Forecast Details for Chino Hills, CA

Recent Locations: Paupack, PA Denver, CO Chino Hills, CA

Overnight: Patchy fog. Otherwise, cloudy, with a low around 55. Southwest wind around 5 mph.

Saturday: Patchy fog before 11am. Otherwise, cloudy through mid morning, then gradual clearing, with a high near 71. Light southwest wind increasing to 10 to 15 mph in the afternoon. Winds could gust as high as 20 mph.

Saturday Night: Patchy fog after 11pm. Otherwise, increasing clouds, with a low around 52. Southwest wind 5 to 15 mph, with gusts as high as 20 mph.

Sunday: Patchy fog before 11am. Otherwise, mostly cloudy through mid morning, then gradual clearing, with a high near 69. Light southwest wind increasing to 10 to 15 mph in the afternoon. Winds could gust as high as 20 mph.

Sunday Night: Patchy fog after 11pm. Otherwise, increasing clouds, with a low around 52. Southwest wind 5 to 15 mph, with gusts as high as 20 mph.

Monday: Patchy fog before 11am. Otherwise, cloudy, then gradually becoming mostly sunny, with a high near 66.

Monday Night: Patchy fog after 11pm. Otherwise, mostly cloudy, with a low around 51.

Tuesday: Patchy fog before 11am. Otherwise, mostly cloudy, then gradually becoming sunny, with a high near 72.

Tuesday Night: Patchy fog after 11pm. Otherwise, increasing clouds, with a low around 53.

Wednesday: Patchy fog before 11am. Otherwise, mostly cloudy, then gradually becoming sunny, with a high near 72.

Wednesday Night: Patchy fog. Otherwise, partly cloudy, with a low around 53.

Thursday: Patchy fog. Otherwise, mostly sunny, with a high near 69.

Thursday Night: Patchy fog. Otherwise, increasing clouds, with a low around 53.

Friday: Patchy fog. Otherwise, mostly cloudy, then gradually becoming sunny, with a high near 69.

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National Weather Forecast for Tomorrow

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North America Water Vapor (Moisture)

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Weather Topic: What are Stratocumulus Clouds?

Home - Education - Cloud Types - Stratocumulus Clouds

Next Topic: Stratus Clouds

Stratocumulus clouds are similar to altocumulus clouds in their fluffy appearance, but have a slightly darker shade due to their additional mass.

A good way to distinguish the two cloud types is to hold your hand out and measure the size of an individual cloud; if it is the size of your thumb it is generally an altocumulus cloud, if it is the size of your hand it is generally a stratocumulus cloud.

It is uncommon for stratocumulus clouds to produce precipitation, but if they do it is usually a light rain or snow.

Next Topic: Stratus Clouds

Weather Topic: What are Wall Clouds?

Home - Education - Cloud Types - Wall Clouds

Wall Clouds Next Topic: Altocumulus Clouds

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: Altocumulus Clouds