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When True Color Is False

One of the most popular GOES products is the True Color RGB. There’s a lot to like about it: a constantly updating full color view of the planet, watching clouds swirl above sapphire seas and emerald forests. It can be positively mesmerizing to watch loops of this product, at least... Read More

One of the most popular GOES products is the True Color RGB. There’s a lot to like about it: a constantly updating full color view of the planet, watching clouds swirl above sapphire seas and emerald forests. It can be positively mesmerizing to watch loops of this product, at least until the sun sets, the terminator arrives, and the visible reflectances go away.

There is an important cacceat to remember, though. The GOES true color product isn’t really a true color image of the planet. The GOES ABI instrument is not like a consumer digital camera, in which separate channels record the red, blue, and green reflectance and assemble those into an easily recognizable photograph. Instead, while ABI has a blue channel (Channel 1, 0.47 microns) and a red channel (Channel 2, 0.64 microns), it doesn’t have a green channel. Instead, ground processing does a little trickery. Channel 3, at 0.86 microns, is very sensitive to vegetation. What we can do instead is create an RGB product where red is red, blue is (wait for it…) blue, and green is a channel that is strongly representative of surfaces that are green. Most of the time this works just fine for the majority of users.

However, this all relies on the assumption that vegetation is green. But what happens if you have a lot of vegetation that isn’t green at all? How would that appear on the GOES True Color RGB? This image, taken on 17 November 2025, shows the southeastern United States as seen from GOES-19. Note how lush the forests in this region look. There’s lots of green throughout the region. If you were looking to identify where fall colors weer at their peak, it might be challenging to do so with this image.

VIIRS tells a different story. This image, obtained via direct broadcast, was taken at approximately the same time from the NOAA-21 satellite. The VIIRS instrument has true red, green, and blue channels, so a true color RGB is much closer to what our eyes would perceive if we were looking down from space. Note how the green areas of this image are much smaller in extent. Florida, southern Alabama, and the coastal regions of Georgia and South Carolina still retain much of their verdant colors as before. However, the hardwood forests of Appalachia, including the dense forests along the Tennessee / North Carolina border, are much browner than before.

The following slider allows you to directly compare the two images to see how they differ. Check out how the colors along the coasts, where trees are still green, are mostly the same between the two images, but they are very different in the forested regions where leaves have already turned.

This slider also does a good job of illustrating parallax and how cloud height exacerbates it. As you slide the bar back and forth, note that there’s very small displacements in the positions of the low clouds, like the popcorn convection throughout the Florida peninsula. However, the high cirrus (likely aged contrails) over Georgia and Alabama show a much greater horizontal displacement due to the very different scanning positions of the two instruments.

This simple example shows that it’s important to remember that the GOES ABI True Color product is really representing an idealized version of what we think the planet is supposed to look like, rather than a direct capture of what it actually looks like right now. Note that this is not as much of an issue with many other geostationary satellites. The Flexible Combined Imager (FCI) on EUMETSAT’s Meteosat-12, the Advanced Himawari Imager (AHI) on the Himawari series operated by Japan, and the Advanced Meteorological Imager (AMI) on South Korea’s GEOKOMPSAT-2a all have the necessary channels to produce full spectrum true color images. Note that this is not true for SEVIRI, still in operational use over the Indian Ocean on Meteosat-9 and in wide use in central and eastern Asia. EUMETSAT’s Natural Color RGB is a combination of 1.6 (red), 0.8 (green), and 0.6 (blue), which has even fewer visible channels than the GOES True Color.

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Pyrocumulonimbus clouds in Western Australia

10-minute Full Disk scan JMA Himawari-8 Visible, Shortwave Infrared and Infrared Window images (above) showed 2 pulses of pyrocumulonimbus (pyroCb) clouds that were spawned by a large bushfire in Western Australia on 17 November 2025. The pyroCb cloud pulses exhibited a cloud-top 10.4 µm infrared brightness temperature (IRBT) of -40ºC... Read More

10-minute Himawari-8 “Red” Visible (0.64 µm, left), Shortwave Infrared (3.9 µm, middle) and “Clean” Infrared Window (10.4 µm, right) images, from 0400-0800 UTC on 17 November [click to play animated GIF]

10-minute Full Disk scan JMA Himawari-8 Visible, Shortwave Infrared and Infrared Window images (above) showed 2 pulses of pyrocumulonimbus (pyroCb) clouds that were spawned by a large bushfire in Western Australia on 17 November 2025. The pyroCb cloud pulses exhibited a cloud-top 10.4 µm infrared brightness temperature (IRBT) of -40ºC or colder (denoted by darker blue pixels) — a necessary condition to be classified as a pyroCb (since that temperature assures that heterogeneous glaciation has occurred at the cloud top). Note that the pyroCb cloud tops appeared as darker shades of gray in the Shortwave Infrared images, due to enhanced solar reflection off the smaller smoky ice crystals.

