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Northward advection of stratus along the Oregon and Washington coasts

An AWIPS image of the Suomi NPP VIIRS 11.45 – 3.74 µm IR brightness temperature difference “fog/stratus product” at 10:26 UTC or 2:26 AM local time on 11 September 2013 (above) revealed a relatively narrow tongue of stratus cloud (darker orange to red... Read More

Suomi NPP VIIRS IR brightness temperature difference "fog/stratus product"

Suomi NPP VIIRS IR brightness temperature difference “fog/stratus product”

An AWIPS image of the Suomi NPP VIIRS 11.45 – 3.74 µm IR brightness temperature difference “fog/stratus product” at 10:26 UTC or 2:26 AM local time on 11 September 2013 (above) revealed a relatively narrow tongue of stratus cloud (darker orange to red color enhancement) which was beginning to move northward along the nearshore coastal waters of Oregon. The northward stratus advection was being driven by the presence of an elongated trough of low pressure off the West Coast of the US, with some embedded closed low circulations along the trough axis.

During the subsequent daylight hours, McIDAS images of GOES-15 0.63 µm visible channel data (below; click image to play animation) showed the continued northward and northwestward spread of the plume of stratus cloud along and just off the coast of Washington, with some inland intrusions of marine stratus noted later in the day. One of the aforementioned closed cyclonic circulations (which was not well-analyzed by the GFS40 model surface winds on the VIIRS image above) could be seen within the marine boundary layer stratus off the coast of Oregon. Other features of interest included the dispersion of smoke plumes from 2 small wildfires that were burning in southwestern Oregon. Meteorological fun fact: on this day, for the Lower 48 states both the daily lowest temperature (22º F at Silver Lake) and the daily highest temperature (102º F at Medford) occurred in the state of Oregon!

GOES-15 0.63 µm visible channel images (click image to play animation)

GOES-15 0.63 µm visible channel images (click image to play animation)

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Regeneration of Tropical Storm Gabrielle

After a four and a half day hiatus, Tropical Storm Gabrielle began to regenerate south of Bermuda on 10 September 2013. AWIPS images of 1-km resolution POES AVHRR 0.86 µm visible channel and 12.0 µm IR channel data at 13:41 UTC (above) showed... Read More

POES AVHRR 0.84 µm visible channel and 12.0 µm IR channel images (with overlays of surface buoy, surface analysis, and ASCAT winds)

POES AVHRR 0.84 µm visible channel and 12.0 µm IR channel images (with overlays of surface buoy, surface analysis, and ASCAT winds)

After a four and a half day hiatus, Tropical Storm Gabrielle began to regenerate south of Bermuda on 10 September 2013. AWIPS images of 1-km resolution POES AVHRR 0.86 µm visible channel and 12.0 µm IR channel data at 13:41 UTC (above) showed overlays of surface buoys, surface analysis, and ASCAT surface scatterometer winds. A number of these ASCAT winds exhibited speed values of 45-46 knots, prompting NHC to adjust the intensity of Gabrielle upward:

TROPICAL STORM GABRIELLE SPECIAL DISCUSSION NUMBER   9
NWS NATIONAL HURRICANE CENTER MIAMI FL       AL072013
130 PM AST TUE SEP 10 2013

A PAIR OF ASCAT PASSES FROM 1342Z AND 1436Z INDICATE THAT GABRIELLE 
IS STRONGER THAN PREVIOUSLY ESTIMATED. BOTH PASSES SHOWED SEVERAL 
45-KT WIND RETRIEVALS...AND THAT IS THE INITIAL INTENSITY FOR THIS
SPECIAL ADVISORY. THE INTENSITY FORECAST HAS BEEN ADJUSTED UPWARD
AT 12 AND 24 HOURS TO 50 KT BASED ON THE INCREASE IN THE INITIAL
INTENSITY. THE ANALYZED 34-KT WIND RADII HAVE ALSO BEEN ADJUSTED
OUTWARD BASED ON THE ASCAT DATA...AND THEIR FORECAST HAS BEEN
MODIFIED AS WELL TO REFLECT THE LARGER WIND FIELD. AN AIR FORCE
RESERVE AIRCRAFT WILL INVESTIGATE GABRIELLE LATER THIS AFTERNOON TO
PROVIDE MORE DETAILED INFORMATION ON THE STRENGTH AND STRUCTURE OF
THE CYCLONE.
850 hPa relative vorticity product (04-10 September) - click image to play animation

850 hPa relative vorticity product (04-10 September) – click image to play animation

A sequence of 6-hour interval 850 hPa relative vorticity product images from the CIMSS Tropical Cyclones site (above; click image to play animation) showed that the lower-tropospheric vorticity feature associated with Tropical Storm Gabrielle remained fairly intact during the 06-10 September period (between the times when Gabrielle had exhibited tropical cyclone organization and intensity).

