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Yukon wildfire produces a pyrocumulonimbus cloud

GOES-18 (GOES-West) Day Land Cloud Fire RGB, Shortwave Infrared (3.9 µm), “Clean” Infrared Window (10.3 µm) and “Red” Visible (0.64 µm) images with an overlay of the Fire Power derived product — Fire Power is a component of the GOES Fire Detection and Characterization Algorithm FDCA — (above) showed signatures associated with a wildfire (located about 20 miles WNW of Mayo,... Read More

GOES-18 Day Land Cloud Fire RGB (top left), Shortwave Infrared (3.9 µm, top right), “Clean” Infrared Window (10.3 µm) (bottom left) and “Red” Visible (0.64 µm) + Fire Power derived product (bottom right) [click to play animated GIF | MP4]

GOES-18 (GOES-West) Day Land Cloud Fire RGB, Shortwave Infrared (3.9 µm), “Clean” Infrared Window (10.3 µm) and “Red” Visible (0.64 µm) images with an overlay of the Fire Power derived product — Fire Power is a component of the GOES Fire Detection and Characterization Algorithm FDCA — (above) showed signatures associated with a wildfire (located about 20 miles WNW of Mayo, Yukon CYMA) that produced a pyrocumulonimbus (pyroCb) cloud late in the day on 06 August 2023.

At 2130 UTC, the wildfire exhibited a maximum 3.9 µm infrared brightness temperature of 106C, with a Fire Power value of 5257 MW (below).

Cursor-sampled values of GOES-18 Day Land Cloud Fire RGB (top left), Shortwave Infrared (3.9 µm, top right), “Clean” Infrared Window (10.3 µm) (bottom left) and “Red” Visible (0.64 µm) + Fire Power derived product (bottom right) at 2130 UTC [click to enlarge]

The pyroCb cloud exhibited a cloud-top 10.3 µm infrared brightness temperature as cold as -48.15C at 2350 UTC (below).

Cursor-sampled values of GOES-18 Day Land Cloud Fire RGB (top left), Shortwave Infrared (3.9 µm, top right), “Clean” Infrared Window (10.3 µm) (bottom left) and “Red” Visible (0.64 µm) + Fire Power derived product (bottom right) at 2350 UTC [click to enlarge]

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Eruption of Mount Shishaldin in the Aleutian Islands

GOES-18 (GOES-West) Ash RGB images (above) showed the northeastward drift of volcanic clouds produced by an eruption of Mount Shishaldin that began just before 1300 UTC on 04 August 2023 (a Mesoscale Domain Sector was positioned over that region at 1603 UTC, providing 1-minute imagery after that time). Those northeast-moving volcanic clouds contained moderate concentrations of ash (denoted... Read More

GOES-18 Ash RGB and SO2 RGB images [click to play animated GIF | MP4]

GOES-18 (GOES-West) Ash RGB images (above) showed the northeastward drift of volcanic clouds produced by an eruption of Mount Shishaldin that began just before 1300 UTC on 04 August 2023 (a Mesoscale Domain Sector was positioned over that region at 1603 UTC, providing 1-minute imagery after that time). Those northeast-moving volcanic clouds contained moderate concentrations of ash (denoted by shades of pink in the Ash RGB images) — then after 1700 UTC, SO2 RGB images revealed the formation of a southeast-moving volcanic cloud that contained modest concentrations of SO2 (shades of yellow) that drifted just to the south of False Pass (in the SO2 RGB images, the northeast-moving ash clouds exhibited darker shades blue). High clouds began to overspread the area from the west after 1830 UTC, which tended to mask the volcanic signatures.

1-minute GOES-18 True Color RGB images from the CSPP GeoSphere site (below) helped to highlight the ash-rich volcanic cloud (shades of tan to brown) moving northeast from the summit of Shishaldin, and also showed the higher-altitude volcanic cloud drifting southeast (which contained SO2).

GOES-18 True Color RGB images [click to play MP4 animation]

A plot of 0000 UTC rawinsonde data from Cold Bay, Alaska (below) indicated that northwesterly winds existed at altitudes of 28000 ft (9 km) and higher, with southwesterly winds below that level (down to altitudes around 20000 ft or 6 km).

Plot of 0000 UTC rawinsonde data from Cold Bay, Alaska [click to enlarge]

Radiometrically-retrieved GOES-18 Ash Cloud Height from the NOAA/CIMSS Volcanic Cloud Monitoring site (below) showed that maximum height values were generally in the 6-8 km (20000-26000 ft) range.

GOES-18 Ash Cloud Height [click to play animated GIF | MP4]

Given that volcanic ash presents a significant hazard to aviation, Volcanic Ash Advisories and Forecasts were issued (below).

GOES-18 Ash RGB image, with Volcanic Ash Advisory (red) and Forecast (violet) polygons issued at 2013 UTC [click to enlarge]

GOES-18 Ash RGB images with a few Pilot Reports that mentioned the altitude of volcanic ash are shown below.

