During the one month period of IMPROVE-2 an active weather pattern setup over the eastern Pacific, with a series of frontal systems making landfall along the Pacific Northwest coast. This resulted in over 2 meters of snowfall over the Oregon Cascades during the first two weeks of the experiment alone. The first part of the experiment was highlighted by a significant trough passage on 28-29 November (IOP1), which produced ~ 0.3-1 m of snowfall over the mountains. The S-Pol radar provided information on particle types, while the NOAA P-3 aircraft mapped out the low-level flow using the tail Doppler radar, and the University of Washington Convair-580 aircraft collected microphysical measurements aloft. Other significant events, which targeted more post-frontal regimes, will be highlighted. Some of the case studies are being simulated down to 1.3 km resolution using the Penn State-NCAR mesoscale model (MM5). These modeling results will be compared with observations.
Supplementary URL: