3. Mist and Fog Forecasting Techniques Mist Is Defined As

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3. Mist and Fog Forecasting Techniques Mist is defined as ... … a suspension in the air of microscopic water droplets or wet hygroscopic particles, reducing visibility at the earth’s surface. used when visibility is ≥1000m and ≤5000m and RH >95% Tdry-Tdew ≤ 0.5 C. © Crown copyright 2004 Page 2 Fog is defined as ... … a suspension of microscopic water droplets in the air reducing visibility at the earth’s surface to: < 1000m for met. observations, aviation and shipping < 200m (dense fog) for public service purposes Tdry ≈ Tdew. © Crown copyright 2004 Page 3 Freezing fog and ice fog Freezing fog − Supercooled drops which freeze on impact with a surface (produce rime) Ice fog − Tiny suspended ice particles − Requires T≤ -30°C © Crown copyright 2004 Page 4 Fog types There are three main types: Radiation fog Warm Advection fog Upslope fog © Crown copyright 2004 Page 5 RADIATION FOG © Crown copyright 2004 Page 6 Radiation fog formation Overnight clear skies Moist air in lowest 100m Moist ground Light surface wind = fog >5KT surface wind = low cloud (turbulent stratus) Valleys or ‘bowls’ Fog point © Crown copyright 2004 Page 7 Fog point Definition: The screen temperature at which fog may be expected to form The fog point may be much lower than the air mass dew point Why? © Crown copyright 2004 Page 8 Dew formation Fall in surface temperature on radiation night Air cools to dew point Dew deposition − Latent heat given out during condensation slows temperature fall − Air near the ground becomes drier Dew point falls So fog point < Air mass dew point © Crown copyright 2004 Page 9 The effect of the hydrolapse Large positive hydrolapse Much drier air aloft 2 3 5 7 s e n i Moisture losses at ground L not replaced by diffusion R M H Large amount of cooling for fog Fog point << airmass dewpoint © Crown copyright 2004 Page 10 The effect of the hydrolapse Small positive hydrolapse Slightly drier air aloft 2 3 5 7 s e n i Drying at surface soon L produces negative R hydrolapse M H Less cooling for fog Fog point slightly < airmass dewpoint © Crown copyright 2004 Page 11 The effect of the hydrolapse Negative hydrolapse More moist air aloft 2 3 5 7 s e n i Moisture losses at ground L readily replaced from R above M H No further cooling for fog Fog point = airmass dewpoint Saunders © Crown copyright 2004 Page 12.

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