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INTERPRETATION OF RADAR RETURN FROM CLEAR AIR AND
INTERPRETATION OF RADAR RETURN FROM CONVECTIVE STORMS
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20 knots Arrow length azimuth bull's eyes circulation center color computer algorithms convergence and cyclonic core radius Curved streamlines represent cyclonic rotation divergence region Doppler radar Doppler velocities represent Doppler velocity band Doppler velocity data Doppler velocity displays Doppler velocity pattern Doppler velocity values downdraft edge elevation angle environmental wind field extreme Doppler velocity Figure flow features forecasters gust front length is proportional mesocyclone center mesocyclone core mesocyclone's core region Negative Doppler velocities overall flow pattern pattern in Fig Patterns Associated peak tangential velocity plan position indicator positive Doppler velocity positive velocities represent proportional to wind radar and positive radar beam Radar is 65 Radar location radar points radar return radar viewing direction radial represent the overall simulated Doppler velocity slant range storm motion storm-scale updraft velocities represent flow velocity pattern right Weather Radar wind direction veers wind profile left window zero band zero Doppler velocity