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1-minute Mesoscale Domain Sector GOES-19 (GOES-East) Water Vapor and Visible images (above) included plots of Pilot Reports (PIREPs) of Moderate to occasionally Severe turbulence — several of which were in the vicinity of mountain waves over parts of eastern Colorado on 05 January 2026. It was notable that in the area where mountain... Read More
1-minute GOES-19 Water Vapor images (6.9 µm, left) and Visible images (0.64 µm, right) with plots of Pilot Reports of turbulence, from 1811-2310 UTC on 05 January [click to play MP4 animation]
1-minute Mesoscale Domain Sector GOES-19 (GOES-East) Water Vapor and Visible images (above) included plots of Pilot Reports (PIREPs) of Moderate to occasionally Severe turbulence — several of which were in the vicinity of mountain waves over parts of eastern Colorado on 05 January 2026. It was notable that in the area where mountain waves were very apparent in Water Vapor images (immediately downwind of the high terrain of the Rocky Mountains), there were no clouds seen in the corresponding Visible images.
Cursor samples of 2 PIREPs of Moderate to Severe turbulence are shown below. In the immediate vicinity of the earlier 1939 UTC PIREP, the distinct signature of mountain waves — adjacent bands of warm/dry subsiding air (shades of yellow) and cool/moist rising air (shades of blue) — was evident in the Water Vapor image.
GOES-19 Water Vapor image (6.9 µm, left) and Visible image (0.64 µm, right) at 1939 UTC on 05 January, with a cursor sample of a PIREP of Moderate to Severe turbulence between the altitudes of 12500-13500 ft [click to enlarge]
GOES-19 Water Vapor image (6.9 µm, left) and Visible image (0.64 µm, right) at 2310 UTC on 05 January, with a cursor sample of a PIREP of Moderate to Severe turbulence at an altitude of 11000 ft [click to enlarge]
A common sight on calm nights and early mornings is radiation fog: as the surface cools at night, the air above the ground cools as well. The absolute moisture content of the air remains the same, but since the temperature is dropping less water vapor can be contained in equilibrium... Read More
A common sight on calm nights and early mornings is radiation fog: as the surface cools at night, the air above the ground cools as well. The absolute moisture content of the air remains the same, but since the temperature is dropping less water vapor can be contained in equilibrium and thus the relative humidity goes up. If the temperature cools enough, it will reach the dew point and fog will form.
But what happens when you throw a dense city into the mix? Cities are warmer than the surrounding land for a number of reasons. First and foremost, the building materials like concrete and asphalt that are prevalent in cities are better at absorbing the sun’s energy than vegetation is. The vertical dimension of cities also matters: the perpendicular surfaces of tall buildings strongly absorb the sun’s rays when the sun is low in the sky and the rest of the landscape is absorbing very little, and the infrared radiation that is emitted outward by one building is often absorbed by a different building right next door. Thus, cities retain their heat at night in a phenomenon known as the urban heat island, or UHI.
On the morning of 5 January 2026, widespread areas of radiation fog were visible over the southeastern continental United States, as large scale nocturnal cooling took place over the Carolinas and Georgia. This can be seen in the Day Cloud Phase Distinction RGB from the GOES-19 geostationary satellite as large regions of cyan clouds. Note how the clouds seem to follow terrain, which is expected for fogs. This particular loop spans the period from before to after sunrise, and (as one can guess from the name) the Day Cloud Phase Distinction product is a daytime only product, so it really only the end of the loop that can be interpreted in this way.
However, something interesting happens when you zoom in on Atlanta, Georgia. While the population of the city of Atlanta proper is relatively small (fewer than 500,000 people), it is the heart of the nation’s 8th largest metropolitan area, ranking it ahead of the Philadelphia, Phoenix, or Boston metros. With so much development, it has a well-pronounced UHI. Let’s look at the same product, zoomed into the Atlanta metro. This map shows the Interstate highways, and the center of the image where the highways all converge is the heart of Atlanta.
Note the gap in the fog right in the heart of the city. This is because the urban heat island kept the temperature of the central core of the city from cooling enough to allow fog to form. In the regions further out, however, the UHI was weaker. Out there, the air cooled more and condensation was able to take place. Sometimes, if you want to avoid the fog, all you have to do is head downtown.
10-minute Full Disk scan GOES-19 (GOES-East) True Color RGB images along with the Aerosol Optical Depth derived product from the CSPP GeoSphere site (above) showed a pulse of blowing dust that was moving northward and westward across the northern Patagonia region of Argentina on 01 January 2026.Surface analyses (below) depicted a cold front that was... Read More
10-minute GOES-19 True Color RGB images (left) and Aerosol Optical Depth derived product (right), from 1500-2300 UTC on 01 January 2026 [click to play MP4 animation]
10-minute Full Disk scan GOES-19 (GOES-East) True Color RGB images along with the Aerosol Optical Depth derived product from the CSPP GeoSphere site (above) showed a pulse of blowing dust that was moving northward and westward across the northern Patagonia region of Argentina on 01 January 2026.
Surface analyses (below) depicted a cold front that was moving northward across that area during the day — a narrow cloud band denoted part of the leading edge of this cold front. The circulation around a compact area of high pressure that developed along the coast (south of the cold front, at 0000 UTC) acted to transport some of the blowing dust farther inland (westward).
