Forecast Details for Paxinos, PA

Recent Locations: Paxinos, PA  
Overnight: Mostly cloudy, with a low around 27. Blustery, with a northwest wind 18 to 20 mph, with gusts as high as 29 mph.
Saturday: Sunny, with a high near 47. Northwest wind around 16 mph, with gusts as high as 28 mph.
Saturday Night: Clear, with a low around 27. West wind 5 to 11 mph.
Sunday: Sunny, with a high near 55. Calm wind becoming west around 5 mph in the afternoon.
Sunday Night: A chance of showers after 2am. Mostly cloudy, with a low around 38. Southwest wind 3 to 5 mph. Chance of precipitation is 30%. New precipitation amounts of less than a tenth of an inch possible.
Monday: A chance of showers. Cloudy, with a high near 51. Chance of precipitation is 50%. New precipitation amounts of less than a tenth of an inch possible.
Monday Night: Mostly cloudy, with a low around 25.
Tuesday: Mostly sunny, with a high near 41.
Tuesday Night: Mostly clear, with a low around 23.
Wednesday: Sunny, with a high near 48.
Wednesday Night: Mostly clear, with a low around 30.
Thursday: Mostly sunny, with a high near 55.
Thursday Night: Partly cloudy, with a low around 36.
Friday: Mostly sunny, with a high near 59.

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Weather Topic: What are Hole Punch Clouds?

Home - Education - Cloud Types - Hole Punch Clouds

hole punch clouds Next Topic: Mammatus Clouds

A hole punch cloud is an unusual occurrence when a disk-shaped hole appears in a cirrostratus, cirrocumulus, or altocumulus cloud.

When part of the cloud forms ice crystals, water droplets in the surrounding area of the cloud evaporate. The effect of this process produces a large elliptical gap in the cloud. The hole punch cloud formation is rare, but it is not specific to any geographic area.

Other names which have been used to describe this phenomena include fallstreak hole, skypunch, and cloud hole.

Next Topic: Mammatus Clouds

Weather Topic: What are Shelf Clouds?

Home - Education - Cloud Types - Shelf Clouds

shelf clouds Next Topic: Wall Clouds

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: Wall Clouds