Template:Featured Image/March, 2014
From CSU-CHILL
|
Layered air flow CSU-CHILL S-band radial velocity data in an RHI scan on azimuth 015 degrees. Inbound (negative in sign) velocities maximize within the surface-based, post cold frontal airmass. Above 2 km AGL, the direction of the synoptic flow varies with height in a way that causes the radial velocity observed in the RHI plane to have layers with both positive and negative signs. (Both away from and towards the radar motion components.) Photo credit: Pat Kennedy |
