The mesoscale analyses shown will demonstrate the relative impacts of assimilating frequent PECAN soundings, vertical profilers (wind and thermodynamic retrievals), low-flying research aircraft in situ data, and mobile radar clear air radial velocities. Although analyses assimilating no observations for a 4-5 hour period prior to CI do reasonably well at producing the observed convection, and all analyses initiate convection 1-2 hours early, all assimilated research observation types at least subtly improve the ensemble representation of convection at its earliest stages. A possible exception includes the assimilation of large quantities of clear air radar radial velocities directly surrounding the location of CI. Surprisingly, assimilation such data appear to disrupt the observed organization of storms at their CI stage. This presentation will demonstrate what aspects of the environment (e.g., local areas of elevated mesoscale convergence, gravity waves, elevated moisture, etc.) are improved via the assimilation of non-conventional observation types that were collected in PECAN.
- Indicates paper has been withdrawn from meeting
- Indicates an Award Winner