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Snow and light drizzle each produce radar reflectivity with about the identical worth. Melting snow and average rain also have related values. Very excessive reflectivity’s (the greys on the dimensions on the image above) are all the time associated with hail.
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Tornadoes are sometimes located at the center of a hook-formed echo on the southwest side of thunderstorms. The hook is best noticed within the reflectivity field. This picture reveals a reflectivity field containing several hook echoes associated with thunderstorms that occurred in Tennessee and Kentucky on May 18https://bojankezastampanje.com 1995. Normallyhttps://bojankezastampanje.com it’s troublesome to tell apart precipitation sort on the basis of the radar reflectivity alone.
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The location of the collared radar echoes indicate the place precipitation is falling and the various colors point out the depth of the precipitation by way of the colour code within the decrease left corner of the image. The example radar picture above shows several sturdy thunderstorms shifting via Illinois and Indiana on April 20https://bojankezastampanje.com 1996. Regions of light and darkish blue point out areas of lighter precipitation while areas of purple and pink point out sturdyhttps://bojankezastampanje.com to sometimes extreme thunderstorms. Full decision knowledgehttps://bojankezastampanje.com however recorded with …
