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

Types of T-storms
 
storm spectrum
 
single cell storms
 
multicell clusters
 
multicell lines
 
supercells

Supercells
 
introduction
 
on radar
 
schematic diagrams
 
features
 
variations
 
hp supercells
 
lp supercells
 
multicell to supercell
 
tornadic supercell

LP Supercells
 
characteristics
 
with tornado

User Interface
 
graphics
text

.
LP Supercell With Tornado
plus rotating cloud bands and vaulted appearance

A westward view of the LP storm model's vertical cross-section shows the LP storm's undersized, rotating Cb and its small, nearly transparent precipitation area. Rotating cloud signatures are commonly visible in this supercell type, and wall clouds are frequently observed.

[Image: vertical cross-section of lp supercell (53K)]

An oddity is that this bare-bones storm type occasionally fosters small funnel clouds that extend from the mid-levels of the Cb rather than from the Cb base! At times weak or even strong tornadoes develop from the vicinity of the wall cloud.

This LP storm did produce tornadoes -- two of them. The storm actually bordered between an LP and a classic supercell as it has a fairly large and intense radar echo (VIP 5), including a pendant. In this westward view, we note that the wall cloud was on the north side of the rain-free base, with spectacular rotating bands arranged much like barber pole stripes around the parent Cb.

[Image: lp supercell with tornado (46K)]
Photograph by: Moller

This view gives us an excellent feel for the scale relationships between the rotating updraft and the tornado that occasionally develops beneath such an updraft. Remember, the radar hook echo is roughly equivalent in scale to the rotating Cb, whereas the tornado itself is much smaller.

[Image: vaulted lp supercell (69K)]
Photograph by: Moller

The same storm is pictured looking northwest, as the tornado was lifting/weakening into a funnel cloud (extreme lower left). The storm has a spectacularly vaulted appearance adjacent to the precipitation area, which was nearly transparent. Scattered raindrops were falling in this precipitation area, along with 5 inch diameter hail! Thus, the lack of an opaque precipitation curtain does not preclude the possibility of very damaging hail.

This storm produced about 5 million dollars in hail damage in Borger, Texas, with one rain gauge that survived the hail fall showing only 1/4 of an inch of liquid rain. The tornado that we have witnessed in these photographs produced several hundred thousand dollars damage to an oil refinery, and several injuries.



characteristics
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