Summary/Discussion

• 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.

Slide 23