Yesterday's Weather for New York, NY

Your Recent Locations:  New York, NY  

How much rain or snow did New York, NY get yesterday? The answer is below!

Yesterday's High was 65 °F

Yesterday's Low was 44 °F

Yesterday's Precipitation was 0.00 inches

Observations on February 23, 2017:
Time Temp Wind Conditions
12:51 AM EST 52.0 °F 0.0 mph Scattered Clouds
1:51 AM EST 50.0 °F 0.0 mph Clear
2:51 AM EST 48.9 °F 0.0 mph Clear
3:51 AM EST 46.9 °F 3.5 mph Clear
4:51 AM EST 46.0 °F 3.5 mph Clear
5:51 AM EST 45.0 °F 3.5 mph Clear
6:51 AM EST 44.1 °F 0.0 mph Clear
7:51 AM EST 48.0 °F 0.0 mph Clear
8:17 AM EST 48.0 °F 3.5 mph Mostly Cloudy
8:43 AM EST 48.9 °F 0.0 mph Overcast
8:51 AM EST 48.9 °F 5.8 mph Overcast
9:51 AM EST 52.0 °F 4.6 mph Overcast
10:51 AM EST 54.0 °F 0.0 mph Overcast
11:51 AM EST 53.1 °F 9.2 mph Haze
12:51 PM EST 57.0 °F 9.2 mph Haze
1:51 PM EST 60.1 °F 5.8 mph Haze
2:51 PM EST 64.0 °F 3.5 mph Clear
3:51 PM EST 64.9 °F 4.6 mph Clear
4:51 PM EST 61.0 °F 6.9 mph Clear
5:51 PM EST 61.0 °F 4.6 mph Clear
6:51 PM EST 59.0 °F 3.5 mph Clear
7:51 PM EST 57.9 °F 3.5 mph Mostly Cloudy
8:51 PM EST 55.9 °F 0.0 mph Clear
9:51 PM EST 63.0 °F 4.6 mph Partly Cloudy
10:51 PM EST 64.0 °F 4.6 mph Clear
11:51 PM EST 63.0 °F 5.8 mph Scattered Clouds
 
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Weather Topic: What are Nimbostratus Clouds?

Home - Education - Cloud Types - Nimbostratus Clouds

nimbostratus clouds Next Topic: Stratocumulus Clouds

A nimbostratus cloud is similar to a stratus cloud in its formless, smooth appearance. However, a nimbostratus cloud is darker than a stratus cloud, because it is thicker.

Unlike a stratus cloud, a nimbostratus cloud typically brings with it the threat of moderate to heavy precipitation. In some cases, the precipitation may evaporate before reaching the ground, a phenomenon known as virga.

Next Topic: Stratocumulus Clouds

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