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Wildfires in Idaho

McIDAS images of GOES-13 0.63 µm visible channel data (above; click image to play animation) showed the smoke plumes emanting from a number of large wildfires that were burning in parts of Idaho on 24 August 2012. Note that some of the low-altitude smoke was being channeled southward through valleys... Read More

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 GOES-13 0.63 µm visible channel data (above; click image to play animation) showed the smoke plumes emanting from a number of large wildfires that were burning in parts of Idaho on 24 August 2012. Note that some of the low-altitude smoke was being channeled southward through valleys by strong northerly winds. The surface visibility at Salmon, Idaho (surface identifier KSMN) was reduced to 2 miles due to smoke, and at Dillon, Montana (station identifier KDLN) the surface visibility dropped to 1.25 miles.

The GOES-13 satellite had been placed into Rapid Scan Operations (RSO) mode, providing images as frequently as every 5-10 minutes (as opposed to the standard 15-minute image interval).

MODIS true color image (viewed using Google Earth)

MODIS true color image (viewed using Google Earth)

A 250-meter resolution Aqua MODIS true color image from the SSEC MODIS Today site (above; viewed using Google Earth) showed a detailed view of the smoke plumes at 20:13 UTC.

Suomi NPP VIIRS 3.74 µm shortwave IR + 0.8 µm Day/Night Band images

Suomi NPP VIIRS 3.74 µm shortwave IR + 0.8 µm Day/Night Band images

During the following night-time hours, a comparison of AWIPS images of Suomi NPP VIIRS 3.74 µm shortwave IR and 0.8 µm Day/Night Band (DNB) data (above) demonstrated how the DNB imagery can detect the glow of the actively-burning fires (co-located with the black to yellow to red color enhanced “hot spots” on the shortwave IR image) in addition to the city lights across the region. Stray light contamination was affecting the far northeastern portion of the DNB image.

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GOES-14 SRSOR: Tropical Storm Isaac

McIDAS images of GOES-14 1-minute interval Super Rapid Scan Operations for GOES-R (SRSOR) 1-km resolution 0.63 µm visible channel images (above; click image to play animation) showed overshooting tops and cloud-top gravity waves associated with a large convective burst located just to the southwest of the center of Read More

GOES-14 0.63 µm visible channel images (click image to play animation)

GOES-14 0.63 µm visible channel images (click image to play animation)

McIDAS images of GOES-14 1-minute interval Super Rapid Scan Operations for GOES-R (SRSOR) 1-km resolution 0.63 µm visible channel images (above; click image to play animation) showed overshooting tops and cloud-top gravity waves associated with a large convective burst located just to the southwest of the center of Tropical Storm Isaac on 23 August 2012.

The corresponding 4-km resolution GOES-14 10.7 µm IR channel images (below) revealed the fluctuation of cold cloud top IR brightness temperatures in the -80 to -90º C range (light to dark purple color enhancement). The white tropical cyclone symbol denotes the 12:00 UTC position of the center of Tropical Storm Isaac according to the National Hurricane Center.

GOES-14 10.7 µm IR channel images (click image to play animation)

GOES-14 10.7 µm IR channel images (click image to play animation)

===== 24 August Update =====

GOES-14 0.63 µm visible channel images (click image to play animation)

GOES-14 0.63 µm visible channel images (click image to play animation)

A GOES-14 visible image animation from early morning on August 24th (above; click image to play animation), about 24 hours after the animation at top, continues to show active convection, although the storm itself remains poorly organized with an elongated center of circulation as seen on OSCAT scatterometer surface winds (below). The presence of increasingly organized curved convective banding is obvious, however.

GOES-13 10.7 µm IR channel images + OSCAT scatterometer surface winds

GOES-13 10.7 µm IR channel images + OSCAT scatterometer surface winds

GOES-14 0.63 µm visible channel images and 10.7 µm images (click image to play animation)

GOES-14 0.63 µm visible channel images and 10.7 µm images, 1200-1259 UTC 24 August 2012 (click image to play animation)

The animation above shows an hour of 1-minute visible (0.63 µm) and Infrared (10.7 µm) imagery starting at 1200 UTC on 24 Friday. The cold cloud tops of the active convection, and the episodic overshooting tops, are evident. Note that the slight flicker that is apparent in the 10.7 µm imagery may be due to the timing of space looks that the ‘cold end’ that is used in the IR calibration. An animation for the one hour starting 1800 UTC is below. Significant changes in the structure of the storm are apparent.

