Others blogs have also noted this clouds, including Scott Sistek KOMO Weather Blog. On that blog, he had a very nice picture taken by Dan Magden.
And perhaps most extraordinary of all, the cam on the top of the atmospheric science building caught the brief generation and dissipation of this breaking wave clouds (click on picture to view):
And, of course, you need the atmosphere to be close enough to saturation to get such clouds.
Meteorologist can use our numerical models to simulate such KHI. You can view one by clicking on the picture below:
If you look at the photos above you will notice, that many of the waves are breaking to the left, but some...on the right hand side...seem to be breaking to the right. This seemed really strange to me and to a number of you. I had never seen this before. Perhaps it is just an illusion.
So let's play detective a bit.
How high were the clouds? Looking at probably the closest airport to the action (Boeing Field), the reported cloud base was 6000 ft, which seems reasonable from the pictures.
What were the winds and temperatures aloft at that time? Well, we have some good luck...an aircraft landed at Seattle-Tacoma Airport during the previous hour (3:20 PM) and took atmospheric measurements.
Here is the sounding from the plane. Heights are given in terms of pressure: keep in mind that 850 represents about 5000 ft and 700 about 10,000 ft. Blue is wind speed and white is temperature. In the area of the wave clouds the winds were from the west, with little change in direction. There is modest wind shear in that layer (increasing from roughly 7 meters per second at 5000 ft to 12 meters per second at 10000 ft). Roughly double winds in meters per second to convert to knots.
So in the layer of the clouds the wind was increasingly westerly with height, which should tend to shear the waves to the east as we see for most of the clouds. But why did some of the clouds on the western side of the line appear to shear in the opposite direction?
Perhaps the winds over the western part of the Sound were different aloft.
But we don't have any observations there. But wait, we do have our very high resolution WRF model. Here are the winds forecast for 4 PM at 850 hPa (again around 5000 ft) for the central Puget Sound from that model. The winds do appear to shift across the Sound to an easterly direction there..you can see the winds splaying out over Seattle. The winds above the airport are much more westerly. So one speculation is that there was a layer of opposite shear west of the city and that produced the opposite cant of the waves there. But if there was a reversal of the shear, I can not see how there would be a continuous line of the wave clouds. So that supports the illusion theory.
I am open for suggestions on this one....
And if you still hunger for more clouds, click on this wonderful cloud video produced by Greg Johnson. It even has music.
http://vimeo.com/82890411
Fracking and Ozone
UW Professor Becky Alexander has established a page on the Microoryza crowdfunding web site that outlines her project to understand why natural gas fracking often leads to high ozone values over snow (go here to see it). If you want to learn more about this important project and how you can help it happen, check out the web site.
UW Professor Becky Alexander has established a page on the Microoryza crowdfunding web site that outlines her project to understand why natural gas fracking often leads to high ozone values over snow (go here to see it). If you want to learn more about this important project and how you can help it happen, check out the web site.
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