Squall - Wikipedia, the free encyclopedia
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A squall is a sudden, sharp increase in wind speed which is usually associated with active weather, such as rain showers, thunderstorms, or heavy snow. Squalls refer to an increase in the sustained ...
en.wikipedia.org/wiki/Squall
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A "squall line" refers to a linearly-oriented zone of convection (i.e., thunderstorms). ... Detailed squall line and bow echo information is given below, including pre-storm environments, and WSR-88D radar reflectivity, velocity, and mesocyclone characteristics.; ... UPPER-LEVEL FEATURES;
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www.crh.noaa.gov/lmk/soo/docu/bowecho.php
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This squall line was more than 100 km wide, oriented north-south and traveled eastward at approximately 14 m s-1. It produced rainfall of 2-h duration at surface stations. ... Squall line ; Momentum ; Atmospheric convection ; Vertical component ; Atmospheric humidity ; Flow field ; Velocity distribution ; Mid latitude ;
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cat.inist.fr/?aModele=afficheN&cpsidt=4318671
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The simulated features include mesoscale cold pools behind a narrow gust front, multi-cellular and three-dimensional structures of the squall line, low and high pressure patterns across the gust front, major branches of front-to-rear and rear-to-front circulations, convective-scale updrafts and downdrafts,
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www.caps.ou.edu/ARPS/papers/98NWP3.html
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Areas that have been warmed are marked in red, while the blue areas point to locations that have experienced cooling. The cloud outline is superimposed, marked by the thick black line. ... Features 3, 4 and 5, farthest to the rear, are the remnants of earlier cells. The latter two are convectively inactive.
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www.atmos.ucla.edu/~fovell/ASres/ftan/ftan.html
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The schematic above is a depiction of the structure of a well-formed squall line. Such schematics are often a key result of a scientific investigation and can be based on observations, model and/or theory. They help communicate some of the key features in a simple and concise way.
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ww2010.atmos.uiuc.edu/(Gl)/guides/mtr/svr/modl/line/squ...
ww2010.atmos.uiuc.edu/(Gl)/guides/mtr/svr/modl/line/squall.rxml
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A non-severe squall line that developed on 21 June 1993 along the northern foothills of the Colorado Rocky Mountains is analyzed using a series of triple-Doppler analyses and compared to the conceptual model for a typical squall line with trailing stratiform rain area. ... Accession Number : ADA300051 ... Based on the simulations,
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stinet.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=...
stinet.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA300051
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November 6th, 2005 - Severe Thunderstorms with a Cold Front ... November 6th - Late Season Severe Thunderstorms/Squall Line ... Squall line of thunderstorms moving through north-central PA...
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www.erh.noaa.gov/ctp/features/2005/6Nov/
www.erh.noaa.gov/ctp/features/2005/6Nov/
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A line of strong thunderstorms developed in parts of the Midwest during the day on Friday, and moved rapidly east through Pennsylvania. These thunderstorms produced high winds across much of the state with storm damage reported from Warren to Lancaster Counties. ... Severe Squall Line Event June 8th, 2007...
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www.erh.noaa.gov/ctp/features/2007/06_08/
www.erh.noaa.gov/ctp/features/2007/06_08/
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