- #Weather radar in motion ohio update
- #Weather radar in motion ohio archive
- #Weather radar in motion ohio full
- #Weather radar in motion ohio plus
Use radar data with caution especially if your area of interest is far from the nearest radar location! A lot can happen between 0 and 5,000 feet and therefore the depiction of precipitation given by radar may differ some from what’s actually happening on the ground. Because of this phenomenon, the radar beam will only see precipitation falling through the mid levels of the atmosphere. To see this in action, imagine a circle (earth) with a straight line emanating from some point on the circle if you continue this line out into space, it will gradually get farther and farther from the circle. Because the earth is round and the radar beam is flat, the farther away from the radar tower the beam (energy) travels, the farther removed from the ground becomes. There is a notable constraint to radar data though. This is the highest resolution radar data available which enables you to see features such as sea breeze or outflow boundaries that standard resolution radar entirely misses. This data is gathered from over a hundred radar towers located across the US.
#Weather radar in motion ohio plus
Adfree Plus (with extra features) Extra.Lake Murray, Ardmore OK (WeatherOK, USA).
#Weather radar in motion ohio archive
#Weather radar in motion ohio update
The URL will automatically update as you select the view and settings.
#Weather radar in motion ohio full
This view provides a full map view of all alert hazards (similar to WWA map). This view is similar to a radar application on a phone that provides radar, current weather, alerts and the forecast for a location. This view combines radar station products into a single layer called a mosaic and storm based alerts. This view provides specific radar products for a selected radar station and storm based alerts. This site is organized into views that provide relevant radar products and weather information for a common task or goal.