Frequent images we obtain from #GOES16 show motion in the atmosphere nicely. Here’s a great loop of fog in the Strait this evening. #wawx http://pic.twitter.com/f0HI1yS8ab
— NWS Seattle (@NWSSeattle) May 21, 2017
** The GOES-16 data posted on this page are preliminary, non-operational data and are undergoing testing. **
As seen in a Tweet from NWS Seattle/Tacoma (above), a plume of fog/stratus moved rapidly eastward through the Strait of Juan de Fuca on 20 May 2017. A closer view of GOES-16 Visible (0.64 µm) images (below; also available as an MP4 animation) shows the formation of “bow shock waves” as the leading edge of the fog/stratus plume reached Whidbey Island at the far eastern end of the Strait near sunset — surface observations indicated that the visibility at Naval Air Station Whidbey Island was reduced to 0.5 mile just after the time of the final 0327 UTC image in the animation.
A Suomi NPP VIIRS Visible (0.6 µm) image with RTMA surface winds (below) showed that the wind speeds were around 15 knots at 21 UTC (just after the primary fog/stratus plume began to move into the western end of the Strait).Suomi NPP VIIRS Visible (0.64 µm) images, with RTMA surface winds plotted in cyan [click to enlarge]
Suomi NPP VIIRS infrared Brightness Temperature Difference (11.45 – 3.74 µm) “Fog/Stratus Product” image, with RTMA surface winds plotted in cyan [click to enlarge]
In the absence of visible imagery at night, evolution of fog is depicted well in #GOES16 fog difference. #wawx From: https://t.co/1tH0TQCKm3 http://pic.twitter.com/j6lMd4tDMa
— Bill Line (@bill_line) May 22, 2017
from CIMSS Satellite Blog http://ift.tt/2q4hnFW
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