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Cyclonic Storm Jawad and Typhoon Nyatoh in GK2A imagery

South Korea’s GK2A satellite (carrying the AMI instrument that is very similar to both AHI on Himawari-8 and ABI on GOES-16/GOES-17) is overhead on the Equator at 128 E Longitude, and satellite imagery (link) and products (link) are available online. The low-level Water Vapor animation (GK2A Band 10, 7.3 µm),... Read More

GK2A Low-level water vapor (Band 10, 7.3 µm), hourly from 0740 to 1640 UTC on 3 December 2021 (Click to enlarge)

South Korea’s GK2A satellite (carrying the AMI instrument that is very similar to both AHI on Himawari-8 and ABI on GOES-16/GOES-17) is overhead on the Equator at 128 E Longitude, and satellite imagery (link) and products (link) are available online. The low-level Water Vapor animation (GK2A Band 10, 7.3 µm), above, hourly from 0740 to 1640 UTC on 3 December 2021, shows the evolution of Nyotah from a symmetric to asymmetric storm in the central Pacific. The 1500 UTC Advisory from the Joint Typhoon Warning Center shows a storm south and east of Japan that is forecast to weaken significantly in the next two days. The animation also shows Jawad in the Bay of Bengal in a moist corridor between very dry low-level air over southeast Asia and western India/the Arabian Sea. The 1500 UTC advisory for Jawad suggests modest strengthening in the next day then landfall near the border of India and Bangladesh.

MIMIC Total Precipitable Water fields for the 24 hours ending 1600 UTC on 3 December 2021, below, show drying around Nyotah, and the deep (but somewhat isolated) moisture surrounding Jawad.

MIMIC Total Precipitable Water fields, 1700 UTC 2 December – 1600 UTC 3 December 2021 (Click to enlarge)

One of the products available at the GK2A product site is Rain Rate, and a toggle of that product at 1540 UTC (overlain on top of clean window infrared imagery) and low-level water vapor imagery is shown below. Heaviest instantaneous rains are diagnosed in the ITCZ Monsoon trough centered near Indonesia.


Thanks to KMA for making these awesome products and channels available!

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Assessing the freezing level with NUCAPS profiles

The highest peaks of the Big Island of Hawai’i are under Blizzard warnings as of early 3 December 2021, as shown in the screen capture below from the National Weather Service in Honolulu.The image above shows NUCAPS Sounding Availability in AWIPS over the central Pacific. A long swath of profiles was available from a... Read More

The highest peaks of the Big Island of Hawai’i are under Blizzard warnings as of early 3 December 2021, as shown in the screen capture below from the National Weather Service in Honolulu.

Graphical Forecast for Hawaii, 1907 UTC on 3 December 2021
NUCAPS Soundings Availability plots over the central Pacific Ocean, 1201 UTC on 3 December 2021. Profiles at select points as indicated. Text shows the Total Precipitable Water and the diagnosed freezing level (Click to enlarge)

The image above shows NUCAPS Sounding Availability in AWIPS over the central Pacific. A long swath of profiles was available from a NOAA-20 overpass near 1200 UTC. Each of the dots represents a profile of temperature and moisture over the Pacific, a large region with little observational data. These retrieved profiles can give useful information about the structure of the atmosphere in advance of a storm. In this case, moisture is apparent, and so is mid-tropospheric drying; thus, evaporational cooling from precipitation might be important. The freezing level of the profiles is also shown, and most values are near 12500′. (Mauna Loa and Mauna Kea top out at 13,679′ and 13,803′, respectively). Note that the relatively low freezing levels extend far to the south, as shown in this NUCAPS profile at 17.3N, 160 W, at the southern edge of the domain above!

Two of the NUCAPS soundings in the animation above are near upper-air radiosondes at Hilo and at Lihue. A toggle between the Hilo sounding and NUCAPS profile is just below; underneath that profile is the toggle between the Lihue soundings and the adjacent NUCAPS profile. Keep in mind with these comparisons that the radiosonde is a sensor at one point moving up through the atmosphere whereas the NUCAPS profile represents a large volume of air. Gross aspects of the two soundings agree: moisture in the levels, dry air aloft.

Hilo (PHTO) rawindsonde at 1200 UTC on 3 December 2021, and a nearby NUCAPS Profile at the same time (Click to enlarge)
Lihue (PHLI) rawindsonde at 1200 UTC on 3 December 2021, and a nearby NUCAPS Profile at the same time (Click to enlarge)

Individual NUCAPS profiles can be aggregated into gridded fields to depict values along horizontal surfaces. These can be found at this website, for example, from SPoRT. The 850-mb field (a level far below the peaks!) shows temperatures near freezing not too far north of Hawai’i.

