Forecast Details for Bartlesville, OK

Recent Locations: Bartlesville, OK  
Overnight: Clear, with a low around 55. Calm wind.
Wednesday: Sunny, with a high near 83. Calm wind.
Wednesday Night: Clear, with a low around 57. Calm wind.
Thursday: Sunny, with a high near 87. Calm wind becoming south around 5 mph in the morning.
Thursday Night: Partly cloudy, with a low around 61. Southeast wind around 5 mph becoming calm in the evening.
Friday: Sunny, with a high near 87. Light south wind increasing to 5 to 10 mph in the morning.
Friday Night: Mostly clear, with a low around 66. South wind around 5 mph.
Saturday: Sunny, with a high near 90. Light south wind increasing to 5 to 10 mph in the morning.
Saturday Night: Mostly clear, with a low around 70. South wind around 5 mph.
Sunday: Sunny, with a high near 92. South wind 5 to 15 mph.
Sunday Night: Partly cloudy, with a low around 73. South wind 5 to 10 mph.
Monday: A 30 percent chance of showers and thunderstorms. Mostly sunny, with a high near 92. Southwest wind 5 to 10 mph.
Monday Night: A 30 percent chance of showers and thunderstorms. Partly cloudy, with a low around 72. South wind around 5 mph becoming calm in the evening.
Tuesday: Mostly sunny, with a high near 92. Calm wind becoming south around 5 mph in the morning.

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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