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  • 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.

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