Session 18 |
| Mesoscale And Synoptic Scale Processes And Severe Convection II |
| Organizers: Nolan T. Atkins, Lyndon State College, Lyndonville, VT; Harald Richter, NOAA/NSSL, Norman, OK
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| 10:30 AM | 18.1 | An analysis of low-level moisture flux convergence prior to the 3 May 1999 Oklahoma City tornadoes Ralph A. Petersen, NOAA/NWS/NCEP, Camp Springs, MD; and W. F. Feltz, J. Schaefer, and R. Schneider |
| 10:45 AM | 18.2 | The role of storm/boundary anchoring in the development of supercells in high bulk richardson number environments Adam L. Houston, Univ. of Illinois, Urbana, IL; and R. B. Wilhelmson |
| 11:00 AM | 18.3 | The suppression of deep moist convection near the southern plains dryline Harald Richter, NOAA/NSSL, Norman, OK; and L. F. Bosart |
| 11:15 AM | 18.4 | Airborne Doppler analysis of a dryline-outflow boundary intersection and subsequent convection Christopher C. Weiss, Univ. of Oklahoma, Norman, OK; and H. B. Bluestein |
| 11:30 AM | 18.5 | The vertical distribution of humidity: a crucial factor in the organization of convection George H. Bryan, Penn State Univ., University Park, PA; and J. M. Fritsch |
| 11:45 AM | 18.6 | The evolution of two tornadic supercells into an intense bow echo over southwest Nebraska and northwest Kansas Eric Martello, NOAA/NWS, Jackson, MS |