Weather Alert in Wisconsin
Tornado Watch issued July 16 at 12:17PM CDT until July 16 at 6:00PM CDT by NWS Green Bay WI
AREAS AFFECTED: Brown, WI; Calumet, WI; Kewaunee, WI; Manitowoc, WI; Outagamie, WI; Portage, WI; Waupaca, WI; Waushara, WI; Winnebago, WI; Wood, WI
DESCRIPTION: THE NATIONAL WEATHER SERVICE HAS ISSUED TORNADO WATCH 517 IN EFFECT UNTIL 6 PM CDT THIS EVENING FOR THE FOLLOWING AREAS IN WISCONSIN THIS WATCH INCLUDES 10 COUNTIES IN CENTRAL WISCONSIN PORTAGE WAUSHARA WOOD IN EAST CENTRAL WISCONSIN CALUMET MANITOWOC WINNEBAGO IN NORTHEAST WISCONSIN BROWN KEWAUNEE OUTAGAMIE WAUPACA THIS INCLUDES THE CITIES OF ALASKA, APPLETON, ARNOTT, AURORAVILLE, BAKERVILLE, BORTH, CLINTONVILLE, DARBOY, DUNDAS, DUVALL, GREEN BAY, KEWAUNEE, KING, LIND CENTER, MACKVILLE, MANITOWOC, MARSHFIELD, MENASHA, NEENAH, NEW LONDON, NORMAN, NORTHERN LAKE WINNEBAGO, NORTHPORT, OSHKOSH, PLOVER, POINT BEACH STATE PARK, RANKIN, RIO CREEK, ROSTOK, RURAL, SHOTO, SILVER LAKE, STEVENS POINT, TWO RIVERS, WAUPACA, WAUTOMA, WINNEBAGO, WISCONSIN RAPIDS, AND WITTMAN FIELD.
INSTRUCTION: N/A
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Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
Weather Topic: What is Graupel?
Home - Education - Precipitation - Graupel
Next Topic: Hail
Graupel is a form of precipitation that is created by atmospheric conditions
which cause supercooled water droplets to contact snow crystals and freeze to
their surface.
Sometimes known as soft hail or snow pellets, graupel is delicate and easily
destroyed by touch. Whereas hail usually falls during severe weather, graupel
doesn't require such conditions to form, and can form in mild precipitation
similar to situations which produce snowfall.
Next Topic: Hail
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