I just got back from spending the weekend over in Asheville, NC. Asheville is an awesome city (minus the hideous road system), and my girlfriend and I took in several of the “touristy” things to do in the area, with my favorite probably being the Biltmore Estate. Now, I’m no history buff (in fact, unless weather or sports are involved I usually don’t like talking history), however, in my older age, I am beginning to appreciate the subject I hated most through my elementary school days, but that Biltmore House is simply remarkable, and I found myself drifting back to thinking what it would have been like living here in 1895 when the house opened (Christmas Eve, to be exact- how’s that for a Christmas present?!). A tour to the Biltmore House coupled with many stops in the shops and restaurants through the town made for a really enjoyable weekend.
ANYWAY…it was really interesting watching the wedge set up along the eastern slope of the Blue Ridge. When we talk about the wedge (or cold air damming events) all it is is a cold push of air, most of the time associated with high pressure (centered over New England or the mid Atlantic) nosing a chilly northeasterly flow into the southern Appalachian region. Similar to northwesterly upslope flow events on this side of the mountain, a northeasterly flow is an upslope flow for the eastern half of the divide. This pushes shallow cold air down the eastern slopes of the mountains and can lead to ice storms quite frequently during the winter months. Now while the CAD, or wedge, typically impacts the eastern slope of the Appalachians (from Boone, Blowing Rock south to Asheville and even into GA), if the event is strong enough, the cooler air can “ooze” down the Trade gorge and impact the eastern sections of Johnson County as well. Such was the case this weekend.
When we arrived in Asheville Saturday morning, temperatures were in the middle 50s, with showers and a westerly wind. That said, as the afternoon ”churned” on, I felt the wind back around to the east and within minutes of the wind shift, temperatures began a slow decline. The slow decline in temperatures was also accompanied by low clouds, fog, and drizzle. Sunday was stuck in the upper 30s to lower 40s. (Even a little light freezing rain was reported in the Blowing Rock community earlier in the day). As we ventured back “over the mountain” that chilly easterly upslope flow switched around to a “milder” downslope flow on the TN side of the mountain (in Unicoi County). That low cloudiness and fog gave way to brightening skies, a ten degree temperature jump, and a gusty downsloping wind.
Ah…you have to love mountain weather!
(Thanks to Intellicast for the above graphic).
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