GOES-14 0.63 µm visible channel images and 10.7 µm images (click image to play animation)

GOES-14 0.63 µm visible channel images and 10.7 µm images, 1800-1859 UTC 24 August 2012 (click image to play animation)

For more information on Isaac, refer to the CIMSS Tropical Cyclones site and the National Hurricane Center. One-minute imagery for the storm can be viewed in real time here.

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Flooding Rains in Las Vegas

GOES-14 is in SRSOR operations today and was well-positioned to monitor the flooding rains that occurred in Las Vegas (which received a daily record 1.65 inches of rainfall). The animation above shows cold cloud tops northeast of Las Vegas, with more convection moving in from the southwest. Click here for a large (85... Read More

GOES-14 SRSOR 0.62 µm and 10.7 µm Imagery (click image to play animation)

GOES-14 SRSOR 0.62 µm and 10.7 µm Imagery (click image to play animation)

GOES-14 is in SRSOR operations today and was well-positioned to monitor the flooding rains that occurred in Las Vegas (which received a daily record 1.65 inches of rainfall). The animation above shows cold cloud tops northeast of Las Vegas, with more convection moving in from the southwest. Click here for a large (85 M) animated gif file of one-minute imagery from 1415 UTC through 1859 UTC).

The Blended Total Precipitable Water product (TPW) for this afternoon shows a local maximum in TPW over the southwestern United States. A MIMIC TPW animation suggests that the moisture has originated from a surge up the Gulf of California. During the previous night-time hours, MODIS TPW values of 50-60 mm were seen across far southeastern California, far southwestern Arizona, and in the Las Vegas area as well.

Suomi NPP VIIRS 0.64 µm visible channel and 11.45 µm IR channel images (with cloud-to-ground lightning strikes)

Suomi NPP VIIRS 0.64 µm visible channel and 11.45 µm IR channel images (with cloud-to-ground lightning strikes)

AWIPS images of Suomi NPP VIIRS 0.64 µm visible channel and 11.45 µm IR channel data (above) showed the convective cluster in southern California at 20:29 UTC (which was seen early on the GOES-14 image animation). Cloud top IR brightness temperatures were as cold as -69º C (dark red color enhancement), and a number of cloud-to-ground lightning strikes (mostly of negative polarity) were detected within a 15-minute period as this thunderstorm was growing in size and intensity.

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GOES-14 SRSOR: Fires in northern California

McIDAS images of GOES-14 1-minute interval Super Rapid Scan Operations for GOES-R (SRSOR) 4-km resolution 3.9 µm shortwave IR channel data and 1-km resolution 0.63 µm visible channel data (above; click image to play animation) showed a number of significant wildfires burning across parts of northern California on 21 August 2012. The... Read More

GOES-14 3.9 µm shortwave IR (left) and 0.63 µm visible (right) images (click image to play animation)

GOES-14 3.9 µm shortwave IR (left) and 0.63 µm visible (right) images (click image to play animation)

McIDAS images of GOES-14 1-minute interval Super Rapid Scan Operations for GOES-R (SRSOR) 4-km resolution 3.9 µm shortwave IR channel data and 1-km resolution 0.63 µm visible channel data (above; click image to play animation) showed a number of significant wildfires burning across parts of northern California on 21 August 2012. The largest and most intense fires exhibited pronounced “hot spots” (black to yellow to red color enhancement) on the shortwave IR imagery, with optically-thick smoke plumes on the corresponding visible imagery.

The GOES-14 satellite has been brought out of on-orbit storage to be tested in SRSOR mode through the end of October 2012, allowing it to provide images at 1-minute intervals for an extended period of time over special regions of interest (similar to the future GOES-R satellite, which will be capable of producing imagery at 30-second intervals over special sectors of interest).

During the previous night-time hours, a comparison of AWIPS images of 1-km resolution MODIS 3.7 µm data with the corresponding 4-km resolution GOES-15 3.9 µm shortwave IR data (below) demonstrated the value of improved spatial resolution for identifying the location of smaller fires, as well as more accurately assessing the location and shape of the more intense portions of larger actively burning fires.

MODIS 3.7 µm vs GOES-15 3.9 µm shortwave IR images

MODIS 3.7 µm vs GOES-15 3.9 µm shortwave IR images

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