Himawari-8 Fire Temperature RGB + Infrared Window images viewed using RealEarth (below) indicated that the large bushfire was burning near the Zyotdorp Nature Reserve.

10-minute Himawari-8 Fire Temperature RGB + Infrared Window images, from 0400-0800 UTC on 17 November [click to play MP4 animation]

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Satellite signatures of the EUMETSAT Sentinel-6B launch

The EUMETSAT Sentinel-6B satellite was launched from Vandenberg Space Force Center in California at 0521 UTC on 17 November 2025 (9:21 PM Pacific Time on 16 November). A 1-minute multi-panel display of all 16 ABI spectral bands on the GOES-18 (GOES-West) satellite (above) showed that a thermal signature of the Falcon... Read More

Multi-panel display of all 16 ABI spectral bands on GOES-18, from 0521-0524 UTC on 17 November [click to play MP4 animation]

The EUMETSAT Sentinel-6B satellite was launched from Vandenberg Space Force Center in California at 0521 UTC on 17 November 2025 (9:21 PM Pacific Time on 16 November). A 1-minute multi-panel display of all 16 ABI spectral bands on the GOES-18 (GOES-West) satellite (above) showed that a thermal signature of the Falcon 9 rocket booster was evident in many of the spectral bands — particularly the Near-Infrared bands 03/04/05/06 and Infrared bands 07/08/09/10 and 16. However, subtle thermal signatures could be seen in the other Infrared spectral bands as well.

In addition, a signature of the glaciated rocket condensation cloud (darker blue pixels) was seen in Nighttime Microphysics RGB images (below) as it drifted eastward away from the launch site.

1-minute GOES-18 Nighttime Microphysics RGB images, from 0521-0536 UTC on 17 November [click to play MP4 animation]

A plot of 0000 UTC rawinsonde data from Vandenberg (below) showed the presence of westerly winds throughout the depth of the troposphere, which were responsible for the eastward drift of the rocket booster condensation cloud.

Plot of rawinsonde data from Vandenberg Space Force Base, California at 0000 UTC on 17 November [click to enlarge]

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Satellite signatures of the Blue Origin New Glenn NG-2 launch

The Blue Origin New Glenn NG-2 mission launched from Cape Canaveral Space Force Station, Florida at 2055 UTC on 13 November 2025. A multi-panel display showing all 16 ABI spectral bands on the GOES-19 (GOES-East) satellite (above) revealed distinct thermal signatures in the 3 Water Vapor bands (08/09/10) at 2056 UTC, with... Read More

Multi-panel display showing all 16 ABI spectral bands of GOES-19, from 2051-2106 UTC on 13 November; KXMR denoted the Cocoa Beach rawinsonde site [click to play MP4 animation]

The Blue Origin New Glenn NG-2 mission launched from Cape Canaveral Space Force Station, Florida at 2055 UTC on 13 November 2025. A multi-panel display showing all 16 ABI spectral bands on the GOES-19 (GOES-East) satellite (above) revealed distinct thermal signatures in the 3 Water Vapor bands (08/09/10) at 2056 UTC, with a more subtle signature in the CO2 band (16) and one faintly-brighter pixel in the Cirrus band (04). A signature of the rocket booster condensation cloud was evident in all 16 ABI spectral bands, closer to the coast. Unfortunately, there was no 1-minute GOES-19 Mesoscale Domain Sector coverage over that area — so only 5-minute CONUS Sector imagery was available.

A slightly longer sequence of GOES-19 True Color RGB images (below) highlighted the rapid dissipation of the rocket booster condensation cloud as it drifted eastward away from the launch site. Farther inland, the dense smoke plume from a prescribed burn is apparent.

GOES-19 True Color RGB images, from 2051-2126 UTC on 13 November [click to play MP4 animation]

A plot of rawinsonde data from Cocoa Beach, Florida (KXMR) during the morning preceding the launch (below) showed dry air aloft throughout much of the troposphere — which contributed to the fairly rapid dissipation of the rocket booster’s condensation cloud as it drifted away from the coast.

Plot of rawinsonde data from Cocoa Beach, Florida (KXMR) at 1100 UTC on 13 November [click to enlarge]

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