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

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{{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 northeast Colorado.  The radial velocity pattern shown here occurred during the early stages of a blizzard on 26 March, 2009}}
{{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 Colorado.  The 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
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