Weather Alert in Indiana
Severe Thunderstorm Watch issued March 26 at 5:16PM EDT until March 27 at 12:00AM EDT by NWS Northern Indiana
AREAS AFFECTED: Adams, IN; Allen, IN; Blackford, IN; Cass, IN; De Kalb, IN; Elkhart, IN; Fulton, IN; Grant, IN; Huntington, IN; Jay, IN; Kosciusko, IN; Lagrange, IN; La Porte, IN; Marshall, IN; Miami, IN; Noble, IN; Pulaski, IN; St. Joseph, IN; Starke, IN; Steuben, IN; Wabash, IN; Wells, IN; White, IN; Whitley, IN
DESCRIPTION: THE NATIONAL WEATHER SERVICE HAS ISSUED SEVERE THUNDERSTORM WATCH 76 IN EFFECT UNTIL MIDNIGHT EDT /11 PM CDT/ TONIGHT FOR THE FOLLOWING AREAS IN INDIANA THIS WATCH INCLUDES 24 COUNTIES IN NORTH CENTRAL INDIANA KOSCIUSKO ST. JOSEPH IN NORTHERN INDIANA ADAMS ALLEN IN BLACKFORD CASS IN DE KALB ELKHART FULTON IN GRANT HUNTINGTON JAY LA PORTE LAGRANGE MARSHALL MIAMI NOBLE PULASKI STARKE STEUBEN WABASH WELLS WHITE WHITLEY THIS INCLUDES THE CITIES OF AKRON, ALBION, ANGOLA, AUBURN, BASS LAKE, BERNE, BLUFFTON, BREMEN, BROOKSTON, COLUMBIA CITY, CULVER, DECATUR, DUNKIRK, ELKHART, FORT WAYNE, FRANCESVILLE, FREMONT, GARRETT, GAS CITY, GOSHEN, GRANGER, GRISSOM AFD, HARTFORD CITY, HUNTINGTON, KENDALLVILLE, KNOX, LA PORTE, LAGRANGE, LIGONIER, LOGANSPORT, MARION, MEDARYVILLE, MEXICO, MICHIGAN CITY, MISHAWAKA, MONON, MONTICELLO, MONTPELIER, NAPPANEE, NEW HAVEN, NORTH JUDSON, NORTH MANCHESTER, OSSIAN, PERU, PLYMOUTH, PORTLAND, ROANOKE, ROCHESTER, ROYAL CENTER, SHIPSHEWANA, SOUTH BEND, SOUTH WHITLEY, TOPEKA, TRI-LAKES, UPLAND, WABASH, WARSAW, WINAMAC, AND WINONA LAKE.
INSTRUCTION: N/A
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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
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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