Weather Alert in Minnesota

Recent Locations: Lee Center, NY   El Centro, CA   Good Thunder, MN  
Current Alerts for Good Thunder, MN: Winter Weather Advisory

Winter Weather Advisory issued March 31 at 2:50PM CDT until April 2 at 7:00PM CDT by NWS Twin Cities/Chanhassen MN

AREAS AFFECTED: Douglas; Todd; Morrison; Mille Lacs; Kanabec; Stevens; Pope; Stearns; Benton; Lac Qui Parle; Swift; Chippewa; Kandiyohi; Meeker; Yellow Medicine

DESCRIPTION: ...MESSY SPRING SYSTEM TO BRING RAIN, FREEZING RAIN, SLEET, AND SNOW TO PORTIONS OF MINNESOTA AND WISCONSIN WEDNESDAY THROUGH THURSDAY... .A strong system is expected to bring a variety of precipitation types to the region Wednesday through Thursday. While there is still some uncertainty in the exact track of the low, a mix of snow and sleet is expected for much of central and western Minnesota. Further to the south and east, sleet and freezing rain will be the primary precipitation type. Some shifts in the track are still anticipated, which will influence the total accumulations of snow, sleet, freezing rain, and rain. * WHAT...Mixed precipitation expected. Total snow accumulations between 3 and 5 inches, sleet accumulations around three quarters of an inch, and ice accumulations around one tenth of an inch. * WHERE...Benton, Kandiyohi, Meeker, Morrison, Stearns, Todd, Kanabec, Mille Lacs, Chippewa, Douglas, Lac Qui Parle, Pope, Stevens, Swift, and Yellow Medicine Counties. * WHEN...From 1 PM Wednesday to 7 PM CDT Thursday. * IMPACTS...Plan on slippery road conditions. The hazardous conditions will impact the Wednesday evening and Thursday morning commutes.

INSTRUCTION: Slow down and use caution while traveling. Call 5 1 1 or visit 511mn.org for road conditions.

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Weather Topic: What is Condensation?

Home - Education - Precipitation - Condensation

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

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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