Weather Alert in Iowa
Flood Watch issued June 25 at 9:18PM CDT until July 2 at 10:30PM CDT by NWS Quad Cities IA IL
AREAS AFFECTED: Linn
DESCRIPTION: ...The Flood Watch continues for the following rivers in Iowa... Cedar River at Vinton affecting Benton County. Cedar River AT Palo Blairs Ferry Rd affecting Linn County. ...The Flood Watch is extended for the following rivers in Iowa... Cedar River at Cedar Rapids affecting Linn County. Cedar River near Conesville affecting Muscatine and Louisa Counties. Cedar River at Cedar Bluff affecting Muscatine, Cedar and Johnson Counties. * WHAT...Flooding is possible due to rounds of thunderstorms and locally heavy rainfall. * WHERE...Cedar River at Palo Blairs Ferry Rd. * WHEN...From Monday morning to Wednesday, July 02. * IMPACTS...At 13.5 feet, Chain Bridge Road accessing the boat ramp is closed. * ADDITIONAL DETAILS... - At 8:15 PM CDT Wednesday the stage was 10.4 feet. - Forecast...Flood stage may be reached Monday morning. - Flood stage is 12.5 feet.
INSTRUCTION: If you are in the watch area, remain alert to possible flooding. Stay tuned to further developments by listening to your local radio, television, or NOAA Weather Radio for further information. The next statement will be issued by Thursday evening at 930 PM CDT.
Want more detail? Get the Complete 7 Day and Night Detailed Forecast!
Current U.S. National Radar--Current
The Current National Weather Radar is shown below with a UTC Time (subtract 5 hours from UTC to get Eastern Time).
National Weather Forecast--Current
The Current National Weather Forecast and National Weather Map are shown below.
National Weather Forecast for Tomorrow
Tomorrow National Weather Forecast and Tomorrow National Weather Map are show below.
North America Water Vapor (Moisture)
This map shows recent moisture content over North America. Bright and colored areas show high moisture (ie, clouds); brown indicates very little moisture present; black indicates no moisture.
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
Current conditions powered by WeatherAPI.com
