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130-131 E/E
130 is a close-up of what could easily be interpreted as a true funnel cloud.
The smooth, tapered shape seems correct and the clouds above could be viewed
as a messy lowering. Not so. It is a very deceiving false funnel - scud moulded
to near-perfection in a twisting updraft. Take a look at 131 to see the context.
The storm's core is left of the view and the dark base is a combination flanking
line and gust front, since outflow is pushing it forward, forming scud. The
low cloud at lower left is a true, though disorganized, lowering. The false
funnel appears to its right, separate and unrelated to it.
132-135 Four inflow tails. In 132, outflow driving a sharp gust
front is lifting scud in chunks and in tails within stronger updrafts. 133 and
134 are lowerings with an inflow tail extending back towards the rain and outflow.
The cloud mass in 135 is the backside of a storm. A short flanking line ends
(SW side) as a tapered extension of the cloud base where the updrafts are focused
to a point. As seen in 18 and 119, such LP storms can produce brief true funnels
at the very back, too.
136 SW/E A collapsing heavy rain core (lower right) has
sent out a burst of outflow, forming a giant cloud "claw" that lunges forward
with teeth bared. Along the leading edge of this gust front, numerous small
updrafts condense as fingers of scud that can briefly look very much like funnel
clouds.
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Created :
2002-08-26
Modified :
2002-12-19
Reviewed :
2002-12-19
Url of this page : http://www.msc.ec.gc.ca /education/severe_weather/page42_e.cfm
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