So much of our interesting weather is associated with air moving up and down our substantial terrain and tomorrow will be a stellar example. Huge weather contrasts will occur tomorrow over the lowlands. In some locations, wind will gust to 60-80 mph--as strong as Hurricane Sandy--while 20-30 miles away you will barely feel a breeze. In some lowland locations there will be not a single flake, while 20-30 miles away nearly a foot could snarl traffic.
December 25, 2012 Weather |
Boring Weather Comes With No Terrain |
With strong southeasterly winds over the Cascade crest and a big east-west pressure difference over the mountains, we have a very good set up for very strong easterly downslope winds on the western Cascade slopes and adjacent lowlands of western Washington. Enumclaw, Black Diamond, North Bend and many eastside communities will get hit hard, with wind gusts reaching 50-70 mph in a few places. Trees will fall. Power will fail. And strong winds will occur in the Strait and over the offshore waters. Forget your sailing lessons unless you want to end up in the mid-Pacific.
Here are the predicted maximum gusts (in knots) at 1 PM tomorrow from the super-high resolution WRF 1.3km resolution model. Wow. Gusts reaching 60 knots over parts of the Strait and offshore of the central WA coast. 45 knot (52 mph) gusts along the western Cascade foothills at that time (with some higher values).
What about snow? The National Weather Service and I are generally on the same page (SE of the Olympics is the focus), but they are going for the possibility of a few inches over Seattle and vicinity.
Looking at the latest runs, I believe it will be too warm for snow in Seattle and that the powerful easterlies will dry things out enough to lessen the snow chances near sea level around the Seattle Metro area. Here is the latest WRF model forecast. First, the 24h ending 4 PM Christmas Day. Same story as yesterday: Kitsap and Mason counties get the brunt of the lowland snow.
The next 24-h (ending 4 PM on Wednesday). Eastern Washington's turn!
But although I think the above is the most probably scenario, the snow level could descend toward the high hills of the lowlands if the precipitation is heavier and the easterly flow weakens more than forecast. This is a classic Seattle snow forecasting problem: temperatures are marginal and everything depends on precipitation rate and the temperature/humidity structure of the air above us. By the end of the afternoon it will be too warm for snow that is clear. But I have learned not to be too confident about Seattle snow and freezing rain forecasts.
Roads are relatively warm right now. Here is the latest air and road (boxes) temperatures from Seattle SNOWWATCH. Elevated and non-elevated roadways are in the 40s. That is good place to start. If clouds come in soon enough tonight, temperatures will not fall too much and even if few flakes hit the road, they will melt quickly.
Your introduction makes a fine point--we are lucky indeed to live in western Washington, with its unmatched local variation in climate, and its even greater variation in weather. Even better, we live in the Northwest where the Consortium's WRF-GFS modeling, combined with the admirable skill of our local Federal forecast office, makes it easy for all of us to reap the benefits of this variation. On any but the rarest of bad days there is SOME place in western Washington where the weather is good enough to enjoy being outdoors, and it's the WRF that lets us find that place. Over the past ten years or more, the WRF has spared me a great deal of time, grief, and money by enabling me to find just the right time and place to enjoy our region's delightful natural heritage--which, in turn, is so delightful partly as an environmental consequence of our great local variation in climate.
ReplyDeleteNow, an off-topic question: In a news article about the severe cold weather currently afflicting eastern Europe, the BBC wrote "The harsh weather has been attributed to a high pressure front over Russia and Kazakhstan."
What is a "high pressure front"?
Cliff,
ReplyDeleteWith all due respect, do you think you sometimes rely too much on the UW WRF-GFS? Is it me, or has it under-performed in past snow events of the last couple of years (although it pretty much nailed last week's snow here north of Seattle)? NAM clearly shows snow to sea-level in all of Puget Sound, so it'll be interesting to see how it pans out. As of this writing, it surely doesn't seem like it'll be cold enough, but, as NWS points out, dry air from the east may play a decisive role.
I hope that NAM is correct. (Don't we all :)?)
Merry Christmas.
Alex,
ReplyDeleteFirst, the WRF this year is considerably different than WRF last year...major upgrades. But more important, the temperatures are too warm. Dry easterly air cuts both ways...yes, it promotes evaporational cooling, but it also lessens precip intensity which is crucial for bringing down the freezing level. In addition, the ECMWF model and others concur with the WRF...not good for snow over Seattle...cliff
When you mention "boring rain", does "boring" mean "dull" or "drilling"? :-)
ReplyDeleteIt tried to snow here in Olalla - about 9:30 or so it snowed quite hard for a little while, and slush started to accumulate on cars and lawns. But it was 34 degrees then, and the snow changed quickly enough to boring rain.
ReplyDeleteI hope you are having a great Christmas Day!
Nice dusting of snow here at 1050' MSL in Preston. Some gusty winds but we are just outside the typical "foothills windstorm" regions so we don't typically get high winds in these scenarios.
ReplyDeleteUsed to live on the hwy 516 corridor near Covington - what an incredible micro-climate that is - about a kilometer wide stretch where it can be calm just blocks to the north or south, but the region coming from Four Corners towards Covington is a wind tunnel. I'll bet the winds are howling there today.
Cliff, your forecast was extremely accurate. All rain in Olympia, and ten miles North, Northwest in Shelton I was able to get the Subaru into the snow:
ReplyDeletehttp://imgur.com/a/CFrrr#2