CIMSS research scientist Rich Dworak sent along a sequence of NOAA-20 VIIRS Day/Night Band images (above) that included satellite-derived Atmospheric Motion Vectors — which depicted an anomalously deep polar low just north of Greenland during the 25-26 May 2026 period.

Another feature of interest seen in the Day/Night Band imagery was the breakup of ice in the northeastern portion of Baffin Bay — which was also evident in a Blended Ice Concentration product from the VIIRS Enterprise Ice Products site (below). The ice-free North Water Polynya was also very apparent.

According to products from the Canadian Ice Service on 25 May (below), the Ice Concentration was only 1/10th to 3/10ths across much of the northern part of Baffin Bay, with large areas of <1/10th ice concentration (having an Ice Stage classification of Icebergs) within the North Water Polynya.

The Ice Concentration Departure From Normal was substantially negative (shades of red) in northern and northeastern/eastern portions of Baffin Bay (below).

View only this post Read Less

10-minute Full Disk scan Visible, Shortwave Infrared and Infrared Window images from GOES-18 (GOES-West) and GOES-16 (above) showed a wildfire in Canada’s Northwest Territories that produced multiple pulses of pyrocumulonimbus (pyroCb) clouds late in the day on 23 May 2026. Each of the pyroCb clouds exhibited slightly warmer signatures (darker shades of gray) in the Shortwave Infrared images, due to enhanced solar reflection off the smaller smoke-filled ice crystals of their anvil tops — in addition to cold Infrared Window brightness temperatures in the -50s C (shades of red).

In a comparison of Day Land Cloud Fire RGB images from the 2 satellites — created using Geo2Grid (below), the wildfire’s thermal signature (shades of pink to red) was often obscured from the far western view of GOES-18 by pyro-convection; however, during many of those instances the thermal signature could be seen in GOES-16 imagery (since that satellite was positioned farther to the east, at 104.7 W longitude, during its annual test period).

View only this post Read Less

The SpaceX Starship Flight Test 12 was launched from the Starbase facility at 2230 UTC on 22 May 2026 — and 5-minute CONUS Sector GOES-16 and GOES-19 (GOES-East) True Color RGB images created using Geo2Grid (above) showed the Super Heavy rocket booster condensation cloud as it drifted away from the South Texas coast and eastward across the Gulf of Mexico. Enhanced forward scattering from the GOES-19 satellite perspective led to a more hazy appearance of those images (GOES-16, positioned more closely overhead at 104.7 W longitude during its annual test period, was therefore not as affected by forward scattering at that time of day).

GOES-16 Rocket Plume RGB imagery (below) captured a vivid high-altitude signature of the trail of superheated water vapor (shades of yellow to lime green in the 2231 UTC image) in the wake of the Super Heavy rocket booster shortly after launch. The eastward drift of the lower-altitude rocket booster condensation cloud (darker shades of reddish-brown) was also apparent.

A toggle between the 2231 UTC GOES-16 Rocket Plume RGB and True Color RGB images (below) revealed that there was no corresponding signature of the high-altitude superheated water vapor trail in the True Color image — but a signature of the lower-altitude rocket booster condensation cloud appeared in both images, immediately off the coast. During the 22:31:19 UTC CONUS Sector image, GOES-16 was actually scanning the area of the rocket plume at 22:32:23 UTC — when the Super Heavy booster was at an altitude of around 50 km in the Stratosphere.

View only this post Read Less

NWS Pago Pago forecasters (and Friends of the Blog) Jane Allen and Brayden Barton sent along some video and pictures of a significant thunderstorm that rocked the American Samoan Island of Tutuila in the hours before sunrise on Wednesday, May 20th, 2026. First, here is a video showing the intensity of the rainfall. Keep an eye on the palm trees and note how the wind direction practically reverses itself about midway through at 23 seconds in.

Winds were significant enough to cause noticeable amounts of damage as can be seen by the pictures in the following photo gallery.

This storm was characterized by rapid upscaling as it moved southward. To gain a perspective on how this storm developed, let’s start by looking at the environment in those early morning hours. First up, here’s the seat surface temperature (SST) as captured by NESDIS’s blended geostationary/polar orbiter SST product as displayed in SSEC Real Earth. From this, we can see that the SSTs surrounding the Samoan islands are around 26 C, or close to 79 F. This is slightly warmer than the ambient air temperature at the time as recorded at the Pago Pago airport, which was at 78 F.

