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Lake effect cloud plume produces light snow downwind of the Great Salt Lake

5-minute CONUS Sector GOES-18 (GOES-West) and GOES-19 (GOES-East) Nighttime Microphysics RGB + daytime True Color RGB images from the CSPP GeoSphere site (above) showed a lake effect cloud plume that developed over the southern half of Great Salt Lake on 17 April 2026 — which produced a swath of light snowfall downwind (southeast) of the lake... Read More

5-minute GOES-18 (left) and GOES-19 (right) Nighttime Microphysics RGB + daytime True Color RGB images, from 0401-1556 UTC on 17 April [click to play MP4 animation]

5-minute CONUS Sector GOES-18 (GOES-West) and GOES-19 (GOES-East) Nighttime Microphysics RGB + daytime True Color RGB images from the CSPP GeoSphere site (above) showed a lake effect cloud plume that developed over the southern half of Great Salt Lake on 17 April 2026 — which produced a swath of light snowfall downwind (southeast) of the lake that was apparent in True Color RGB images after sunrise.

Day Snow-Fog RGB images from GOES-18 and GOES-19 created using Geo2Grid (below) were helpful in discriminating between the lake effect clouds (shades of white) and the fresh snow cover (shades of red) immediately downwind of the Great Salt Lake after sunrise. Bare ground appeared as shades of green.

5-minute Day Snow-Fog RGB images from GOES-18 (left) and GOES-19 (right), from 1331-1801 UTC on 17 April [click to play MP4 animation]

A plot of the 24-hour total observed snowfall (below) indicated that amounts were generally 1 inch or less at lower-elevation sites downwind of the Great Salt Lake (with 2 sites near topographical features reporting 3.0 inches).

Plot of 24-hour total observed snowfall ending at 1200 UTC on 17 April [click to enlarge]

Plot of 24-hour total observed snowfall ending at 1200 UTC on 17 April [click to enlarge]

GOES-18 Infrared images (below) depicted cloud-top infrared brightness temperatures within the lake effect cloud plume that were as cold as -35ºC. Note that Salt Lake City International Airport (KSLC) was reporting light snow which reduced the surface visibility to 8 miles at 0454 UTC, as the lake effect cloud was moving over that location.

5-minute GOES-18 Infrared images, from 0401-1201 UTC on 17 April [click to play MP4 animation]

5-minute GOES-18 Infrared images, from 0401-1201 UTC on 17 April [click to play MP4 animation]

According to a plot of 0000 UTC rawinsonde data from Salt Lake City (below), an air temperature of -35ºC occurred at an elevation of 5900 m (19358 ft). Since the water temperature of the lake was around 50ºF or 10ºC that day, the surface temperature of the sounding was modified to match that value.

Plot of rawinsonde data from Salt Lake City at 0000 UTC on 17 April [click to enlarge]

Surface-temperature-modified plot of rawinsonde data from Salt Lake City at 0000 UTC on 17 April [click to enlarge]

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Lightning-related fatality in Wisconsin

1-minute Mesoscale Domain Sector GOES-19 (GOES-East) Infrared images (above) included plots of 1-minute GLM Flash Points (which are parallax-corrected to correspond to their surface locations) — and showed an increase in thunderstorm coverage and lightning activity across southeastern Wisconsin late in the day on 15 April 2026.Unfortunately, one lightning-related fatality occurred south of... Read More

1-minute GOES-19 Infrared images, with plots of GLM Flash Points (white dots), from 2301 UTC on 15 April to 0100 UTC on 16 April [click to play MP4 animation]

1-minute GOES-19 Infrared (10.3 µm) images with plots of GLM Flash Points (white dots) and METAR surface reports (cyan), from 2301 UTC on 15 April to 0100 UTC on 16 April [click to play MP4 animation]

1-minute Mesoscale Domain Sector GOES-19 (GOES-East) Infrared images (above) included plots of 1-minute GLM Flash Points (which are parallax-corrected to correspond to their surface locations) — and showed an increase in thunderstorm coverage and lightning activity across southeastern Wisconsin late in the day on 15 April 2026.

Unfortunately, one lightning-related fatality occurred south of Pewaukee, Wisconsin around 0043 UTC or 7:43 PM Central Time (Local Storm Report). A cursor sample of a GLM Flash Point just southeast of Pewaukee (below) revealed a rather large flash area of 1114 km2 at 0041 UTC (7:41 PM Central Time).

GOES-19 Infrared image at 0041 UTC on 16 April, with a cursor sample of a GLM Flash Point near Pewaukee, Wisconsin [click to enlarge]

GOES-19 Infrared (10.3 µm) image at 0041 UTC on 16 April, with a cursor sample of a GLM Flash Point (white dot) near Pewaukee, Wisconsin [click to enlarge]

1-minute GOES-19 Infrared images with contours of ProbSevere LightningCast probability (below) indicated that the LightningCast probability over Pewaukee was consistently at or above 90% beginning at 0015 UTC.

