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Flooding in Alberta, Canada

Very heavy rainfall in much of southwestern Alberta (upwards of 200 mm or 7.9 inches) caused severe flooding in the Calgary (YYC) area beginning on 19 June and 20 June 2013. A sequence of McIDAS images... Read More

GOES-15 6.5 µm water vapor channel images with plots of surface weather (click image to play animation)

GOES-15 6.5 µm water vapor channel images with plots of surface weather (click image to play animation)

Very heavy rainfall in much of southwestern Alberta (upwards of 200 mm or 7.9 inches) caused severe flooding in the Calgary (YYC) area beginning on 19 June and 20 June 2013. A sequence of McIDAS images of hourly GOES-15 6.5 µm water vapor channel data (above; click image to play animation) showed three distinct pulses of moisture that moved across the YYC region during the 18 June – 21 June period. The circulation around an area of low pressure that was moving slowly across the northwestern US (below) allowed deep tropospheric moisture to be transported eastward against the high terrain of the Rocky Mountains, which was a factor in producing such heavy precipitation amounts.

Water vapor image composites + ECMWF model 500 hPa geopotential heights

Water vapor image composites + ECMWF model 500 hPa geopotential heights

 

Blended Total Precipitable Water product

Blended Total Precipitable Water product

The Blended Total Precipitable Water product (above) showed TPW values as high as 31 mm or 1.2 inches over much of the region on the morning of 20 June — these TPW values were 190-200% above normal for this area and this time of the year (below).

Blended Total Precipitable Water Percent of Normal product

Blended Total Precipitable Water Percent of Normal product

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Summer Solstice in Alaska

GOES-15 (GOES-West) 0.63 µm visible channel images (above; click image to play animation) showed the cloud features over much of Alaska on 21 June 2013 (the day of the summer solstice). Record heat had been occurring across much of Alaska during the previous week, and Barrow (BRW) had a daily... Read More

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)

GOES-15 (GOES-West) 0.63 µm visible channel images (above; click image to play animation) showed the cloud features over much of Alaska on 21 June 2013 (the day of the summer solstice). Record heat had been occurring across much of Alaska during the previous week, and Barrow (BRW) had a daily record high temperature of 62 F on 20 June. Note that there were numerous thunderstorms that developed over the Brooks Range and even over the North Slope regions of Alaska — on 20 June, over 4000 cloud-to-ground lightning strikes were detected. The haziness seen early in the animation was due to widespread smoke from wildfires that had been burning in southwestern Alaska a few days earlier.

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West Fork and East Park fires in southern Colorado

Two large fires burning in southern Colorado began to produce pyrocumulonimbus clouds and very large smoke plumes, as seen on GOES-13 0.63 µm visible channel (top panels) and 3.9 µm shortwave IR images (bottom panels)  on 19 June (above; click image to play... Read More

GOES-13 0.63 µm visible channel and 3.9 µm shortwave IR channel images (click image to play animation)

Two large fires burning in southern Colorado began to produce pyrocumulonimbus clouds and very large smoke plumes, as seen on GOES-13 0.63 µm visible channel (top panels) and 3.9 µm shortwave IR images (bottom panels)  on 19 June (above; click image to play animation) and on 20 June 2012 (below; click image to play animation). The larger fire on the left is the West Fork Complex, while the smaller fire on the right is the East Park fire.

GOES-13 0.63 µm visible channel and 3.9 µm shortwave IR channel images (click image to play animation)

A comparison of AWIPS images of POES AVHRR 0.86 µm visible channel, Cloud Top Temperature (CTT) product, and Cloud Top Height (CTH) product at 21:25 UTC (below) showed that CTT values just downstream of the fire source were as cold as -60 C (darker red color enhancement), where CTH values were as high as 12 km (darker green color enhancement).

POES AVHRR visible channel image, Cloud Top Temperature product, and Cloud Top Height product

POES AVHRR visible channel image, Cloud Top Temperature product, and Cloud Top Height product

Some photos of the West Fork Complex pyrocumulonimbus clouds are shown below, from the Wildfire Today site.

Photo of West Fork Complex fire

Photo of West Fork Complex fire

 ===== 21 June Update =====

GOES-15 (left panels) and GOES-13 (right panels) visible and shortwave IR channel  images (click image to play animation)

The West Fork fire complex continued to burn at an explosive rate on 21 June — a comparison of GOES-15 (left panels) and GOES-13 (right panels) 0.63 µm visible channel and 3.9 µm shortwave IR channel images ((above; click image to play animation) showed two very large smoke plumes with pyrocumulonimbus (pyroCb) clouds forming near the source of the fires.

