Rasmussen: both pseudo-global warming and downscaling approaches find decreased weak convection and increased strong convection in a future climate, associated with larger CAPE and larger CIN over central and eastern CONUS
Rasmussen: both pseudo-global warming and downscaling approaches find decreased weak convection and increased strong convection in a future climate, associated with larger CAPE and larger CIN over central and eastern CONUS
Mullendore: Lower entrainment in observed updrafts for high shear, high LCLs, high ECAPE, low midlevel RH, and low MUCAPE; first such analysis for midlatitude continental storms
Mullendore: Lower entrainment in observed updrafts for high shear, high LCLs, high ECAPE, low midlevel RH, and low MUCAPE; first such analysis for midlatitude continental storms
Lane: Stratiform orientation and system tilt in Australian linear convection determined by MUCAPE and deeper layers of shear, rather than 0-3-km shear or possible cold pool strength
Lane: Stratiform orientation and system tilt in Australian linear convection determined by MUCAPE and deeper layers of shear, rather than 0-3-km shear or possible cold pool strength
Marinescu: among fields important for convective storms, CAPE, near-surface winds, and mid-tropospheric moisture are most variable, and temperature and upper-level winds are least variable
Marinescu: among fields important for convective storms, CAPE, near-surface winds, and mid-tropospheric moisture are most variable, and temperature and upper-level winds are least variable
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