Surface analyses at 1200 UTC on 01 January and 0000 UTC on 02 January [click to enlarge]
Continuing in the tradition of a blog post looking back on some of the most noteworthy events of the year as seen by GOES, here is a summary of 2025 CIMSS Satellite Blog posts. In previous years, a selection of several GOES ABI loops during 2022 and 2023 and 2024 showcased the diverse range of features observed,... Read More
The goal here is to show a variety of phenomena and locations that NOAA‘s GOES ABI routinely monitors. Just one highlight per month (most months, sometimes it’s hard to choose just one) and we’re covering a lot of types of events, some of which were tragic, deadly, and/or costly. Most loops generated are from the University of Wisconsin-Madison CIMSS Satellite Blog, and the original blog posts are linked if you’re interested in reading more on any of these cases. Imagery from GOES-16, -18, and -19 are showcased, along with the ABI‘s three different scan sectors: Full Disk (10-min intervals), Contiguous U.S. (5-min intervals) and Mesoscale Sectors (typically 1-min intervals). The GOES-R Series has more than an Imager instrument on it though, and we’ll include some Solar Ultraviolet Imager (SUVI) and Geostationary Lightning Mapper (GLM) data as well.
First we can celebrate 2025 with some Full Disk animations from GOES-East using the CIMSS Natural True Color RGB. We will start with the sunset view from GOES-East, from Winter Solstice 2024 (Dec 21, 2024) to Winter Solstice 2025 (Dec 21, 2025). Winter Solstice in the northern hemisphere is when the north pole reaches its maximum tilt away from the sun. Sunset for GOES-East (at the location on Earth directly below the satellite, roughly at the equator and 75W) is around 23 UTC. The exact time of sunset varies somewhat through the year, but we just chose the nominal 2300 UTC image for each day to make things simpler. And a handful of days are missing, because of bad data.
GOES-East Winter Solstice 2024 to Winter Solstice 2025 satellite sunset animation (mp4, click to play).
Next is satellite noon in CIMSS Natural True Color RGB from GOES-East for all of 2025 (minus a handful of days with bad data). Noon for GOES-East is around 1700 UTC.
GOES-East satellite noon animation for all of 2025 (mp4, click to play).
5-minute GOES-16 Red Visible (0.64 µm, left) and Clean Infrared Window (10.3 µm, right) images, with/without an overlay of GLM Flash Extent Density, from 2031-2221 UTC on 24 February 2025 [click to play MP4 animation]
1-minute daytime GOES-19 True Color RGB images + nighttime Dust RGB images, from 2130 UTC on 16 May to 0200 UTC on 17 May 2025.
June
In recent years we have seen more interest in the media as some part of the United States sees air quality impacts from wildfire smoke coming from Canada, and 2025 was no exception. One example from June 11th was Canadian wildfire smoke over Alaska:
10-minute GOES-18 True Color RGB images (top) and Near-Infrared “Cirrus” (1.37 µm) images (bottom), from 1200 UTC on 11 June to 0500 UTC on 12 June 2025.
5-minute GOES-19 Infrared (10.3 µm) images centered on Kerr County, Texas from 0001-1801 UTC on 04 July, with plots of Flood Advisories (green polygons), Flood Warnings (brighter/solid green polygons) and Flash Flood Warnings (red polygons) against County outlines — along with plots of 15-minute METAR surface report.
GOES-18 SUVI Fe171 (171 Å) images, from 0652-1000 UTC on 07 September [click to play MP4 animation]
October
This year we celebrated the 50th Anniversary of the launch of GOES-1 on October 16th, 1975 with this special look at a GOES animation from each of all 50 states: Fifty Loops for the 50th Anniversary of GOES
1-minute CIMSS True Color RGB images, from 1131-2159 UTC on 28 October 2025.
November
In addition to being the 50th anniversary of the launch of GOES-1, 2025 was also the 50th anniversary of the sinking of the Edmund Fitzgerald. This is one of the most well-remembered weather-related disasters in US history, and we take a fresh look at this storm from November 10th, 1975 with modern reanalysis data and modern tools. We don’t have any GOES imagery of this storm in our possession, but we have the next best thing: Synchronous Meteorological Satellite (SMS)-2. The SMS series was an experimental series of satellites that NASA launched and operated until SMS-C became GOES-1. SMS-1, -2 and GOES-1 through -4 are all the same design.
A portion of the SMS-2 full disk infrared image at 0615 UTC (12:15 AM CST) on November 10, 1975.
With the two operational GOES, we can see over half the surface of the earth, from the west coast of the African continent to the east coast of Australia, and not quite to the north and south poles. American forecasters have responsibility across a large portion of that area, and to highlight that here is a case from November 20th of flash flooding in American Samoa — where they don’t have a radar, so satellite observations are critical. (Incidentally, there were a least 4 times in 2025 when a 1-minute Mesoscale Sector was positioned over American Samoa to monitor flash flooding.)
GOES-18 Day Convection RGB from 16:11 to 18:01 UTC on November 20, 2025.
December
For the last month of the year we will highlight two events. Both of these events have gone on longer than maybe one would want or expect. There was been a long-duration Tule fog event in the Central Valley of California that started on November 21st and continued for over a month. Meanwhile Mt Kilauea in Hawaii has been erupting since December 23 of last year!
10-minute GOES-18 daytime True Color RGB and Nighttime Microphysics RGB images, from 1000 UTC on 21 November to 0000 UTC on 20 December 2025.
5-minute GOES-18 Shortwave Infrared (3.9 µm) images, from 1601 UTC on 06 December to 0701 UTC on 07 December 2025 [click to play MP4 animation]
Thank You!
To close out 2025, we would like to say thank you to all of our readers! The author would like to say a special thank you to the authors of the blog posts that he borrowed imagery from today: Scott Bachmeier, Scott Lindstrom, Tim Schmit, and Tim Wagner. Thanks to all who make the GOES imagery possible, the ingest and software to display the imagery (including, but not limited to McIDAS-X, Geo2Grid, GeoSphere, RealEarth and AWIPS). Special thanks to Dave Stettner of the UW/CIMSS AWG Imagery Team.
Special note: Scott Lindstrom has retired from UW-Madison and we will miss him, especially here on the Blog!