Forecast Details for Fremont, IN

Recent Locations: Los Osos, CA Axtell, TX Fremont, IN

Overnight: Showers likely, mainly before 3am. Cloudy, with a low around 51. Northwest wind 5 to 10 mph. Chance of precipitation is 70%.

Thursday: Partly sunny, with a high near 66. Northwest wind 5 to 10 mph.

Thursday Night: Mostly clear, with a low around 47. West wind 5 to 10 mph becoming south in the evening.

Friday: Mostly sunny, with a high near 69. South wind 15 to 20 mph becoming west in the afternoon. Winds could gust as high as 30 mph.

Friday Night: Mostly cloudy, with a low around 45. West wind 5 to 10 mph.

Saturday: Mostly sunny, with a high near 66.

Saturday Night: Partly cloudy, with a low around 43.

Sunday: Mostly sunny, with a high near 66.

Sunday Night: Mostly clear, with a low around 41.

Monday: Sunny, with a high near 69.

Monday Night: Mostly clear, with a low around 45.

Tuesday: Mostly sunny, with a high near 74.

Tuesday Night: Partly cloudy, with a low around 51.

Wednesday: Mostly sunny, with a high near 78.

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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

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North America Water Vapor (Moisture)

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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

Weather Topic: What are Altostratus Clouds?

Home - Education - Cloud Types - Altostratus Clouds

Next Topic: Cirrocumulus Clouds

Altostratus clouds form at mid to high-level altitudes (between 2 and 7 km) and are created by a warm, stable air mass which causes water vapor to condense as it rise through the atmosphere. Usually altostratus clouds are featureless sheets characterized by a uniform color.

In some cases, wind punching through the cloud formation may give it a waved appearance, called altostratus undulatus. Altostratus clouds are commonly seen with other cloud formations accompanying them.

Next Topic: Cirrocumulus Clouds