Weather Alert in Iowa

Recent Locations: San Ysidro, CA   Allegan, MI   Tama, IA  
Current Alerts for Tama, IA: Blizzard Warning High Wind Warning

High Wind Warning issued March 15 at 1:18PM CDT until March 16 at 1:00AM CDT by NWS Omaha/Valley NE

AREAS AFFECTED: Montgomery

DESCRIPTION: * WHAT...For the High Wind Warning, northwest winds 35 to 40 mph with gusts up to 60 mph. For the Cold Weather Advisory, very cold wind chills as low as 20 below expected. * WHERE...Montgomery County. * WHEN...For the High Wind Warning, until 1 AM CDT Monday. For the Cold Weather Advisory, from 1 AM to 10 AM CDT Monday. * IMPACTS...Damaging winds may blow down a few trees and power lines. Isolated power outages are expected. Travel will be difficult, especially for high profile vehicles. The dangerously cold wind chills as low as 20 below zero could cause frostbite on exposed skin in as little as 30 minutes.

INSTRUCTION: Delay travel if possible. If you must travel, use caution on the roads. Watch for falling debris and tree limbs. Use caution while traveling outside. Wear appropriate clothing, a hat, and gloves.

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Weather Topic: What are Altocumulus Clouds?

Home - Education - Cloud Types - Altocumulus Clouds

Altocumulus Clouds Next Topic: Altostratus Clouds

Similar to cirrocumulus clouds, altocumulus clouds are characterized by cloud patches. They are distinguished by larger cloudlets than cirrocumulus clouds but are still smaller than stratocumulus clouds.

Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km) and may resemble, at times, the shape of a flying saucer. These uncommon formations, called altocumulus lenticularis, are created by uplift in the atmosphere and are most often seen in close proximity to mountains.

Next Topic: Altostratus Clouds

Weather Topic: What are Cirrocumulus Clouds?

Home - Education - Cloud Types - Cirrocumulus Clouds

Cirrocumulus Clouds Next Topic: Cirrostratus Clouds

Cirrocumulus clouds form at high altitudes (usually around 5 km) and have distinguishing characteristics displayed in a fine layer of small cloud patches. These small cloud patches are sometimes referred to as "cloudlets" in relation to the whole cloud formation.

Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the water droplets in the cloud freeze into ice crystals and the cloud becomes a cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud formations generally pass rapidly.

Next Topic: Cirrostratus Clouds

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