Weather Alert in Alaska
Flood Watch issued August 25 at 8:05AM AKDT until August 26 at 4:00PM AKDT by NWS Fairbanks AK
AREAS AFFECTED: Southern Seward Peninsula Coast; Interior Seward Peninsula; Eastern Norton Sound and Nulato Hills
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall is possible. * WHERE...Including the following areas, Eastern Norton Sound and Nulato Hills, Interior Seward Peninsula and Southern Seward Peninsula Coast. This includes the cities of Nome, White Mountain, Golovin, Serpentine Hot Springs, Council, Haycock, Pilgrim Springs, Taylor, Unalakleet, Stebbins, St Michael, Elim, Koyuk, And Shaktoolik. * WHEN...From 4 PM AKDT this afternoon through Tuesday afternoon. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. * ADDITIONAL DETAILS... - Heavy rainfall is expected across the interior and southern Seward Peninsula as well as the eastern Norton Sound Monday afternoon through Tuesday. Rainfall amounts of 2 to 3 inches are forecast across the region, resulting in rapid rises along rivers, creeks, and streams. Smaller streams may see water rises to near or above flood stage overnight Monday night through Tuesday morning. - Http://www.weather.gov/aprfc
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. Stay tuned to further developments by listening to your local radio, television, or NOAA Weather Radio for further information.
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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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