Forecast Details for New York, NY

Your Recent Locations:  New York, NY  
Today: Rain. High near 39. Wind chill values between 25 and 30. North wind 15 to 17 mph. Chance of precipitation is 90%. New precipitation amounts between a tenth and quarter of an inch possible.
Tonight: A 50 percent chance of rain, mainly before midnight. Cloudy, then gradually becoming partly cloudy, with a low around 36. Wind chill values between 25 and 30. Northwest wind 14 to 17 mph.
Wednesday: Sunny, with a high near 49. Wind chill values between 30 and 40 early. Northwest wind around 10 mph.
Wednesday Night: A 30 percent chance of showers after midnight. Partly cloudy, with a low around 42. Southwest wind 5 to 7 mph.
Thursday: Partly sunny, with a steady temperature around 47. West wind 9 to 15 mph.
Thursday Night: Partly cloudy, with a low around 35.
Friday: Partly sunny, with a high near 42.
Friday Night: Partly cloudy, with a low around 31.
Saturday: Mostly sunny, with a high near 39.
Saturday Night: Partly cloudy, with a low around 29.
Sunday: Mostly sunny, with a high near 39.
Sunday Night: Partly cloudy, with a low around 28.
Monday: Mostly sunny, with a high near 37.

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Weather Topic: What are Mammatus Clouds?

Home - Education - Cloud Types - Mammatus Clouds

mammatus clouds Next Topic: Shelf Clouds

A mammatus cloud is a cloud with a unique feature which resembles a web of pouches hanging along the base of the cloud.

In the United States, mammatus clouds tend to form in the warmer months, commonly in the Midwest and eastern regions.

While they usually form at the bottom of a cumulonimbis cloud, they can also form under altostratus, altocumulus, stratocumulus, and cirrus clouds. Mammatus clouds warn that severe weather is close.

Next Topic: Shelf Clouds

Weather Topic: What are Wall Clouds?

Home - Education - Cloud Types - Wall Clouds

wall clouds Next Topic: Condensation

A wall cloud forms underneath the base of a cumulonimbus cloud, and can be a hotbed for deadly tornadoes.

Wall clouds are formed by air flowing into the cumulonimbus clouds, which can result in the wall cloud descending from the base of the cumulonimbus cloud, or rising fractus clouds which join to the base of the storm cloud as the wall cloud takes shape.

Wall clouds can be very large, and in the Northern Hemisphere they generally form at the southern edge of cumulonimbus clouds.

Next Topic: Condensation