- While primarily a pulse day, it appears outflow interaction was able to sustain/enhance the primary area of convection over Madison/Chenango counties.
- Westernmost outflow remained stationary, provided an anchored convergence zone.
- The stationary movement was made possible by low-level northwesterly flow.
- Outflow from ALB CWA brought another area of enhanced convergence.
- These two outflow boundaries appeared to merge over Madison/Chenango counties.