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Published byDorthy Bruce Modified over 9 years ago
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Advanced Shallow Weather and Orographic
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Boundaries Thunderstorm Outflows Lake Breezes
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Arc of blowing dust Reflectivity “thin lines” Gust Fronts Very shallow feature, emanate from a thunderstorm. Recall the depth-detection discussion.
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Example of Boundary in Reflectivity -10 to 20 dBZ
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Rapid Storm Evolution (Time lapse < 5 hours) Animation 120 km
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Movie Loop Showing Cold Front, Gravity Wave and Dry Line Interactions International H 2 0 Water Vapor Project (IHOP) May 11, 2002
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Gravity Waves International H 2 0 Water Vapor Project (IHOP) May 11, 2002
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Drizzle
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A Typical Z – R Beijing Summer
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Reflectivity and Drizzle Beijing Summer
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How to remember beamheight numbers? Aside
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S = r θ 1 o = 180/pi = 0.0175 radians At r=100 km then s = 100 * 0.0175 S = 1.75km = beamwidth at 100km For flat Earth, for beam at 1 o elevation angle, height of beam centre ~= 1.75km H = sqrt ( r^2 + 2*Ke*ae*r + sin ( theta_e ) ) – ke * ae r s θ
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Beam Height Diagram
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What is the approximate Height / Width the Beam 0.5 o beamwidth1.0 o beamwidth Elevation Angle0.5 o 1.0 o 0.5 o 1.0 o Range 50 km 100 km Arc distance = r theta 1 deg = 180 / pi = 0.01745329
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Forest Fires
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Kelowna Forest Fires
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Nocturnal bird migration looks like drizzle
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Insect migration and Cb
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Lake Breezes and Tornados Pat King and Dave Sills
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Morning Mid Afternoon “Pure” LB example Enhance convergence Lake Breeze Boundaries Lake Huron Lake Ontario Lake St Clair Lake Erie
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++++ = Pure lake breeze Moderate SW Flow Lake Breezes
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Average of 6 VIS Images from 1500-1800 UTC
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Spring (15 Mar - 15 Jun) Tornado Touchdown Points Confirmed and probable only
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Spring (15 Mar - 15 Jun) Tornado Touchdown Points … overlaid with boundaries from 31 July 1994... … tornadoes are suppressed in regions where Southwest winds are onshore... … and enhanced in regions where lake breeze boundaries often form. Forecasters use knowledge of lake breeze positions in their severe weather forecast for weak tornadoes
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Lee Side Troughing On a very small terrain feature
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Southern Ontario is relatively flat. Elevations rise from about 200m on Lake Huron to about 400m just south of Georgian Bay. Lake Huron Lake Ontario Lake Erie Georgian Bay Topography of Southern Ontario
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Average of six GOES images over a 3-hour period Moderate WSW flow Dissipation of thin SC cloud in downslope flow SC cloud forming beneath an inversion at 1500 m above ground Dissipation of Clouds in a SW Flow
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Topography of Southern Ontario Niagara Escarpment Average of six GOES images over a 3-hour period
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20 February, 2008 2008 NWA Conference - Louisville, KY Sam Lashley – National Weather Service Northern Indiana Jon Hitchcock – National Weather Service Buffalo, NY
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Mountain Top Radars Show Rodger Brown Paper graphs
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Negative Elevation Scans Show DEM and the one degree beam Show negative elevation angle Discuss caveats – need gc filtering Need 3dB filling Show
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Scanning in Complex Terrain Valley Radars Show the v10 radar DEM and discuss with respect the weather NOT surveillance
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Radar Detection Issues CAPPI (too high) 0 o PPI
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Lake Breezes and Convection Initiation/Suppression Review the wilson boundary rules/Aurora did a poster on this Show Pat King Lake Breeze and Prevailing Wind Analysis Show Pat King Tornado climatology and Lake Breezes Show AF358 or another case
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Lake Effect Snow Bands Show the EGPM lake effect snow bands Show single bands Show multiple bands Show the convergence in the middle of the band Talk about TREC tracking
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Sea Spray
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Orographic Effects Precipitation Enhancement – upslope condensation and development Precipitation Suppression –lee side troughing –Blocked flow –Radar Blockage – can not see Explanation – Impact of Froude Number
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