GOES-13 0.63 µm visible channel images (click image to play animation)

GOES-13 0.63 µm visible channel images (click image to play animation)

McIDAS images of 1-km resolution GOES-13 0.63 µm visible channel data (above; click image to play animation) revealed a well-defined central dense overcast (CDO) convective burst early in the day, followed by the emergence of the low-level circulation of Gabrielle as the middle and high-altitude cloud layers were sheared off to the northeast.

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GOES-15 Navigation Anomalies

GOES-15, in service as GOES-West over the Equator at 135 W, has experienced navigation anomalies on each of the past three mornings, September 8, 9 and 10, 2013 (as noted here, for example). Navigation anomalies occur approximately between 0830 and 1100 UTC. GOES Engineers are investigating the source of the... Read More

GOES-15 3.9 µm shortwave IR images on 10 September (click image to play animation)

GOES-15 3.9 µm shortwave IR images on 10 September (click image to play animation)

GOES-15, in service as GOES-West over the Equator at 135 W, has experienced navigation anomalies on each of the past three mornings, September 8, 9 and 10, 2013 (as noted here, for example). Navigation anomalies occur approximately between 0830 and 1100 UTC. GOES Engineers are investigating the source of the anomaly, which can be on the order of 40 km. The animation above is the shortwave infrared from Tuesday 10 September. Animations for 6, 7, 8 and 9 September are below. Note that even the 6 September and 7 September have small navigation issues.

(Update: From SATOPS: NOTE: GOES-15 (West) Image registration (alignment of images to earth grid coordinates) was shifted by approximately 40 kilometers on DOY251 (ed. note: 8 September) from 08:50z to 10:50z and shifted by approximately 25 kilometers on DOY252 & DOY253 (ed. note: 9 and 10 September) from 9:30z to 10:40z. The earth coordinate grid shift was due to a lack of available valid star data for predicting the proper attitude pointing profile around eclipse. The root cause is under investigation.) In other words, the Star Pointer was unable to find enough targets to produce accurate navigation. (Link)

Update, 11 September: The anomalies continued on 11 September, starting after the 0845 UTC image, peaking at the 1000 UTC image, and subsiding by 1045 UTC. Link.

Update, 17 September: Large navigation anomalies were not present overnight.

GOES-15 3.9 µm shortwave IR images on 6 September (click image to play animation)

GOES-15 3.9 µm shortwave IR images on 6 September (click image to play animation)

GOES-15 3.9 µm shortwave IR images on 7 September (click image to play animation)

GOES-15 3.9 µm shortwave IR images on 7 September (click image to play animation)

GOES-15 3.9 µm shortwave IR images on 8 September (click image to play animation)

GOES-15 3.9 µm shortwave IR images on 8 September (click image to play animation)

GOES-15 3.9 µm shortwave IR images on 9 September (click image to play animation)

GOES-15 3.9 µm shortwave IR images on 9 September (click image to play animation)

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Morgan Fire northeast of San Francisco

The Morgan Fire began burning in the Mount Diablo State Park northeast of San Francisco during the afternoon hours on 08 September 2013, which caused the evacuation of dozens of homes near the fire. McIDAS images of 4-km resolution GOES-15 3.9 µm shortwave... Read More

GOES-15 3.9 µm shortwave IR images (click image to play animation)

GOES-15 3.9 µm shortwave IR images (click image to play animation)

The Morgan Fire began burning in the Mount Diablo State Park northeast of San Francisco during the afternoon hours on 08 September 2013, which caused the evacuation of dozens of homes near the fire. McIDAS images of 4-km resolution GOES-15 3.9 µm shortwave IR data (above; click image to play animation; also available as a .mp4 file) revealed that the fire “hot spot” (red color enhancement) first appeared on the 21:30 UTC (2:30 PM local time) image. The fire appeared to “settle down” for a few hours after sunset, but then there was an apparent flare-up of the fire from 04:00 – 06:30 UTC.

One thing to note on the GOES-15 shortwave IR animation above is that there was a significant Image Navigation and Registration (INR) anomaly during the 08:45 – 10:41 UTC period. An AWIPS 1-km resolution Suomi NPP VIIRS 3.74 µm shortwave IR image was available at 09:24 UTC (during the GOES-15 INR anomaly) — a comparison of this VIIRS image with the closest available GOES-15 shortwave IR image (below) demonstrates the value of higher spatial resolution VIIRS data to aid in a more accurate determination of the actual fire size and location.

Suomi NPP VIIRS 3.74 µm and GOES-15 3.9 µm shortwave IR images

Suomi NPP VIIRS 3.74 µm and GOES-15 3.9 µm shortwave IR images

Hot spots associated with the ongoing Rim Fire — so far the 3rd-largest fire on record in California — can also be seen about 100 miles to the east-southeast.

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