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Weather radar in Norman, Oklahoma with rainshaft Weather (WF44) radar dish University of Oklahoma OU-PRIME C-band, polarimetric, weather radar during construction. Weather radar, also called weather surveillance radar (WSR) and Doppler weather radar, is a type of radar used to locate precipitation, calculate its motion, and estimate its type (rain, snow, hail etc.).
Weather map. A surface weather analysis for the United States on October 21, 2006. A weather map, also known as synoptic weather chart, displays various meteorological features across a particular area at a particular point in time and has various symbols which all have specific meanings. [1] Such maps have been in use since the mid-19th ...
Artists can use a motion-capture rig to get footage of a human performing an action and then replicate it perfectly with computer-generated imagery so that it looks normal. The lack of anatomically correct digital models contributes to the necessity of motion-capture as it is used with computer-generated imagery.
From local forecasts to global climate patterns, we bring you the latest insights and accurate predictions so you know how to dress and style yourself as you start your day. Dive in and discover ...
The agency was known as the United States Weather Bureau from 1890 until it adopted its current name in 1970. [8] The NWS performs its primary task through a collection of national and regional centers, and 122 local Weather Forecast Offices (WFOs).
On average, 72% of all tornado-related fatalities occur in homes, 54% of which are in mobile homes, according to the National Weather Service. Someone in a mobile home is 15 to 20 times more ...
Microscale meteorology or micrometeorology is the study of short-lived atmospheric phenomena smaller than mesoscale, about 1 kilometre (0.6 mi) or less. [1] [2] These two branches of meteorology are sometimes grouped together as "mesoscale and microscale meteorology" (MMM) and together study all phenomena smaller than synoptic scale; that is ...
Atmospheric circulation. Atmospheric circulation is the large-scale movement of air and together with ocean circulation is the means by which thermal energy is redistributed on the surface of the Earth. The Earth's atmospheric circulation varies from year to year, but the large-scale structure of its circulation remains fairly constant.
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