Yesterday's Weather for Atlanta, GA

Your Recent Locations:  Atlanta, GA  

How much rain or snow did Atlanta, GA get yesterday? The answer is below!

Yesterday's High was 63 °F

Yesterday's Low was 25 °F

Yesterday's Precipitation was 0.00 inches

Observations on January 20, 2018:
Time Temp Wind Conditions
12:53 AM EST 28.0 °F 0.0 mph Clear
1:53 AM EST 28.0 °F 0.0 mph Clear
2:53 AM EST 27.0 °F 0.0 mph Clear
3:53 AM EST 27.0 °F 0.0 mph Clear
4:53 AM EST 26.1 °F 0.0 mph Clear
5:53 AM EST 27.0 °F 0.0 mph Clear
6:53 AM EST 26.1 °F 0.0 mph Mostly Cloudy
7:53 AM EST 28.9 °F 0.0 mph Overcast
8:53 AM EST 32.0 °F 0.0 mph Overcast
9:53 AM EST 37.9 °F 0.0 mph Scattered Clouds
10:53 AM EST 46.9 °F 3.5 mph Mostly Cloudy
11:53 AM EST 52.0 °F 3.5 mph Overcast
12:53 PM EST 57.9 °F 4.6 mph Partly Cloudy
1:53 PM EST 60.1 °F 9.2 mph Clear
2:53 PM EST 62.1 °F 9.2 mph Clear
3:53 PM EST 63.0 °F 5.8 mph Clear
4:53 PM EST 62.1 °F 5.8 mph Clear
5:53 PM EST 57.9 °F 0.0 mph Clear
6:53 PM EST 51.1 °F 0.0 mph Clear
7:53 PM EST 46.9 °F 0.0 mph Clear
8:53 PM EST 44.1 °F 0.0 mph Clear
9:53 PM EST 42.1 °F 0.0 mph Clear
10:53 PM EST 39.0 °F 0.0 mph Clear
11:53 PM EST 37.0 °F 0.0 mph Clear
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Current U.S. National Radar--Current

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Current U.S. National Radar

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Todays National Weather Map

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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