Kotsch - Weather for the Mariner - Fog Flashcards
1
Q
Fog - results from…
A
- cooling air that remains at earth’s surface
2
Q
Fog - Dew Point is…
A
- temperature a given parcel of air must be cooled for saturation to occur
- at constant pressure and water vapor content
3
Q
Fog - Dew point spread is…
A
- difference between air temperature and dew point
- fog is imminent as spread approaches zero
4
Q
Fog - dew point of maritime air masses are…
A
- higher than land air masses
5
Q
Fog - dew point - higher vs. lower temperature changes
A
- small rise in higher temperatures allows for much more water vapor accommodation than same rise in lower temperatures
- takes longer to dissipate fog in winter than summer
6
Q
Fog - Radiation fog is favorable during…
A
- autumn and winter
7
Q
Fog - Radiation fog occurs with these factors present…
A
- nightime
- land based
- clear sky
- light wind, ﹤15 kts
- high relative humidity at sunset
8
Q
Fog - Radiation fog occurs when…
A
- small decrease in night temperature reaches dew point
9
Q
Fog - Radiation fog is land based because…
A
- heating qualities of water
- water surfaces day/night temperature change is ≤ 3℉
10
Q
Fog - Radiation fog collects…
A
- in valley bottoms and shorelines where the cool air drains to
11
Q
Fog - Radiation fog usually dissipates…
A
- 1-3 hours after sunrise
12
Q
Fog - Advection fog occurs when…
A
- day or night
- warmer air blows over colder surface (land or water) cooling the air to the dew point
- the cooling air becomes more stable and does not rise
13
Q
Fog - Advection fog over the sea with wind
A
- still forms with wind ≤ 30 kts due to less friction over the water
14
Q
Fog - Advection fog - reasons for colder water surface
A
- cold water current (ie. Labrador Current)
- cold upwelling of water (ie. off northern California coast)
- contrasting water temps (ie. Bering Sea colder than North Pacific along Aleutians)
- river drainage of colder fresh water (less dense) into relatively warm salt water (ie. northern Gulf of Mexico in winter)
15
Q
Fog - Tropical-Air fog is…
A
- advection fog from the gradual cooling of air as it travels to higher latitudes