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Precipitation Types Global and Regional Mean Precipitation 1. Types of Precipitation: 2. Measurement: FIT, Feb 15, 2012 1
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Global Mean Precipitation 2 Satellite measurement of precipitation What happens in Hawaii?
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Hawaii Mean Precipitation 3 Precipitation measurement by Rain Gauge Mean = 70 in Without land = 25 in
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Honolulu Mean Precipitation 4
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Surface Analysis (Feb 11, 2012, 18 UTC) 5
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Hawaii (Feb 12, 2012, 0245 UTC) 6 Radar measurement of rain
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Precipitation Types 7
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Precipitation Types Drizzle: diameter < 0.5 mm Rain: diameter >= 0.5 mm Where are the raindrops larger, Miami or Seattle? Raindrops almost always < 6 mm because collision among raindrops too large raindrops tend to break up Start as rain, but may fall as drizzle. Does rain always reach the surface? 8
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Falling precipitation that evaporate before reaching surface - -- Virga Low humidity - - evaporation - - drops become smaller - - rate of fall decreases Strong updraft Sudden rain shower and cloudburst (Cumuliform) Rain and no-rain in places next to each other (Cumulonimbus) Continuous rain at small vertical currents (layered cloud or Nimbostratus) How does “Virga” look like and where does it happen? 9
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Fig. 7-14, p. 174 Virga (Rain not reaching the surface) 10
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Fig. 2, p. 175 Shape of Raindrops Spherical 2 mm (surface area / volume) is minimum for 2. 11
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Table 7-2, p. 175 12 Intensity of Rainfall
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Precipitation Types 13
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Fig. 7-15, p. 176 14 Falling ice-crystals and snowflakes (Fallstreaks) from cirrus clouds. Snow
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Fig. 7-16, p. 176 Fig. 7-17, p. 178 15 Common forms of ice crystal Dendrite Why is dendrite most common?
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Table 7-3, p. 176 16 Why is dendrite most common? Growth = f(temperature, sat. vap. Pr. difference) Maximum growth rate is at -12 to -16 C, when saturation vapor pressure difference between water and ice is maximum.
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Table 7-4, p. 178 17 Intensity of Snowfall Is visibility the best way to measure snowfall? Can wind lead to visibility problem?
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Fig. 4, p. 179 18 Some more terms related to snowfall Flurries : light and intermittent from developing cumulus cloud Snow squall : brief but more intense than flurries, usually from cumuliform clouds Drifting snow : surface movement Blowing snow : in air movement Ground blizzard : after falling snow has ended Blanket of snow: snow covering the landscape
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Fig. 4, p. 179 19 Snow as Sound Absorbant
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Fig. 7-18, p. 179 20 Annual Average Snowfall over US Why is Hawaii not included?
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Snow in Hawaii !! 21 Mauna Kea
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Precipitation Types 22
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Fig. 7-19, p. 180 23 Sleet and Freezing Rain Partially melted snowflake or cold raindrop - - freezes Deep freezing layer - - Sleet <= 5 mm Shallow freezing layer - - freezing rain >=0.5 mm
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Fig. 7-20, p. 180 24 Formation of Rime Supercooled droplets in contact with object at below freezing temperature - - white milky granular ice
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Fig. 7-21, p. 180 25 Destruction due to Freezing Rain Syracuse, New York, January 1998
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Fig. 5, p. 181 26 Aircraft de-icing
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Fig. 7-22, p. 181 27 Average number freezing rain/drizzle days
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Fig. 7-23, p. 182 28 Vertical Temperature Profile and Precipitation Type
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Precipitation Types 29
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Fig. 4, p. 179 30 Snow Grains and Snow Pellets Snow GrainsSnow Pellets Diameter< 1 mm< 5 mm Showernoyes Brittleness/bouncynoyes OriginStratus cloudCumulus congestus Opaqueyes
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Fig. 7-24, p. 182 31 Formation of Graupel / Snow Pellets Ice particle + cloud droplets -- rimed ice crystal -- graupel (dift shape than rime) -- snow pellet During summer: graupel - - large raindrop Vigorously convective cloud: graupel - - hailstones
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Fig. 7-27, p. 183 32 Formation of Hail/Hailstone
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Fig. 7-25, p. 182 Fig. 7-26, p. 183 33 Hail and Hailstone Dia = 17.8 cm (7 in) ; Circumference = 47.6 cm (18.7 in); weight > 1.75 lb
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Table 7-5, p. 185 34 Summary of Precipitation Types
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35 Measurement of Precipitation In-situ measurement : Rain gauge; accurate but spotty. Remote measurement : Radar, Satellite; not so accurate but large coverage. Combination of the above.
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Fig. 7-29, p. 184 36 Components of the standard rain gauge Area of collector = 10 x area of measuring tube
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Fig. 7-30, p. 185 37 Tipping bucket rain gauge
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38 Radar Transmitted energy backscatter
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Fig. 7-31a, p. 187 39 ReflectivityPrecipitation Oklahama, April 24, 1999
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Fig. 7-31a, p. 187 40 Reflectivity Precipitation Precipitation due to Fay (2008)
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THE END 41
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Fig. 7-23a, p. 182 42
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Fig. 7-23b, p. 182 43
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Fig. 7-23c, p. 182 44
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Fig. 7-23d, p. 182 45
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Fig. 7-28a, p. 184Fig. 7-28b, p. 184 46
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Fig. 7-32, p. 189 47
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Fig. 7-32, p. 189 48
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