The study area is located halfway between the Delaware River running through Philadelphia to the east and the peaks of the Blue Ridge Mountains to the west. The total elevation gain of over 600 m along the 250 km section results in upslope enhancement of precipitation for easterly flow. Conversly, strong westerly flows can trigger trains of lee waves from the Blue Ridge Mountains that extend downstream past the Millersville area. On a smaller scale, a number of hills and valleys exist along this rise, including the nearby Sesquehama River which is a favored area of lingering fog that may dissipate under the influence of thermally-driven circulations. The presence of these regimes were monitored during weather briefings that are routinely carried out as part of the campus weather service.
 - Indicates paper has been withdrawn from meeting
 - Indicates paper has been withdrawn from meeting - Indicates an Award Winner
 - Indicates an Award Winner