Same thing happens in the western Willamette Valley when we are in the icebox and a low pressure system overruns it. The eastern outflow from the Columbia River Gorge toward the low center creates a cold air dam that pushes the column of cold air in the west valley higher, so as to delay or outright prevent freezing rain or sleet developing (such as what happened in 2008). This is why places like Lebanon, Silverton and areas in the east valley have the warm nose affect them sooner with freezing rain/sleet or simply rising above freezing in the lower levels sooner than, say, McMinnville, Grand Ronde, Dallas, Monmouth/Independence, and sometimes even Philomath/Corvallis