WW2010
University of Illinois

WW2010
 
welcome
 
online guides
 
archives
 
educational cd-rom
 
current weather
 
about ww2010
 
index

Online Guides
 
introduction
 
meteorology
 
remote sensing
 
reading maps
 
projects, activities

Meteorology
 
introduction
 
air masses, fronts
 
clouds, precipitation
 
el nino
 
forces, winds
 
hurricanes
 
hydrologic cycle
 
light, optics
 
midlatitude cyclones
 
severe storms
 
weather forecasting

Severe Storms
 
introduction
 
dangers of t-storms
 
types of t-storms
 
tstorm components
 
tornadoes
 
modeling

Tstorm Components
 
introduction
 
updrafts/downdrafts
 
wind shear
 
outflow phenomena
 
wall clouds

Updrafts/Downdrafts
 
introduction
 
lemon techique (lt)
 
multicell lt-analysis
 
supercell lt-analysis
 
supercell matures

User Interface
 
graphics
text

.
Supercell Analysis
using the lemon technique

A few storms take the intensification process further, to the supercell stage. The updraft becomes virtually erect and the storm top shifts off of the low-level echo gradient to the area above the developing pendent echo. Radar reflectivities continue to increase in both the low level and extensive mid-level overhang echoes. As mentioned earlier, evidence suggests that storm circulation associated with the mesocyclone holds the gust front in check. Therefore, rather than racing ahead of the updraft to eventually choke it off, the gust front remains quasi-stationary relative to the moving storm and aids in continued lifting of warm air into the updraft.

[Image: lemon technique analysis of supercell (55K)] A bounded WER (BWER) develops where the intense updraft is surrounded by mid-level overhang. When a hook or pendant echo is not visible on radar, a BWER often is, provided that the radar operator searches for it with the suggested vertical tilt sequence rather than with the range-height indicator (RHI) mode.

The supercell in this illustration does have a pendant echo, with the top of the rotating updraft above the WER and just east of the pendant. The radar operator must be aware that spotters are likely to see a well-developed wall cloud, often with vigorous rotation, beneath the radar BWER.

Why is the supercell updraft so intense? Obviously, instability is one factor. Another contributor is rotation. Research has shown that the lowest pressures in the rotating updraft initially are in the mid-levels (20,000 feet or so) in a supercell, causing an acceleration of the updraft, because of the upward oriented pressure gradient. This can result in a 50 percent increase in updraft speeds!

[Image: panhandle supercell (55K)]
Photograph by: NSSL

The Panhandle storm has become virtually erect, with an extremely crisp Cb top and anvil edge. We are still looking north, from about 30 miles, at the incipient supercell.



multicell lt-analysis
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.

supercell matures