Extended Abstract (1.3M)P1.7
The 4–5 December 2001 IMPROVE-2 event: Orographic flow and precipitation structures and evaluation of model microphysics
Brian A. Colle, Stony Brook University / SUNY, Stony Brook, NY; and Y. Lin, C. P. Woods, and B. F. Smull
Numerous ground-based and aircraft observations were collected over the central Oregon Cascades during the second Improvement of Microphysical Parameterization through Observational Verification Experiment (IMPROVE-2). The most analyzed IMPROVE-2 IOP to date occurred on 13-14 December 2001, which featured strong cross barrier flow (30-40 m/s) and a well-defined landfalling baroclinic wave. This presentation extends the results of IMPROVE-2 by focusing on a weaker orographic precipitation event on 4-5 December 2001, during which the cross barrier flow and precipitation rates were about half as large as the 13-14 December IOP. The weaker flow on 4-5 December resulted in less gravity wave activity over the Cascades and less lee side spillover of precipitation over the Cascade crest. NOAA P-3 observations suggest that there was also less riming over the windward ridges at 2-4 km ASL on 4-5 December as compared to 13-14 December.
The 4-5 December event was simulated down to 1.33-km grid spacing using the both the Pennsylvania State University-NCAR Mesoscale Model (MM5 v3.7) and Weather Research and Forecasting (WRF v2.1) model using the NCEP GFS for initial and boundary conditions, Mellor-Yamada-Janjic (Eta) PBL, Kain-Fritsch convective parameterization on the 36- and 12-km grids, and the Thompson microphysical parameterization, which includes graupel processes. Both MM5 and WRF realistically simulated the three dimensional thermodynamic and kinematic fields at 1.33-km grid spacing, including 1-2 m/s vertical velocities produced by the narrow windward ridges. However, both models overpredicted surface precipitation over portions of the lower windward slope and immediate lee of the Cascade crest, which is similar to other IMPROVE-2 case studies. Microphysical comparison with NOAA P-3 in situ measurements showed that both models produced 2-3 times as much snow as observed at 2-3 km ASL over the Cascades using the Thompson bulk microphysical scheme, while cloud water was overpredicted above some of the windward peaks. The various bulk schemes within MM5 and WRF were also tested, with sensitivity simulations used to explain some of the fundamental bulk scheme differences.
Poster Session 1, Precipitation and Boundary Layers in Complex Terrain
Monday, 28 August 2006, 2:30 PM-4:00 PM, Ballroom North
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