Weather Alert in Ohio
Flood Watch issued April 3 at 11:40AM EDT until April 6 at 8:00AM EDT by NWS Cleveland OH
AREAS AFFECTED: Lucas; Wood; Ottawa; Sandusky; Erie; Lorain; Cuyahoga; Hancock; Seneca; Huron; Medina; Summit; Wyandot; Crawford; Richland; Ashland; Wayne; Stark; Marion; Morrow; Holmes; Knox
DESCRIPTION: * WHAT...Flooding of rivers and creeks remains possible across the region. Flash flooding caused by excessive rainfall continues to be possible mainly Friday night through Sunday morning. * WHERE...Portions of north central, northeast, and northwest Ohio, including the following counties, in north central Ohio, Ashland, Crawford, Erie, Huron, Knox, Lorain, Marion, Morrow and Richland. In northeast Ohio, Cuyahoga, Holmes, Medina, Stark, Summit and Wayne. In northwest Ohio, Hancock, Lucas, Ottawa, Sandusky, Seneca, Wood and Wyandot. * WHEN...Through Sunday morning. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. Flooding may occur in poor drainage and urban areas. Extensive street flooding is possible. * ADDITIONAL DETAILS... - Area rivers continue to rise from the 1 to 3 inches of rainfall Wednesday night. Additional systems will bring multiple rounds of moderate to heavy rainfall across the region Friday and Saturday nights with 2 to 4 inches of rainfall expected. This will bring the event rainfall total between 4 and 6 inches by Sunday. - Please visit www.weather.gov/safety/flood for flood safety and preparedness information
INSTRUCTION: You should monitor later forecasts and be prepared to take action should Flash Flood Warnings be issued.
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Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
Weather Topic: What is Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
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