Yesterday's Weather for Newtown, PA

Your Recent Locations:  Newtown, PA  

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

Yesterday's High was 47 °F

Yesterday's Low was 36 °F

Yesterday's Precipitation was 0.00 inches

Observations on November 20, 2017:
Time Temp Wind Conditions
12:53 AM EST 39.0 °F 8.1 mph Clear
1:53 AM EST 39.0 °F 5.8 mph Clear
2:53 AM EST 37.9 °F 9.2 mph Clear
3:53 AM EST 37.0 °F 9.2 mph Clear
4:53 AM EST 36.0 °F 6.9 mph Clear
5:53 AM EST 37.0 °F 10.4 mph Mostly Cloudy
6:53 AM EST 37.0 °F 11.5 mph Clear
7:53 AM EST 37.0 °F 9.2 mph Clear
8:53 AM EST 39.0 °F 11.5 mph Clear
9:53 AM EST 42.1 °F 15.0 mph Clear
10:53 AM EST 43.0 °F 16.1 mph Clear
11:53 AM EST 44.1 °F 12.7 mph Clear
12:53 PM EST 46.0 °F 12.7 mph Clear
1:53 PM EST 46.0 °F 9.2 mph Clear
2:53 PM EST 46.9 °F 11.5 mph Clear
3:53 PM EST 45.0 °F 10.4 mph Clear
4:53 PM EST 44.1 °F 8.1 mph Clear
5:53 PM EST 43.0 °F 3.5 mph Clear
6:53 PM EST 42.1 °F 5.8 mph Clear
7:53 PM EST 41.0 °F 3.5 mph Clear
8:53 PM EST 39.9 °F 4.6 mph Clear
9:53 PM EST 37.9 °F 5.8 mph Clear
10:53 PM EST 37.9 °F 3.5 mph Clear
11:53 PM EST 37.0 °F 4.6 mph Clear
 
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Weather Topic: What are Contrails?

Home - Education - Cloud Types - Contrails

contrails Next Topic: Fog

A contrail is an artificial cloud, created by the passing of an aircraft.

Contrails form because water vapor in the exhaust of aircraft engines is suspended in the air under certain temperatures and humidity conditions. These contrails are called exhaust contrails.

Another type of contrail can form due to a temporary reduction in air pressure moving over the plane's surface, causing condensation. These are called aerodynamic contrails.

When you can see your breath on a cold day, it is also because of condensation. The reason contrails last longer than the condensation from your breath is because the water in contrails freezes into ice particles.

Next Topic: Fog

Weather Topic: What are Fractus Clouds?

Home - Education - Cloud Types - Fractus Clouds

fractus clouds Next Topic: Hole Punch Clouds

A fractus cloud (scud) is a fragmented, tattered cloud which has likely been sheared off of another cloud. They are accessory clouds, meaning they develop from parent clouds, and are named in a way which describes the original cloud which contained them.

Fractus clouds which have originated from cumulus clouds are referred to as cumulus fractus, while fractus clouds which have originated from stratus clouds are referred to as stratus fractus. Under certain conditions a fractus cloud might merge with another cloud, or develop into a cumulus cloud, but usually a fractus cloud seen by itself will dissipate rapidly.

They are often observed on the leading and trailing edges of storm clouds, and are a display of wind activity.

Next Topic: Hole Punch Clouds