DPWX/Surface divergence and heavy rainfall beneath a thunderstorm: 19 June 2014

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Revision as of 13:32, 28 August 2014 by Pat kennedy (talk | contribs)

A thunderstorm's heavy precipitation area passes to the south of the CSU-CHILL radar site at 0018:39 UTC on 19 June 2014. The NCAR S-Pol and CSU-CHILL radars conducted synchronized volume scans of this storm during the North Carolina State University Radar Observations of Storms for Education (ROSE) project. A dual-Doppler synthesis of the divergent horizontal wind field that was present at low levels in this storm has been generated.