A benefit of Polar Orbiters over northernmost Alaska is a wealth of NUCAPS soundings from NOAA-20! The animation above shows useful profiles near Utqiagvik AK (formerly Barrow) for the nine hours between 1132 and 2128 UTC on 5 December 2021. The vibrant green point is the point selected for the profiles shown below. Note that the profiles at 1633, 1810 and 1948 UTC were microwave-only; that is, the infrared retrieval did not converge (click here to see the distribution from 1633-1948 UTC; you’ll see yellow points in the region near Utqia?vik). The sounding availability suggests near-continuous (at 90-minute timesteps!) monitoring of the tropopshere during the day.

The animation below shows 4 profiles (for which the infrared solution converged in the retrieval); A consistent warming in the profiles is noted, and perhaps a slight drying as well. The tropopause is also shown to rise. These profiles are not reliant on numerical model data; they are an independent measure of the polar atmosphere. It’s important to view similar dot colors in this kind of animation. The animation at the bottom of the post includes in the animation the microwave-only profiles at 1635, 1914 and 1953 UTC. The IR+MW profiles below have far different character than MW-only profiles at bottom; however, the MW-only profiles also show a slow warming.

These NUCAPS profiles were displayed using a method that is detailed here, developed by scientists at STC and SPoRT. NWS forecasters who are interested in this functionality can contact the blog author.

Note that the high temperatures in Utqiagvik (Barrow) on 3, 4 and 5 December were 0º, 19º, and 25º F, respectively, entirely consistent with the warm advection depicted in the NUCAPS profiles.

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GOES-16 Near-Infrared “Snow/Ice” (1.61 µm) images (credit: Tim SchmIt, NOAA/NESDIS) [click to enlarge | MP4]

GOES-16 (GOES-East) Near-Infrared “Snow/Ice” (1.61 µm) images (above) showed the shadow of a total solar ecliipse in the Southern Hemisphere on 04 December 2021. Even though the 1.61 µm imagery is at a lower (1 km) spatial resolution, it provided better contrast than higher-resolution (0.5 km) 0.64 µm “Red” Visible imagery, helping to highlight the shadow (below). Note that the shadow passed over the Antarctic Peninsula.

GOES-16 “Red” Visible (0.64 µm) and Near-Infrared “Snow/Ice” (1.61 µm) images (credit: Tim Schmit, NOAA/NESDIS) [click to enlarge]

GOES-16 CIMSS True Color RGB images created using Geo2Grid (below) provided another view of the eclipse shadow’s progression. 

GOES-16 CIMSS True Color RGB images (credit: Tim Schmit, NOAA/NESDIS) [click to play animated GIF | MP4]

In a 3-panel comparison of GOES-16 “Red” Visible (0.64 µm), Near-Infrared “Snow/Ice” (1.61 µm) and Shortwave Infrared (3.9 µm) images (below), note that the lack of solar reflection within the eclipse shadow led to cooler 3.9 µm brightness temperatures (lighter shades of gray).    

GOES-16 “Red” Visible (0.64 µm, top), Near-Infrared “Snow/Ice” (1.61 µm, middle) and Shortwave Infrared (3.9 µm, bottom) images (credit: Tim Schmit, NOAA/NESDIS/ASPB) [click to play animated GIF | MP4]

The shadow was also apparent in GOES-17 (GOES-West) images (below).

GOES-17 Near-Infrared “Snow/Ice” (1.61 µm) images [click to play animated GIF | MP4]

A composite of POES AVHRR Visible (0.63 µm) swaths around 0700 UTC (below) showed the shadow extending southward across South Georgia and the South Sandwich Islands and reaching the coast of Antarctica. 

Composite of POES AHVRR Visible (0.63 µm) swaths [click to enlarge]

In addition, portions of the solar eclipse shadow could be seen in True Color RGB images from Suomi-NPP and NOAA-20, as viewed using RealEarth (below).

VIIRS True Color RGB images from Suomi-NPP and NOAA-20 [clck to enlarge]

This blog post discusses AMRC/AWS staff viewing the partial eclipse from Antarctica’s McMurdo Station.

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Himawari-8 True Color RGB images [click to play animation | MP4]

JMA Hmawari-8 True Color RGB images created using Geo2Grid (above) showed the southwestward-moving volcanic cloud associated with an eruption of Semeru –located at the center of the images — in East Java around 0750 UTC on 04 December 2021. Due to the high water and ice loading within upper portions of the volcanic cloud, no distinct lower-to-middle-altitude volcanic ash signature was seen. The eruption was responsible for over 40 fatalities and the destruction of over 5000 homes; 

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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.

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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