16.3 BASELINE CLIMATOLOGY OF SOUNDING DERIVED PARAMETERS ASSOCIATED WITH DEEP, MOIST CONVECTION

By J. Craven, H. Brooks, J. Hart. 2002

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Citations in the corpus

A Review of Planetary Boundary Layer Parameterization Schemes and Their Sensitivity in Simulating Southeastern U.S. Cold Season Severe Weather Environments (2015, background): “) in diameter], the necessary conditions are moisture, lift, instability, and vertical wind shear, which are highly variable across the wide spectrum of convection that ensues (e.g., Johns and Doswell 1992; Rasmussen and Blanchard 1998; Thompson et al. 2003; Craven and Brooks 2004; Schneider and Dea”
Global climatology of Convective Available Potential Energy (CAPE) and Convective Inhibition (CIN) in ERA-40 reanalysis (2009, methodology): “For convective precipitation, and severe weather analysis and forecasting the parameter CAPE (ConvectiveAvailable Potential Energy) is used (e.g. Rasmussen and Blanchard, 1998; Craven et al., 2002; Markowski et al., 2002; Brooks et al., 2003; Brooks et al., 2007; Doswell and Evans, 2003).”
Estimations of CIN and LFC Associated with Tornadic and Nontornadic Supercells (2004, unknown): “The area of the diagram enclosed by dashed lines corresponds to combinations of 0–1-km shear and MLLCL more likely to be associated with tornadoes from Craven et al. (2002a).”
Close Proximity Soundings within Supercell Environments Obtained from the Rapid Update Cycle (2003, methodology): “Schwartz and Benjamin (2002a) discussed various choices in CAPE calculations and documented 3- h RUC errors similar to our MLCAPE errors, and Craven et al. (2002b) found that a 100-hPa mean parcel was superior to a surface parcel in determining parcel ascent.”
Climatology and Ingredients of Significant Severe Convection in High-Shear, Low-CAPE Environments (2014, background): “…composite parameter [SCP; effective-layer version from Thompson et al. (2004)], the vorticity generation parameter10 (VGP; Rasmussen and Blanchard 1998), the energy helicity index10 (EHI; Rasmussen and Blanchard 1998), and the Craven–Brooks significant severe parameter (Craven and Brooks 2004).”
A Climatology of Tornadoes in Europe: Results from the European Severe Weather Database (2014, methodology): “Both Storm Data (e.g., Rasmussen and Blanchard 1998; Thompson et al. 2003; Craven and Brooks 2004), and the ESWD (Kaltenböck et al. 2009; Brooks 2009, 2013) have been used in such studies, combining storm reports with radiosonde measurements or data from numerical atmospheric models.”
Refined Supercell and Tornado Forecast Parameters (2003, result): “It should be noted that other multiyear climatological studies have been conducted to attempt to confirm or to refute these recent findings (Craven et al. 2002).”
Characteristics of Vertical Wind Profiles near Supercells Obtained from the Rapid Update Cycle (2003, background): “…importantly, tornadic versus nontornadic supercells (e.g., Rasmussen and Wilhelmson 1983; Brooks et al. 1994a; Davies 1998, 2002; Rasmussen and Blanchard 1998; Markowski et al. 1998; Thompson 1998; Edwards and Thompson 2000; Thompson and Edwards 2000; Brooks and Craven 2002; Craven et al. 2002).”