Search Results

You are looking at 1 - 1 of 1 items for :

  • Bulletin of the American Meteorological Society x
  • Ontario Winter Lake-effect Systems (OWLeS) x
  • All content x
Clear All
David A. R. Kristovich, Richard D. Clark, Jeffrey Frame, Bart Geerts, Kevin R. Knupp, Karen A. Kosiba, Neil F. Laird, Nicholas D. Metz, Justin R. Minder, Todd D. Sikora, W. James Steenburgh, Scott M. Steiger, Joshua Wurman, and George S. Young

(WCR) dual-Doppler analysis showed a solenoidal circulation pattern with near-surface convergence over each lake, buoyant updrafts about 1 km deep, and divergence aloft ( Bergmaier and Geerts 2016 ). Near the downwind shores light snowfall became more widespread as a result of orographic ascent and band interactions with more complex terrain. OBSERVED PROCESSES AND PHENOMENA. Mesoscale band circulation patterns. Previous studies have found that surface buoyant forcing over the relatively warm

Full access