Weather Alert in Iowa

Recent Locations: Fort Dodge, IA  
Current Alerts for Fort Dodge, IA: Extreme Heat Warning

Flood Watch issued June 20 at 9:48PM CDT until June 23 at 11:31AM CDT by NWS Des Moines IA

AREAS AFFECTED: Black Hawk

DESCRIPTION: ...The National Weather Service in Des Moines IA has issued a Flood Watch for the following rivers in Iowa... Cedar River at Cedar Falls affecting Black Hawk county. * WHAT...Flooding is possible. * WHERE...The Cedar River at Cedar Falls, or from the West Fork Cedar River to the Cedar Falls-Waterloo city limits. * WHEN...From Saturday evening to late Monday morning. * IMPACTS...At 89.7 feet, Water affects the road at 1712 and 1118 Cottage Row Rd. * ADDITIONAL DETAILS... - At 8:45 PM CDT Friday the stage was 87.8 feet. - Forecast...Flood stage may be reached late tomorrow evening. - Flood stage is 89.0 feet.

INSTRUCTION: For the latest waterway observations and forecasts refer to weather.gov/desmoines/water. River forecasts include observed precipitation plus forecast precipitation over the next 24 hours.

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Weather Topic: What is Precipitation?

Home - Education - Precipitation - Precipitation

Precipitation Next Topic: Rain

Precipitation can refer to many different forms of water that may fall from clouds. Precipitation occurs after a cloud has become saturated to the point where its water particles are more dense than the air below the cloud.

In most cases, precipitation will reach the ground, but it is not uncommon for precipitation to evaporate before it reaches the earth's surface. When precipitation evaporates before it contacts the ground it is called Virga. Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog and mist are not considered precipitation because the water vapor which constitutes them isn't dense enough to fall to the ground.

Next Topic: Rain

Weather Topic: What are Shelf Clouds?

Home - Education - Cloud Types - Shelf Clouds

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

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