Bulletin of the American Meteorological Society, Volumen49American Meteorological Society, 1968 Vols. for 1990- contain supplemental membership directory. |
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Página 553
... velocity of the particle beyond the diameter of 6 mm decreases unilaterally . So the range usable for mean Doppler velocity is limited to a certain range . Within the range , mean velocity can be shown approximately in a linear form ...
... velocity of the particle beyond the diameter of 6 mm decreases unilaterally . So the range usable for mean Doppler velocity is limited to a certain range . Within the range , mean velocity can be shown approximately in a linear form ...
Página 554
... velocity GRAHAM M. ARMSTRONG AND RALPH J. DONALDSON , JR . Theoretical scanning requirements of the velocity azimuth display ( VAD ) operation of a pulse Doppler weather radar H. L. GROGINSKY Investigation of Cb phase structure by means ...
... velocity GRAHAM M. ARMSTRONG AND RALPH J. DONALDSON , JR . Theoretical scanning requirements of the velocity azimuth display ( VAD ) operation of a pulse Doppler weather radar H. L. GROGINSKY Investigation of Cb phase structure by means ...
Página 572
... velocity vectors . These sets were further combined into a single array of velocity vectors from each of the two echoes by adjusting the locations of all sets relative to their respective echos The spatial adjustment was made in ...
... velocity vectors . These sets were further combined into a single array of velocity vectors from each of the two echoes by adjusting the locations of all sets relative to their respective echos The spatial adjustment was made in ...
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