Forecast Details for Bremerton, WA

Recent Locations: Bremerton, WA

Today: Sunny, with a high near 69. North wind 8 to 10 mph.

Tonight: Mostly clear, with a low around 49. North wind 5 to 10 mph becoming light after midnight.

Tuesday: Sunny, with a high near 73. North wind 3 to 7 mph.

Tuesday Night: Increasing clouds, with a low around 51. North wind 3 to 8 mph.

Wednesday: Mostly cloudy, with a high near 71. South wind 3 to 7 mph.

Wednesday Night: Partly cloudy, with a low around 52.

Thursday: Sunny, with a high near 74.

Thursday Night: Mostly cloudy, with a low around 54.

Friday: Mostly sunny, with a high near 74.

Friday Night: Partly cloudy, with a low around 54.

Saturday: Mostly sunny, with a high near 75.

Saturday Night: Mostly clear, with a low around 55.

Sunday: Sunny, with a high near 79.

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Current U.S. National Radar--Current

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National Weather Forecast--Current

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National Weather Forecast for Tomorrow

Tomorrow National Weather Forecast and Tomorrow National Weather Map are show below.

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.

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