1-minute GOES-19 Infrared images, with an overlay of LightningCast probability contours, from 2340 UTC on 15 April to 0100 UTC on 16 April [click to play MP4 animation]

1-minute GOES-19 Infrared (10.3 µm) images, with an overlay of LightningCast probability contours, from 2340 UTC on 15 April to 0100 UTC on 16 April [click to play MP4 animation]

A plot of LightningCast Probability and GOES-19 GLM Flash Count (below) revealed that the LightningCast Probability was 73% or higher during the 30-minute period preceding a marked increase in GLM Flash Count in the vicinity of Waukesha County Airport (KUES, which is located about 3 miles south of Pewaukee).

Plot of LightningCast Probability and GOES-19 GLM Flash Count in the vicinity of Waukesha Airport (KUES) [click to enlarge]

Plot of LightningCast Probability and GOES-19 GLM Flash Count in the vicinity of Waukesha Airport (KUES) [click to enlarge]

This is the first lightning fatality of 2026. Details are scarce right now.The safest place to be during a thunderstorm is in a substantial building with electrical and plumbing in the walls. Fully enclosed metal vehicles also provide protection.When thunder roars, go indoors!

National Lightning Safety Council (@lightningsafety.bsky.social) 2026-04-16T13:25:15.423Z

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Severe thunderstorms produce tornadoes, large hail and damaging winds across southern Wisconsin

1-minute Mesoscale Domain Sector GOES-19 (GOES-East) Visible images (above) included time-matched (+/- 3 minutes) plots of SPC Storm Reports — which showed the tornadoes, large hail (up to 4.00″ in diameter) and damaging winds (as high as 88 mph) that occurred across much of southern Wisconsin (along with adjacent parts of far northeast Iowa and far... Read More

1-minute GOES-19 Visible (0.64 µm) images with time-matched (+/- 3 minutes) plots of SPC Storm Reports, from 2030 UTC on 14 April to 0015 UTC on 15 April [click to play animated GIF | MP4]

1-minute Mesoscale Domain Sector GOES-19 (GOES-East) Visible images (above) included time-matched (+/- 3 minutes) plots of SPC Storm Reports — which showed the tornadoes, large hail (up to 4.00″ in diameter) and damaging winds (as high as 88 mph) that occurred across much of southern Wisconsin (along with adjacent parts of far northeast Iowa and far southeast Minnesota) on 14 April 2026. Numerous overshooting tops were seen in the Visible images.

The corresponding 1-minute GOES-19 Infrared images (below) revealed pronounced enhanced-V cloud-top signatures with several of the severe thunderstorms.

1-minute GOES-19 Infrared (10.3 µm) images with time-matched (+/- 3 minutes) plots of SPC Storm Reports, from 2030 UTC on 14 April to 0031 UTC on 15 April [click to play animated GIF | MP4]

The coldest cloud-top infrared brightness temperatures exhibited by pulses of overshooting tops were -78ºC (brighter white pixels embedded within dark black areas) — which corresponded to a significant (~2 km) overshoot of the Most Unstable (MU) air parcel’s Equilibrium Level (EL), according to plots of rawinsonde data from Davenport, Iowa (below). CAPE values of 4000-4300 J/kg indicated that significant instability was present south of a frontal boundary which was draped across Iowa, Wisconsin and lower Michigan.

Plots of rawinsonde data from Davenport, Iowa at 1800 UTC and 2100 UTC on 14 April [click to enlarge]

Plots of rawinsonde data from Davenport, Iowa at 1800 UTC and 2100 UTC on 14 April [click to enlarge]

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Typhoon Sinlaku makes landfall on Saipan and Tinian in the Mariana Islands

2.5-minute Target Sector JMA Himawari-9 AHI Visible images (above) showed Super Typhoon Sinlaku as its eye approached Saipan (station identifier PGSN) in the Mariana Islands on 13-14 April 2026. Mesovrticies were evident within the eye. After reaching its peak intensity on 12 April (blog post 1 | blog  post 2), Sinlaku was in the... Read More

2.5-minute Himawari-9 Visible (0.64 µm) images, from 2032 UTC on 13 April to 0802 UTC on 14 April [click to play animated GIF]

2.5-minute Target Sector JMA Himawari-9 AHI Visible images (above) showed Super Typhoon Sinlaku as its eye approached Saipan (station identifier PGSN) in the Mariana Islands on 13-14 April 2026. Mesovrticies were evident within the eye. After reaching its peak intensity on 12 April (blog post 1 | blog  post 2), Sinlaku was in the process of a gradual weakening trend, decreasing from Category 5 intensity to Category 4 intensity by 0000 UTC on 14 April (JTWC discussion).

A longer animation of Himawari-9 Infrared images (below) showed Sinlaku making landfall on the islands of Saipan and Tinian, as a Category 4 storm around 1432 UTC on 14 April.

2.5-minute Himawari-9 Infrared (10.4 µm) images, from 2032 UTC on 13 April to 1519 UTC on 14 April [click to play animated GIF]

Microwave imagery (source) from ATMS (below) displayed the large outer eyewall ring that remained after Sinlaku had undergone a recent eyewall replacement cycle. The islands of Saipan and Tinian were located within this large eyewall.

ATMS Microwave (183 GHz) image at 1559 UTC on 14 April

ATMS Microwave (183 GHz) image at 1559 UTC on 14 April

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