Estimations of CIN and LFC Associated with Tornadic and Nontornadic Supercells

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Effective Storm-Relative Helicity and Bulk Shear in Supercell Thunderstorm Environments (2007, result): “This situation is similar to the “large CIN–high level of free convection (LFC)” environments discussed by Davies (2004). Here, a supercell is defined as elevated when the effective inflow base is above the ground in the associated proximity sounding.”
Verification of Convection-Allowing WRF Model Forecasts of the Planetary Boundary Layer Using Sounding Observations (2013, background): “…of 800 and 100 J kg21, respectively, can make a significant difference in the character of forecasted convection (Rasmussen and Blanchard 1998; Davies 2004; Ziegler et al. 2010; Nowotarski et al. 2011), or even whether or not convection develops (Fabry 2006; Wilson and Roberts 2006),…”