Forecast Details for New York, NY

Recent Locations: New York, NY  
Overnight: A 20 percent chance of showers. Mostly cloudy, with a steady temperature around 68. Light northeast wind.
Wednesday: Mostly sunny, with a high near 81. Northeast wind around 8 mph.
Wednesday Night: Partly cloudy, with a low around 67. East wind around 6 mph becoming light and variable after midnight.
Thursday: Sunny, with a high near 84. North wind around 6 mph.
Thursday Night: Mostly clear, with a low around 70. South wind around 5 mph becoming light and variable in the evening.
Friday: Sunny, with a high near 86.
Friday Night: Mostly clear, with a low around 73.
Saturday: Sunny, with a high near 87.
Saturday Night: Mostly clear, with a low around 73.
Sunday: Sunny, with a high near 89.
Sunday Night: Mostly clear, with a low around 75.
Monday: Sunny, with a high near 91.
Monday Night: Partly cloudy, with a low around 76.
Tuesday: Mostly sunny, with a high near 91.

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Current U.S. National Radar--Current

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North America Water Vapor (Moisture)

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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