Random notes on the big storm
By Scott SistekWith the main story focusing on the forecast, I'll use the blog to highlight some cool stuff going on amidst the madness, most recent post at the top. Sunday 10:35 p.m.: Sunday 10:35 a.m.: It works for snow too -- you can see what people in the network have been reporting at this link (defaults to King County) then just adjust the map to change it to snow and for whatever county you live in or are interested in. By the way, they are still looking for volunteers! If you'd like to join, information is available on their site. Saturday 12:35 p.m.: They warmed back to normal on New Years' Eve and that was the end -- they actually warmed into the 50s by Jan. 11. Here's the same stats for Bellingham: (Thanks to Alan for e-mailng this to me) 18th: High 41, Low 16; flurries Saturday 12:15 p.m. I compiled this using Google Earth, so you can do this yourself if you've downloaded that program. Saturday: 11:50 a.m.
Saturday 8:40 a.m.: First, orient yourself with a map of British Columbia: And here are the current conditions for a few cities along the valley: Also, for weather geeks, watch the pressure gradients -- i.e., the difference in pressure in milibars between Bellingham (BLI) and Williams Lake (YWL) -- it's the table on the upper right and most recent is on top. Anytime that gets into the -15 to -20 range, that means there's a very strong difference in pressure between those two cities, with the pressure some 15 to 20 milibars higher in Williams Lake than Bellingham, and a strong northeast wind follows. That's generated because cold air is very dense and thus is associated with very high atmospheric pressure. Friday 6:35 p.m:
Friday 6:20 p.m.
Friday 2:30 p.m.: And this site from the UW is the holy grail. There's a link at the top of the page that gives what the station codes represent. Column "SP" is sustained speed, "GS" is gust. But on some, if you look over to the right in the comments field, there's a "PK WND" designation, which is the highest gust reported in the hour. It's given as a few numbers, like: "PK WND 13041/2103". The 130 is the wind direction on the compass (so, a southeast wind), the 41 is the speed in knots, and 2103 is the time recorded in UTC, which is 8 hours ahead of PST. So in this case, which is Friday Harbor in their 2 p.m. observation, they had a peak hourly gust of 41 knots from 130 degrees at 1:03 p.m. To convert knots to mph, multiply knots by 1.15. (so, 47 mph.) Finally, if you look in the URL, there's a "what=0" at the end. You can change that '0' to a number to get past hours -- i.e., if you change the 0 to a 1, you'll get the observations from one hour back. '2' is two hours, etc. Friday 1:15 p.m.:
That was caused by strong southwest flow that squeezes out its moisture when it goes up the southwesern side of the Olympic Mountains. The air then dries out when it sinks down the northeastern side of the Olympics. And note who is in the middle of that clearing hole? Sequim, as usual. There's a reason they only get 18" of rain a year :) * Pressure was falling quite rapidly as this storm energized offshore. This photo is from my father's weather station in Port Angeles:
Note the pressure going straight down. Port Angeles' pressure dropped 37 millibars -- from 30.17 to 29.12 on the inches of mercury scale -- between midnight and 1pm. Amazing! Friday: 10:00 a.m.: I'll keep adding tidbits here through Friday and the weekend. |
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