Weather Alert in Minnesota

Recent Locations: Luverne, MN  

Blizzard Warning issued March 14 at 6:12AM CDT until March 16 at 4:00AM CDT by NWS Twin Cities/Chanhassen MN

AREAS AFFECTED: Stevens; Pope; Lac Qui Parle; Swift; Chippewa; Kandiyohi; Meeker; Yellow Medicine; Renville; McLeod

DESCRIPTION: ...POWERFUL WINTER STORM ON TRACK TO BRING EXTREME SNOW ACCUMULATIONS AND STRONG WINDS... ...A WINTRY MIX OF RAIN, FREEZING RAIN, AND SLEET LATE TONIGHT ACROSS SOUTHERN MINNESOTA... ...TRAVEL MAY BECOME IMPOSSIBLE LATE TONIGHT AND SUNDAY... .A major winter storm will move across the Upper Midwest starting late this afternoon and lasting through Sunday evening. The first concern is heavy snow with a broad area of 12 to 18 inches expected across central Minnesota and western Wisconsin. A narrow swath within the broader area may approach 2 feet in parts of far east central Minnesota and west central Wisconsin. Rates of 2 to 2.5 inches per hour are likely late tonight. A wintry mix of rain, freezing rain, and sleet is now expected to work north into southern Minnesota tonight. A half inch of sleet and a tenth of an inch of ice are expected from New Ulm to Red Wing and south. The wintry mix will turn to all snow Sunday morning. The second concern is increasing winds on Sunday. Even though the snow will be tapering off gradually throughout Sunday, northwest winds will increase to 30 to 40 mph. Some gusts of 50 to 55 mph are possible. The combination of falling snow, blowing snow, and gusty winds will reduce visibility and create blizzard conditions late Sunday morning through Sunday evening across western and southern Minnesota. Travel is expected to become very difficult or impossible late tonight through Sunday evening. In addition, the amount of water in the snowpack will make it very heavy, leading to the potential for infrastructure damage and a health hazard for those shoveling. * WHAT...For the Winter Storm Warning, heavy snow expected. Total snow accumulations between 10 and 15 inches. Winds gusting as high as 35 mph. For the Blizzard Warning, blizzard conditions expected. Additional snow accumulations up to two inches. Winds gusting as high as 45 mph. * WHERE...Kandiyohi, McLeod, Meeker, Renville, Chippewa, Lac Qui Parle, Pope, Stevens, Swift, and Yellow Medicine Counties. * WHEN...For the Winter Storm Warning, from 4 PM this afternoon to 10 AM CDT Sunday. For the Blizzard Warning, from 10 AM Sunday to 4 AM CDT Monday. * IMPACTS...Travel could be very difficult to impossible. Widespread blowing snow could significantly reduce visibility. Gusty winds could bring down tree branches. Whiteout conditions are expected and will make travel treacherous and potentially life-threatening.

INSTRUCTION: Travel should be restricted to emergencies only. If you must travel, have a winter survival kit with you. If you get stranded, stay with your vehicle. Call 5 1 1 or visit 511mn.org for road conditions. Prepare now for potential road closures. Delay travel and shelter in place once conditions worsen. Remember, if interstate highways are closed, state highways and county roads are also impassable.

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Weather Topic: What are Stratocumulus Clouds?

Home - Education - Cloud Types - Stratocumulus Clouds

Stratocumulus Clouds Next Topic: Stratus Clouds

Stratocumulus clouds are similar to altocumulus clouds in their fluffy appearance, but have a slightly darker shade due to their additional mass.

A good way to distinguish the two cloud types is to hold your hand out and measure the size of an individual cloud; if it is the size of your thumb it is generally an altocumulus cloud, if it is the size of your hand it is generally a stratocumulus cloud.

It is uncommon for stratocumulus clouds to produce precipitation, but if they do it is usually a light rain or snow.

Next Topic: Stratus Clouds

Weather Topic: What are Wall Clouds?

Home - Education - Cloud Types - Wall Clouds

Wall Clouds Next Topic: Altocumulus Clouds

A wall cloud forms underneath the base of a cumulonimbus cloud, and can be a hotbed for deadly tornadoes.

Wall clouds are formed by air flowing into the cumulonimbus clouds, which can result in the wall cloud descending from the base of the cumulonimbus cloud, or rising fractus clouds which join to the base of the storm cloud as the wall cloud takes shape.

Wall clouds can be very large, and in the Northern Hemisphere they generally form at the southern edge of cumulonimbus clouds.

Next Topic: Altocumulus Clouds

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