Template:Featured Image/November, 2016
From CSU-CHILL
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Radial velocity patterns in a trailing stratiform echo region. Horizontally layered S-band radial velocity pattern in a CSU-CHILL RHI scan. Rear inflow towards more distant convection maximizes at mid-levels. Divergence occurs in the surface based-layer beneath the melting level (shown by the X-band 27 dBZ contour). Photo credit: Patrick Kennedy |