There was also a 1200 UTC radiosonde launched from the Pago Pago forecast office (as plotted by NOAA’s SPC). The sounding shows modest levels of instability for the tropics and a moderate amount of speed shear but little directional shear. The presence of some shear is critical for deep moist convection to develop in the tropics as otherwise a storm will rain in its updraft and kill it off shortly after initiating.

With that background in place, let’s check out the satellite perspective of this event. Since it’s night, the GOES-18 Band 13 (10.3 micron) infrared window channel is an excellent place to start. This first loop covers from 1300 to 1500 UTC (1:00 AM to 3:00 AM local time), covering the initiation and first growth of this storm. The brightness temperatures drop from -20 C to -70 C in a little over an hour, showing significant convective growth.

At the same time as this geostationary loop, the polar-orbiting NOAA-20 passed overhead which gives us the opportunity to see a NUCAPS sounding from Tutuila. There is remarkably good agreement in the mixed layer and most unstable CAPEs between this profile and the radiosonde an hour earlier, which helps us have some confidence in the values retrieved from the satellite. Of particular interest is the 1168 J/kg downward CAPE (DCAPE). This is a quite high value for this parameter, which quantifies the negative buoyancy of descending parcels in a downdraft. Higher values of DCAPE means downdraft parcels are bringing more kinetic energy to the surface, and when those parcels hit the ground it results in faster outflow winds.

The NUCAPS sounding shows a total precpitable water (TPW) value of 1.87 inches. Of course, there are other satellite-based measures of TPW. One of the most popular among forecasters is the CIMSS MIMIC-TPW2 product. Here’s a view of that product at 1300 UTC, where the Samoan islands appear to have a TPW around 2.0 to 2.2 inches. Regardless of the method you use, the TPW is quite high.

Given high SSTs, moderate amounts of instability, enough shear to prevent updraft contamination by rainfall, and a high tropopause, we can expect some deep convection. We can use the Community Satellite Processing Package (CSPP) Level 2 products as displayed on CSPP Geosphere to gain an understanding of just how tall these clouds are becoming. The following video shows the CSPP-derived cloud top heights from 1300 UTC to 1600 UTC (2:00 AM to 5:00 AM). As these clouds develop, they grow to a height exceeding 15000 m (that’s over 42,000 feet!). That’s consistent with the soundings which show a tropopause somewhere between 100 and 150 hPa.

One of the blessings of this storm is that it was pretty quick moving, which limited the total damage it could cause. Tutuila is only about 20 miles across at its maximum width, and from the direction the storms were coming from, it’s only seven miles from one side of the island to the other. Here’s a slowed down and zoomed in view of Band 13 from 1530 to 1730 UTC (4:30 AM to 6:30 AM local time)showing the storm as it traverses the island. Remember, American Samoa lies well outside of the CONUS scan for GOES-18, so in the absence of a mesoscale sector scan, the temporal resolution will only be 10 minutes. The deepest updrafts are over the island for only a few scans, so the worst of the storm only lasted 30 minutes or so. There may be some evidence of cell splitting given the separation of the overshooting tops, though in the absence of a radar to see beneath the anvils it’s hard to say for sure.

The CMORPH2 product is a satellite-based assessment of rain accumulation. SSEC’s Real Earth can display CMORPH precipitation estimates for a one hour, one day, or seven day accumulation period. Here’s the one day total satellite-estimated rainfall accumulation for 20 May 2026. Tutuila is somewhere between 50 and 75 mm for the day, which is basically 2-3 inches of rain.

This storm featured two characteristics that made it particularly impactful. The first was its high TPW value, which translated into significant rainfall on the ground. This could have been even worse if the storm hadn’t been so quickly moving to the southeast. The second is that it had a high DCAPE, which was responsible for strong wind gusts at the surface. Recall that video at the top of this post, with the rapid and direct shift in the wind direction? That’s a tell-tale sign of a microburst, which was likely given the strong downward instability. It’s fortunate that at this time of day there were no aircraft attempting to land at the Pago Pago International Airport, because a microburst like this is a very hazardous situation for aviation. Thanks, Jane and Brayden, for sharing your pictures and your stories!

View only this post Read Less