Dial-an-Expert Tip Sheet: Severe Thunderstorms
BOULDER -- The 1997 storm season has gotten off to an early start, with deadly tornadoes striking Florida before the end of February and twisters raking Minnesota in March and the South in early April. Here are some tips to help you cover severe local storms this spring and summer.
As forecasters sharpen their skills in predicting severe weather, they've come up with a lengthening list of names for storms. Here's a roundup of some important storm types described in the latest forecast training tools from UCAR's Cooperative Program for Operational Meteorology, Education and Training (COMET).
Mesoscale convective system (MCS): The all-encompassing term for groups of thunderstorms that act as a system. An MCS can range across an entire state and might appear as a solid line, a broken line, or a cluster of cells. It can include any of the storm types below.
Multicell: A typical, garden-variety thunderstorm in which new updrafts form along the leading edge of rain-cooled air (the gust front). Individual cells usually last 30 to 60 minutes, while the system as a whole may last for many hours. Multicell storms may produce hail, strong winds, brief tornadoes, and/or flooding.
Supercell: An especially long-lived thunderstorm with a rotating updraft that continually regenerates on the storm's flank (often on the south or right-hand side). Supercells form in regions of strong vertical wind shear. They typically produce large hail and high winds and may also produce violent, long-lived tornadoes, such as those that recently struck in Alabama and Florida. Supercells often feature a hook-like appearance on radar precipitation displays as rain wraps around a tornadic circulation.
Squall line: A linear arrangement of storms, often accompanied by squalls of high wind and heavy rain (see graphic on next page). Squall lines tend to pass quickly and are less prone to produce tornadoes than are supercells. They can be hundreds of miles long but are typically only 10 or 20 miles wide.
Bow echo: The radar signature of a squall line that "bows out" as winds descend behind the line and circulations develop on either end (see graphic on previous page). A strongly bowed echo may indicate high winds in the middle of the line, where the storms are progressing most quickly. Brief tornadoes may occur on the leading edge of a bow echo. Often the north side of a bow echo becomes dominant over time, gradually evolving into a comma-shaped storm complex.
Derecho: A violent, widespread windstorm caused by a long-lived MCS with a series of bow echoes. Derecho (Deh-RAY-cho) is a Spanish word meaning "straight ahead." Derechoes produce winds of 60 to 100 miles per hour, downing trees and power lines over paths tens of miles wide and hundreds of miles long.
Mesoscale convective complex (MCC): A particular type of MCS, an MCC is a large, circular, long-lived cluster of showers and thunderstorms identified by satellite. It often emerges out of other storm types during the late-night and early-morning hours. MCCs can cover an entire state; they played a role in the 1993 Midwest flooding.
Pertinent sites on the World Wide Web
National Severe Storms Laboratory
Storm Prediction Center (SPC)
NCAR/RAP Real-Time Weather Data
Tornado Project Online
contact Milli Butterworth
telephone 303-497-8601 or by email firstname.lastname@example.org
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The University Corporation for Atmospheric Research (UCAR) is a not-for-profit university membership consortium which carries out programs to benefit the atmospheric, oceanic, and related sciences. Among other activites, UCAR operates the National Center for Atmospheric Research with National Science Foundation sponsorship.
Prepared for the web by Jacque Marshall
Last revised: Fri Apr 7 15:38:50 MDT 2000
Last revised: Mon Apr 20 12:56:25 MDT 1998