellowish
Fog
Fog: a cloud in contact with the ground
Fog froms when condensation begins to form on less active nuclei (usually when the RH is closer to 100%)
Fog droplets grow in size and eventually fall to the ground * Fog is formed in 2 ways
Cooling the air to it’s saturation point (dew point) evaporation and mixing (adding more vapor content to the atmosphere) fog is maintained by:

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