There are some interesting elements about the upcoming Northwest heat wave that I wanted to share.
This is NOT going to be an historic heat wave west of the Cascades...but we could well break a daily high temperature record on Monday. So don't expect the high 90s, with peaks about 100F, that we experienced in late July 2009. And there is a chance of some major thunderstorms...but just a chance.
So why will this event be modest? The reason is that the set-up is not correct for one of the big events, because the low-level pressure distribution will be wrong and we won't have sustained offshore flow. Specifically, to get a big heat wave west of the Cascades, we need the upper-level ridge (high pressure) right over us and low-level high pressure to OUR EAST, which encourages offshore flow.
Here is the latest WRF forecasts for the upper air (500 hPa) and sea level pressure (and lower atmosphere temperatures) for Monday at 5 PM. The upper level ridge is centered over Idaho and there is lower pressure over eastern Oregon. There is a hint of a weak thermal trough over the Cascades, but some of that is bogus for reasons I won't get into here. There is on onshore pressure gradient (difference) west of the Cascades, which allows marine air to seep in.
The ridge is so large and strong, and the air is so warm associated with it, that western of the Cascades will still be far above normal: upper 80s to 90 is quite reasonable on Monday and Tuesday, especially away from the water. Eastern Washington, protected from the marine influence and closer to the ridge, will be far warmer: many locations will get to 100-110F. I assume the grapes will like it. Fire danger should be modest because of the recent rains, but the ground will dry quickly with the heat.
Will any records be broken? Well, for Seattle Tacoma Airport I suspect the daily record will fall on Monday. As shown below (look at the second to last column), the record high for Monday is 87F...we have a good chance of exceeding that.
There will be surge of offshore flow near crest level of the Cascades that should result in the highest temperatures that day and Tuesday, but then the pattern will shift subtly after that as a weak system approaches from the west. The result will be increased onshore flow and slow cooling. Into the lower 80s on Wed. and 70s on Thursday, with the return of morning low clouds.
For me a very interesting aspect of this event is the development of very high instability in the lower atmosphere, instability that can lead to thunderstorms. A key measure of the potential thunderstorm "juice" is something called CAPE (Convective Available Potential Energy). Here is the plot for Monday at 5 PM. I don't think I have ever seen such high values here in the NW...reaching 2500-3000. High for us is usually in the few hundred.
The reason the models are not producing massive convection is due to the sinking motion of the high and the lack of strong upward motion necessary to release this instability. In fact, here is the 48-h precipitation forecast ending 5 AM on Wednesday...some convective showers, mainly over the Cascades.
But the models would not have to be very wrong for something very interesting and severe to happen. Need to watch this.
One more thing...does it feel unusually humid outside....reminiscent of the eastern U.S.? Well, it is! Check out the latest dew point temperatures, shown below. (Note dew point is a good measure of the amount of moisture in the air. Starts feeling sticky in the 60s).
Lots of values in the 60s, some in the upper 60s...this is relatively unusual around here and it occurring because today is warming up substantially with a lot of recent rains and wet ground. All the water is evaporating into the air.
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