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 is Condensation?
Home - Education - Precipitation - Condensation
Next Topic: Contrails
Condensation is the process which creates clouds, and therefore
it is a crucial process in the water cycle.
Condensation is the change of matter from a state of gas into a state of liquid,
and it happens because water molecules release heat into the atmosphere and
become organized into a more closely packed structure, what we might see as
water droplets.
Water is always present in the air around us as a vapor, but it's too small for
us to see. When water undergoes the process of condensation it becomes organized
into visible water droplets. You've probably seen condensation happen before on the
surface of a cold drink!
Next Topic: Contrails
Weather Topic: What are Cumulonimbus Clouds?
Home - Education - Cloud Types - Cumulonimbus Clouds
Next Topic: Cumulus Clouds
The final form taken by a growing cumulus cloud is the
cumulonimbus cloud, which is very tall and dense.
The tower of a cumulonimbus cloud can soar 23 km into the atmosphere, although
most commonly they stop growing at an altitude of 6 km.
Even small cumulonimbus clouds appear very large in comparison to other cloud types.
They can signal the approach of stormy weather, such as thunderstorms or blizzards.
Next Topic: Cumulus Clouds
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