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While strong ambient wind fields/vertical shear are relatively common during the cool season, the occurrence of significant tornadoes in the Gulf Coast states appears to be highly sensitive to boundary layer moisture (surface dewpoints 60-65°F or higher in nearly all cases) and relatively subtle changes in available buoyancy. This study will further incorporate composite synoptic patterns, sounding/thermodynamic analysis, and examination of convective mode in an effort to help improve operational forecasting of significant cool season tornadoes in the Gulf Coast states. Student participation was funded by the NOAA Hollings Scholarship program and 2005 Research Experiences for Undergraduates (REU).