Template:Featured Image/June, 2009: Difference between revisions

From CSU-CHILL

(Placeholder for June)
 
m (Fixed typos)
 
(One intermediate revision by one other user not shown)
Line 1: Line 1:
{{POTM|image=17apr2009 LDR bband anot.png|title=LDR bright band|credit=Pat Kennedy|text=Enhanced return signal depolarization associated with the melting level in an RHI scanSurface observers in the high LDR areas reported large, wet, aggregated snow particles.}}
{{POTM|image=Web jun09 vel anot.png|title=Low-level Radial Velocity Maximum|credit=Pat Kennedy|text=Low level wind maxima are often observed in the CSU-CHILL data during deep cyclonic upslope winter precipitation events in northeastern ColoradoThe radial velocity pattern shown here occurred during the early stages of a blizzard on 26 March, 2009}}

Latest revision as of 13:11, 1 June 2009

Low-level Radial Velocity Maximum Low-level Radial Velocity Maximum

Low level wind maxima are often observed in the CSU-CHILL data during deep cyclonic upslope winter precipitation events in northeastern Colorado. The radial velocity pattern shown here occurred during the early stages of a blizzard on 26 March, 2009

Photo credit: Pat Kennedy
More featured pictures...