Forecast Details for Slingerlands, NY

Recent Locations: Johnstown, PA   Monon, IN   Slingerlands, NY  
Current Alerts for Slingerlands, NY: Winter Weather Advisory
Overnight: A slight chance of snow showers before 3am. Mostly cloudy, with a low around 29. Calm wind. Chance of precipitation is 20%.
Saturday: A chance of snow showers before 4pm, then a chance of rain and snow showers between 4pm and 5pm, then a chance of snow showers after 5pm. Mostly cloudy, with a high near 40. Calm wind becoming west around 5 mph. Chance of precipitation is 40%. New snow accumulation of less than a half inch possible.
Saturday Night: A chance of rain and snow showers before midnight, then a chance of snow showers. Cloudy, with a low around 25. Calm wind. Chance of precipitation is 40%. New snow accumulation of less than a half inch possible.
Sunday: Snow likely, mainly between 7am and 1pm. Cloudy, with a high near 36. East wind 6 to 9 mph. Chance of precipitation is 60%. New snow accumulation of less than one inch possible.
Sunday Night: Snow likely, mainly after 1am. Cloudy, with a low around 25. North wind 6 to 15 mph, with gusts as high as 26 mph. Chance of precipitation is 60%.
Monday: Snow likely, mainly before 1pm. Cloudy, with a high near 32. Chance of precipitation is 60%.
Monday Night: Mostly cloudy, with a low around 17.
Tuesday: Partly sunny, with a high near 25.
Tuesday Night: Mostly cloudy, with a low around 10.
Wednesday: A chance of snow. Mostly cloudy, with a high near 35. Chance of precipitation is 50%.
Wednesday Night: Rain and snow likely. Mostly cloudy, with a low around 26. Chance of precipitation is 60%.
Thursday: A chance of rain. Mostly cloudy, with a high near 41. Chance of precipitation is 50%.
Thursday Night: A chance of rain and snow. Mostly cloudy, with a low around 25. Chance of precipitation is 40%.
Friday: Partly sunny, with a high near 38.

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