Hourly Forecast for Galloway, OH
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| Temp (F): | 43° | 41° | 40° | 39° | 38° | 38° | 36° | 36° | 36° | 35° | 39° | 46° |
| Feels Like: | 41° | 39° | 40° | 39° | 38° | 38° | 36° | 36° | 36° | 35° | 39° | 45° |
| Precip: | 0 % | 0 % | 0 % | 0 % | 0 % | 0 % | 0 % | 0 % | 0 % | 0 % | 0 % | 0 % |
| Wind: | N 3 mph |
N 3 mph |
N 2 mph |
NE 2 mph |
NE 2 mph |
NE 2 mph |
NE 2 mph |
NE 2 mph |
NE 2 mph |
NE 2 mph |
NE 2 mph |
E 3 mph |
| Humidity: | 82 % | 85 % | 89 % | 92 % | 92 % | 92 % | 96 % | 96 % | 92 % | 96 % | 89 % | 73 % |
| Dew Point (F): | 38° | 37° | 37° | 37° | 36° | 36° | 35° | 35° | 34° | 34° | 36° | 38° |
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Current U.S. National Radar--Current
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National Weather Forecast--Current
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National Weather Forecast for Tomorrow
Tomorrow National Weather Forecast and Tomorrow National Weather Map are show below.
North America Water Vapor (Moisture)
This map shows recent moisture content over North America. Bright and colored areas show high moisture (ie, clouds); brown indicates very little moisture present; black indicates no moisture.
Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
