Weather Alert in Illinois
Severe Thunderstorm Watch issued March 26 at 9:13PM CDT until March 26 at 11:00PM CDT by NWS Lincoln IL
AREAS AFFECTED: Cass, IL; Champaign, IL; Christian, IL; Clark, IL; Coles, IL; Cumberland, IL; De Witt, IL; Douglas, IL; Edgar, IL; Fulton, IL; Knox, IL; Logan, IL; McLean, IL; Macon, IL; Mason, IL; Menard, IL; Morgan, IL; Moultrie, IL; Peoria, IL; Piatt, IL; Sangamon, IL; Schuyler, IL; Scott, IL; Shelby, IL; Tazewell, IL; Vermilion, IL
DESCRIPTION: SEVERE THUNDERSTORM WATCH 76 REMAINS VALID UNTIL 11 PM CDT THIS EVENING FOR THE FOLLOWING AREAS IN ILLINOIS THIS WATCH INCLUDES 26 COUNTIES IN CENTRAL ILLINOIS CHRISTIAN DE WITT LOGAN MACON MASON MCLEAN MENARD PEORIA SANGAMON SHELBY TAZEWELL IN EAST CENTRAL ILLINOIS CHAMPAIGN CLARK COLES CUMBERLAND DOUGLAS EDGAR MOULTRIE PIATT VERMILION IN WEST CENTRAL ILLINOIS CASS FULTON KNOX MORGAN SCHUYLER SCOTT THIS INCLUDES THE CITIES OF BEARDSTOWN, BLOOMINGTON, CANTON, CHAMPAIGN, CHARLESTON, CLINTON, DANVILLE, DECATUR, GALESBURG, GREENUP, HAVANA, JACKSONVILLE, LINCOLN, MARSHALL, MATTOON, MONTICELLO, NORMAL, PARIS, PEKIN, PEORIA, PETERSBURG, RUSHVILLE, SHELBYVILLE, SPRINGFIELD, SULLIVAN, TAYLORVILLE, TUSCOLA, URBANA, AND WINCHESTER.
INSTRUCTION: N/A
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
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