Pilot Report at 1943 UTC, mentioning ash at two different altitudes (moving in different directions) [click to enlarge]


Pilot Report at 2123 UTC, describing volcanic ash (VA) up to an altitude of 24000 ft [click to enlarge]


Pilot Report at 2139 UTC, mentioning volcanic ash (VA) visible 50 miles north of Cold Bay (CDB) at an altitude of 22000 ft [click to enlarge]


Pilot Report at 2223 UTC, describing volcanic ash (VA) suspended at an altitude of 20000 ft [click to enlarge]

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Western Pacific ITCZ changes from 24 July to 2 August 2023

Hourly estimates of Total Precipitable Water (TPW) from MIMIC, shown above in an mp4 animation (click here for an animated gif), show the Intertropical Convergence Zone (ITCZ, as measured by TPW) over the western Pacific evolving from a linear feature at the start of the animation to one with a... Read More

MIMIC Total Precipitable Water, 0000 UTC 24 July – 0000 UTC 2 August 2023

Hourly estimates of Total Precipitable Water (TPW) from MIMIC, shown above in an mp4 animation (click here for an animated gif), show the Intertropical Convergence Zone (ITCZ, as measured by TPW) over the western Pacific evolving from a linear feature at the start of the animation to one with a significant break near 140oE – 150oE longitude. This has occurred as Typhoons Doksuri (moving between the Philippines and Taiwan at the start of the animation) and Khanun (moving south of Japan at the end of the animation) have developed (here is a blog post on the formation of Khanun). Formation of tropical cyclones during the breakdown of the ITCZ is not uncommon (as noted, for example, here, and here). The mp4 animation below (click here for an animated gif) tracks the Upper- and Lower-level water vapor infrared imagery (Himawari-9 Bands 8 and 10 at 6.24 µm and 7.3 µm, respectively) over the same time period.

Himawari-9 Band 8 (top, 6.24 µm) and Band 10 (bottom, 7.3 µm) infrared imagery, 0000 UTC 24 July – 0000 UTC 02 August 2023 with 3-hour timesteps

Himawari-9 Clean Window imagery, below, at 0000 UTC on 24 July (left) and 2 August (right) show little in the way of ITCZ convection between the Equator and 20oN on 2 August, especially compared to 24 July, over the western Pacific. ITCZ convection does persist to the east of 160oE longitude. MIMIC TPW fields at those two times (here) also show a similar rearrangement of convective centers.

Himawawri-9 Clean WIndow (Band 13, 10.4 µm) infrared imagery, 0000 UTC on 24 July (left) and 2 August 2023 (right) (Click to enlarge)

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Typhoon Khanun passes just south of Okinawa Island

Target Sector (2.5-minute interval) JMA Himawari-9 AHI Visible and Infrared images (above) showed Category 4 Typhoon Khanun as it moved just south of Okinawa Island  from 0502-1002 UTC on 01 August 2023. Visible images depicted mesovortces within the eye.During that 0502-1002 UTC time period, peak wind gusts at the 3 METAR sites located in... Read More

JMA Himawari-9 “Red” Visible (0.64 µm, left) and “Clean” Infrared Window (10.4 µm, right) images, from 0502-1002 UTC on 01 August [click to play animated GIF | MP4]

Target Sector (2.5-minute interval) JMA Himawari-9 AHI Visible and Infrared images (above) showed Category 4 Typhoon Khanun as it moved just south of Okinawa Island  from 0502-1002 UTC on 01 August 2023. Visible images depicted mesovortces within the eye.

During that 0502-1002 UTC time period, peak wind gusts at the 3 METAR sites located in the southern part of the island were in the 70-78 knot range (below) — and soon thereafter reached 85 knots at Naha (ROAH) and Futenma (farther north, the peak wind gust at Kadena RODN was 76 knots).

15-minute METAR observations on the island of Okinawa, from 0000-1830 UTC on 01 August [click to play animated GIF | MP4]

Synthetic Aperture Radar (SAR) winds (source) from an overpass of RCM-3 at 0922 UTC (below) did show a swath of strong winds — with speeds in the 80-90 knot range — north and northwest of Khanun’s eyewall, which was beginning to encroach upon the southern portion of Okinawa Island.

RCM-3 SAR winds at 09:22:39 UTC on 01 August [click to enlarge]

ARCHER analysis using DMSP-16 SSMIS Microwave (85 GHz) imagery at 0848 UTC (below) displayed an arc of colder brightness temperatures (shades of orange) just east of the southern end of Okinawa Island.

ARCHER analysis using DMSP-16 SSMIS Microwave (85 GHz) imagery at 0848 UTC [click to enlarge]

A larger-scale animation of Himawari-9 Infrared images covering a longer period of time (below) revealed a small amount of trochoidal motion with the eye of Khanun — which is a behavior often seen with stronger tropical cyclones (for example, here and here).

JMA Himawari-9 “Clean” Infrared Window (10.4 µm) images, from 2352 UTC on 31 July to 0222 UTC on 02 August [click to play animated GIF | MP4

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