A layer of high cirrus clouds began to move over the fire region later in the afternoon and early evening (01 UTC satellite images), masking the view of the pyroCb clouds and smoke plumes; however, the fire “hot spots” (red enhanced pixels) could still be sensed through the veil of high clouds. At around 01:04 UTC, a fantastic photo (photo 2 | photo 3 | photo 4) of the fire was taken by Luis Rosa (NWS San Juan Puerto Rico) from a passenger aircraft flying at 35,000 feet which showed the northernmost pyroCb cloud — likely the Papoose Fire –  beneath the cirrus cloud layer (below).

Aerial view of pyrocumulonimbus cloud associated with the West Fork Fire Complex

Aerial view of pyrocumulonimbus cloud associated with the West Fork Fire Complex

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Tornado at Denver International Airport

A tornado touched down just east of the Denver International Airport concourses at 20:21 UTC on 18 June 2013, producing a peak wind gust of 97 mph (before the wind instrumentation stopped transmitting data).  AWIPS images of Suomi NPP VIIRS 0.64 µm visible... Read More

Suomi NPP VIIRS 0.64 um visible image and 11.45 um IR channel image (with overlay of METAR surface reports)

Suomi NPP VIIRS 0.64 um visible image and 11.45 um IR channel image (with overlay of METAR surface reports)

A tornado touched down just east of the Denver International Airport concourses at 20:21 UTC on 18 June 2013, producing a peak wind gust of 97 mph (before the wind instrumentation stopped transmitting data).  AWIPS images of Suomi NPP VIIRS 0.64 µm visible channel and 11.45 µm IR channel data at 20:03 UTC (above) showed the storm about 20 minutes before it produced the tornado. The minimum cloud-top IR brightness temperature was -68º C (darker red color enhancement), which was significantly colder that the tropopause temperature of -56º C on the 12 UTC Denver rawinsonde data.

The corresponding Suomi NPP VIIRS true-color Red/Green/Blue (RGB) image (viewed using the SSEC Web Map Server) is shown below.

Suomi NPP VIIRS true-color Red/Green/Blue (RGB) image

Suomi NPP VIIRS true-color Red/Green/Blue (RGB) image

The series of METAR surface reports from Denver (KDEN) during the period from 20:20 to 20:37 UTC:

KDEN 182037Z 09026KT 9SM -TSRA FEW050 BKN080CB BKN180 24/04 A3002 RMK FUNNEL CLOUD B18 FUNNEL CLOUD E20 TORNADO B21 TORNADO E36 AO2 LTG DSNT NE-S RAB03 TORNADO 2 SE MOV N P0005
KDEN 182032Z 09026KT 7SM +FC -TSRA FEW050 BKN080CB BKN180 22/08 A3001 RMK FUNNEL CLOUD B18 FUNNEL CLOUD E20 TORNADO B21 AO2 LTG DSNT NE-S RAB03 TORNADO 2 SE MOV N P0005
KDEN 182022Z 06021G28KT 5SM +FC TSRA FEW050 BKN080CB BKN180 21/07 A3002 RMK FUNNEL CLOUD B18 FUNNEL CLOUD E20 TORNADO B21 AO2 PK WND 07028/2020 LTG DSNT E-S RAB03 OCNL LTGICCG VC E TS OHD MOV E VIRGA SW P0005
KDEN 182021Z 06022G28KT 5SM +FC TSRA FEW050 BKN080CB BKN180 21/06 A3003 RMK FUNNEL CLOUD B18 FUNNEL CLOUD E20 TORNADO B21 AO2 PK WND 07028/2020 LTG DSNT E-S RAB03 OCNL LTGICCG VC E TS OHD MOV E VIRGA SW P0005
KDEN 182020Z 07020G28KT 5SM FC +TSRA FEW050 BKN080CB BKN180 21/07 A3003 RMK FUNNEL CLOUD B18 AO2 PK WND 07028/2020 LTG DSNT E-S RAB03 OCNL LTGICCG VC E TS OHD MOV E VIRGA SW P000

McIDAS images of GOES-13 0.63 µm visible channel data (below; click image to play animation) showed the development of the thunderstorms over the region

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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