Kotsch - Weather for the Mariner - Fog Flashcards

1
Q

Fog - results from…

A
  • cooling air that remains at earth’s surface
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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
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3
Q

Fog - Dew point spread is…

A
  • difference between air temperature and dew point
  • fog is imminent as spread approaches zero
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4
Q

Fog - dew point of maritime air masses are…

A
  • higher than land air masses
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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
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6
Q

Fog - Radiation fog is favorable during…

A
  • autumn and winter
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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
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8
Q

Fog - Radiation fog occurs when…

A
  • small decrease in night temperature reaches dew point
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9
Q

Fog - Radiation fog is land based because…

A
  • heating qualities of water
  • water surfaces day/night temperature change is ≤ 3℉
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10
Q

Fog - Radiation fog collects…

A
  • in valley bottoms and shorelines where the cool air drains to
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11
Q

Fog - Radiation fog usually dissipates…

A
  • 1-3 hours after sunrise
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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
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13
Q

Fog - Advection fog over the sea with wind

A
  • still forms with wind ≤ 30 kts due to less friction over the water
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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)
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15
Q

Fog - Tropical-Air fog is…

A
  • advection fog from the gradual cooling of air as it travels to higher latitudes
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16
Q

Fog - Tropical-Air fog commonality

A
  • more common over water with less friction
  • most common type of fog over open sea
  • most widespread fog observed in US
16
Q

Fog - Frontal fog is…

A
  • rain from warm air above falls to colder air below
  • evaporation of the warm rain raises dew point of colder air
17
Q

Fog - Frontal fog is found…

A
  • sometimes ahead of warm and occluded fronts, and behind cold fronts
18
Q

Fog - Inversion fog is typically found…

A
  • in subtropical west coasts of continents (ie. California)
19
Q

Fog - Inversion fog occurs when…

A
  • wind action over cold upwelling water gives air lower temperature and high relative humidity
  • offshore fog forms similar to advection process and works its way inland at night as the land cools
20
Q

Fog - Inversion fog - inversion created

A
  • higher temperature air above creates “lid” preventing the cool moist air from rising
21
Q

Fog Over the Sea - trade wind belts

A
  • Sea fog is rare except along coasts of California
22
Q

Fog Over the Sea - middle to high latitudes

A
  • common, esp. in spring and summer
23
Q

Fog Over the Sea - spring/summer general occurrence

A
  • warm/moist air from land to sea produces fog over coastal waters
  • wind shift tends to bring that fog back onto land
24
Q

Fog Over the Sea - fall/early winter general occurrence

A
  • air from sea to land produces fog in coastal areas
  • wind shift may drift to sea