Gridded NUCAPS temperature values at 850 mb at 1141 UTC on 3 December 2021 (Click to enlarge)

AWIPS tip: It can be tedious to load up individual soundings. PopUp SkewTs can be used in AWIPS to quickly scan through the profiles to identify any threshold values. PopUp SkewTs can be accessed under the Volume Browser.


NUCAPS Sounding Availability points, 1209 UTC on 8 December 2021

Added, 8 December 2021: The NUCAPS Sounding Availability plot, above, shows a swath several days after the snow, and after warmer air has moved in from the east. The easternmost sounding just south of 20 N, below, shows a freezing level closer to 14600′!

NUCAPS Profiles near 20 N, 154 W, 1208 UTC on 8 December 2021 (Click to enlarge)

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Lower-tropospheric vortex north of Hawai’i

GOES-17 (GOES-West) “Red” Visible (0.64 µm) images, with and without plots of Visible Derived Motion Winds (above) showed a lower-tropospheric vortex propagating west-northwestward to the north of Hawai’i on 02 December 2021. There were no ship or buoy reports in the vicinity of the vortex, but Derived Motion Wind speeds were 20-25 knots... Read More

GOES-17 “Red” Visible (0.64 µm) images, with and without plots of Derived Motion Winds [click to play animated GIF | MP4]

GOES-17 (GOES-West) “Red” Visible (0.64 µm) images, with and without plots of Visible Derived Motion Winds (above) showed a lower-tropospheric vortex propagating west-northwestward to the north of Hawai’i on 02 December 2021. There were no ship or buoy reports in the vicinity of the vortex, but Derived Motion Wind speeds were 20-25 knots or less during this time period.

Convergence near the center of the vortex was aiding in the development of some shallow convection — and GOES-17 Day Cloud Phase Distinction RGB images (below) indicated that the tops of many cloud features comprising the vortex were glaciating (exhibiting shades of green to yellow),

GOES-17 Day Cloud Phase Distinction RGB images [click to play animated GIF | MP4]

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Quiz Time: What county in the USA has all boundaries visible from satellite?

MODIS-derived (from Terra and Aqua satellites) Bidirectional Reflectance Distribution Function (BRDF), above, (as noted in this blog post), shows the (meager) snow distribution as of early December. How many counties (or parishes) in the United States (out of more than 3000!) are clearly delineated in Satellite Imagery such as what is shown... Read More

MODIS-derived BRDF from 1 December 2021 (Click to enlarge)

MODIS-derived (from Terra and Aqua satellites) Bidirectional Reflectance Distribution Function (BRDF), above, (as noted in this blog post), shows the (meager) snow distribution as of early December. How many counties (or parishes) in the United States (out of more than 3000!) are clearly delineated in Satellite Imagery such as what is shown above? Counties that are primarily islands (or peninsulas) — Dare County in North Carolina, for example — show up well (False Color image shown here, in an image taken from VIIRS Today), but the inland borders do not.

For a county to be recognizable from Space, its landcover must differ significantly from adjacent counties. In the zooming-in animation below (from RealEarth, click the image to zoom in), users will note that Menominee County in northeast Wisconsin becomes apparent. Menominee County is almost entirely forest (unlike its neighbors) and as such has a much different signal in the (for example) 0.87 µm channel on VIIRS (or 0.86 µm on GOES-16). When it is zoomed in, the outlines of the County are obvious.

MODIS-derived BRDF from 1 December 2021 at various zoom levels (Click to animate)

The county also shows up well in the VIIRS True Color/False Color toggle below, from 30 November. The southern edge of the snow at that time was just southeast of Menominee County, and the land-use change across the county border is apparent. Snow in the county (cyan in the False Color enhancement) is difficult to view from the imagery — because of the pine forests!

VIIRS True-Color and False-Color imagery over northeastern WI, 1838 UTC on 30 November 2021 (Click to enlarge)

Menominee County has been on this blog before! In 2007, a tornado tracked through Menominee County and left a visible scar in satellite imagery (link). Eight years later (link), the scar was still apparent! November 6 2021 was a clear day over the upper Midwest. Suomi-NPP True Color imagery, below (link to original large image), still shows vestiges of the scar!

Suomi NPP True-Color imagery, 6 November 2021. The outline of Menominee County is apparent, as is the southwest-to-northeast tornado scar

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