Yesterday's Weather for Orrstown, PA

Recent Locations: Orrstown, PA  

How much rain or snow did Orrstown, PA get yesterday? The answer is below!

Yesterday's High was 64 °F

Yesterday's Low was 37 °F

Yesterday's Precipitation was 0.00 inches

Observations on October 19, 2018:
Time Temp Wind Conditions
12:53 AM EDT 46.9 °F 0.0 mph Clear
1:53 AM EDT 42.1 °F 0.0 mph Clear
2:53 AM EDT 41.0 °F 3.5 mph Clear
3:53 AM EDT 42.1 °F 3.5 mph Clear
4:53 AM EDT 37.9 °F 0.0 mph Clear
5:53 AM EDT 37.9 °F 0.0 mph Clear
6:53 AM EDT 37.9 °F 3.5 mph Clear
7:53 AM EDT 37.9 °F 0.0 mph Clear
8:53 AM EDT 42.1 °F 5.8 mph Clear
9:53 AM EDT 46.9 °F 3.5 mph Clear
10:53 AM EDT 53.1 °F 6.9 mph Clear
11:53 AM EDT 55.0 °F 5.8 mph Clear
12:53 PM EDT 57.0 °F 3.5 mph Clear
1:53 PM EDT 60.1 °F 4.6 mph Clear
2:53 PM EDT 62.1 °F 9.2 mph Clear
3:53 PM EDT 63.0 °F 11.5 mph Clear
4:53 PM EDT 62.1 °F 12.7 mph Clear
5:53 PM EDT 61.0 °F 12.7 mph Clear
6:53 PM EDT 57.9 °F 8.1 mph Clear
7:53 PM EDT 59.0 °F 9.2 mph Clear
8:53 PM EDT 59.0 °F 10.4 mph Clear
9:53 PM EDT 59.0 °F 3.5 mph Scattered Clouds
10:53 PM EDT 57.9 °F 8.1 mph Overcast
11:53 PM EDT 59.0 °F 10.4 mph Overcast
 
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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