WW2010
University of Illinois

WW2010
 
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Meteorology
 
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air masses, fronts
 
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Severe Storms
 
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Types of T-storms
 
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multicell lines
 
supercells

Multicell Lines
 
introduction
 
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on satellite images
 
along leading edge
 
retreating lines
 
linear radar echoes
 
bow echoes
 
more bow echoes

User Interface
 
graphics
text

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More About Bow Echoes
schematic radar view and observed events

Squall lines and multicell storms occasionally develop the appearance of a "bow echo" on radar. When the bow shape opens toward the strong mid-level winds (10 to 20 thousand foot level winds of 40 knots or greater), there is an excellent chance that the strong mid-level currents have been transported to the ground in a downburst, forcing a portion of the squall line or multicell storm to accelerate forward. Macroburst and microburst winds are common with these storms, and 100+ MPH winds have been reported in extreme cases.

[Image: schematic of radar view of a bow echo squall line (55K)]

Weak to occasionally strong tornadoes may occur with the comma head, while gustnadoes may form on the strong bow echo gust front.

[Image: gustnado (55K)]
Photograph by: Doswell

This is a northward view of a gustnado, a tornado that develops on a thunderstorm gust front with marked across-front horizontal shear. Gustnadoes typically are weak and short-lived as tornadoes go, since they are not associated with an intense deeply rotating updraft. They are also nearly impossible to warn for, because of their seemingly random occurrence along the gust front.

The bow echo weakens as the accelerating downburst outruns the storm complex. Those who operate radar should be aware that the rotating comma head occasionally has deceptively weak radar reflectivity while producing damaging winds and tornadoes.

[Image: visual observation of a small scale bow echo (65K)]
Photograph by: Moller

Smaller scale bow echoes frequently can be detected from visual observations. This southward view shows the underside of a right to left (eastward) moving storm's shelf cloud, with the southern extent of the complex bowing radically eastward in the background. Damaging winds and a radar bow echo occurred within this area.

We need to stress that it is not the job of spotters to detect and report bow echoes, but spotters should know what they are dealing with and what the main severe weather threats are if Weather Service personnel ask them to check out a bow echo complex.



bow echoes
Terms for using data resources. CD-ROM available.
Credits and Acknowledgments for WW2010.
Department of Atmospheric Sciences (DAS) at
the University of Illinois at Urbana-Champaign.

Supercells