Template:Featured Image/May, 2016
From CSU-CHILL
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Radial velocity vectors in an RHI scan of a thunderstorm. Earth-relative radial velocity vectors imply strong, divergent flow in the downstream anvil region of a thunderstorm. Mid-level convergence exists in the nearer-range side of the echo core. (CSU-CHILL S-band data.) Photo credit: Patrick Kennedy |
