Forecast Details for Lolo, MT

Recent Locations: Anahuac, TX   Oak Bluffs, MA   Lolo, MT  
Overnight: A 20 percent chance of rain. Areas of smoke. Mostly cloudy, with a low around 54. Light south southeast wind.
Sunday: A chance of rain, mainly between noon and 3pm, then a chance of showers and thunderstorms after 3pm. Patchy smoke. Partly sunny, with a high near 86. Calm wind becoming north northwest around 6 mph in the afternoon. Chance of precipitation is 30%.
Sunday Night: A chance of showers and thunderstorms before 9pm, then a chance of rain, mainly between 9pm and midnight. Patchy smoke between 10pm and midnight. Partly cloudy, with a low around 50. Southwest wind around 6 mph becoming calm after midnight. Chance of precipitation is 30%.
Monday: Mostly sunny, with a high near 83. Light and variable wind.
Monday Night: A 20 percent chance of rain after midnight. Partly cloudy, with a low around 49. Light and variable wind.
Tuesday: A chance of rain before noon, then a chance of showers and thunderstorms after noon. Mostly cloudy, with a high near 79. Chance of precipitation is 40%.
Tuesday Night: Rain likely, mainly before midnight. Mostly cloudy, with a low around 46. Chance of precipitation is 60%. New precipitation amounts between a tenth and quarter of an inch possible.
Wednesday: A chance of rain. Patchy fog before 9am. Otherwise, partly sunny, with a high near 76.
Wednesday Night: A chance of rain, mainly before midnight. Mostly cloudy, with a low around 46.
Thursday: A chance of rain before noon, then a chance of showers and thunderstorms after noon. Partly sunny, with a high near 74.
Thursday Night: A chance of rain. Mostly cloudy, with a low around 45.
Friday: A chance of rain. Mostly cloudy, with a high near 73.
Friday Night: A chance of rain. Mostly cloudy, with a low around 45.
Saturday: A chance of rain. Partly sunny, with a high near 74.

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