Weather Alert in Ohio
Severe Thunderstorm Warning issued March 26 at 7:24PM EDT until March 26 at 8:00PM EDT by NWS Northern Indiana
AREAS AFFECTED: Henry, OH; Putnam, OH
DESCRIPTION: SVRIWX The National Weather Service in Northern Indiana has issued a * Severe Thunderstorm Warning for... Northern Putnam County in west central Ohio... Southeastern Henry County in northwestern Ohio... * Until 800 PM EDT. * At 724 PM EDT, severe thunderstorms were located along a line extending from near Holgate to 10 miles southeast of Defiance to Continental, moving east at 65 mph. HAZARD...60 mph wind gusts and quarter size hail. SOURCE...Radar indicated. IMPACT...Hail damage to vehicles is expected. Expect wind damage to roofs, siding, and trees. * Locations impacted include... Ottawa, Leipsic, Deshler, Continental, Pandora, Holgate, Glandorf, Hamler, West Leipsic, Gilboa, Belmore, Miller City, New Bavaria, Prentiss, Kieferville, Gallup, Pleasant Bend, North Creek, and Wisterman.
INSTRUCTION: Remain alert for a possible tornado! Tornadoes can develop quickly from severe thunderstorms. If you spot a tornado go at once into the basement or small central room in a sturdy structure. For your protection move to an interior room on the lowest floor of a building. A Tornado Watch remains in effect until 1100 PM EDT for northwestern and west central Ohio.
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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