Forecast Details for Langdon, ND

Recent Locations: Newark, DE   Shenorock, NY   Langdon, ND  
Overnight: A chance of flurries. Mostly cloudy, with a low around -7. Wind chill values as low as -26. North northwest wind 10 to 15 mph.
Sunday: A chance of flurries before noon, then a chance of snow after noon. Partly sunny, with a high near 0. Wind chill values as low as -26. North wind 9 to 15 mph. Chance of precipitation is 30%. Little or no snow accumulation expected.
Sunday Night: Mostly cloudy, with a low around -13. Wind chill values as low as -25. North wind 5 to 8 mph becoming light and variable.
Monday: Mostly cloudy, with a high near 17. Wind chill values as low as -25. Breezy, with a south southeast wind 9 to 14 mph increasing to 16 to 21 mph in the afternoon.
Monday Night: A 40 percent chance of snow, mainly after midnight. Mostly cloudy, with a low around 7. South wind 14 to 17 mph becoming west northwest after midnight.
Tuesday: A 20 percent chance of snow before noon. Mostly cloudy, with a high near 15. Blustery, with a northwest wind 16 to 21 mph.
Tuesday Night: Partly cloudy, with a low around -9. West northwest wind 7 to 14 mph.
Wednesday: Mostly sunny, with a high near 10. West wind 7 to 10 mph becoming south southeast in the afternoon.
Wednesday Night: Mostly cloudy, with a low around 2. South wind 11 to 16 mph becoming west southwest after midnight.
Thursday: Mostly sunny, with a high near 32. Breezy, with a west southwest wind 16 to 20 mph.
Thursday Night: Partly cloudy, with a low around 20. Breezy, with a west southwest wind 17 to 21 mph.
Friday: Mostly sunny, with a high near 30. Blustery, with a west wind 22 to 29 mph.
Friday Night: Mostly cloudy, with a low around -4. Blustery, with a northwest wind 21 to 25 mph.
Saturday: Partly sunny, with a high near 5. Blustery, with a northwest wind 17 to 22 mph.

Want more detail? Get the Complete 7 Day and Night Detailed Forecast!

Want to Receive our Free Daily Forecast Emails in your inbox by 5 a.m.?
There are no ads! Learn More
We respect your privacy and will not share or sell your email with anyone.

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).

Current U.S. National Radar

National Weather Forecast--Current

The Current National Weather Forecast and National Weather Map are shown below.

Today's National Weather Map

National Weather Forecast for Tomorrow

Tomorrow National Weather Forecast and Tomorrow National Weather Map are show below.

Tomorrows National Weather Map

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.

North American Water Vapor Map

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

Current conditions powered by WeatherAPI.com