Weather Alert in Ohio
Flood Watch issued March 4 at 10:23AM EST until March 5 at 1:00PM EST by NWS Charleston WV
AREAS AFFECTED: Perry; Morgan; Athens; Washington; Jackson; Vinton; Meigs; Gallia; Mason; Jackson; Wood; Pleasants; Tyler; Wirt; Ritchie; Doddridge
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall continues to be possible. * WHERE...Portions of southeast Ohio, including the following counties, Athens, Gallia, Jackson OH, Meigs, Morgan, Perry, Vinton and Washington and West Virginia, including the following counties, Doddridge, Jackson WV, Mason, Pleasants, Ritchie, Tyler, Wirt and Wood. * WHEN...Through Thursday afternoon. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. Creeks and streams may rise out of their banks. * ADDITIONAL DETAILS... - Moderate to heavy rainfall from last night has left soils vulnerable to significant runoff with any additional rainfall. - http://www.weather.gov/safety/flood
INSTRUCTION: You should monitor later forecasts and be alert for possible Flood Warnings. Those living in areas prone to flooding should be prepared to take action should flooding develop. Additional information can be found at https://www.weather.gov/rlx as well as on our X and Facebook pages.
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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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