Mostly clear skies over the Great Lakes early in the morning on 16 June allowed the VIIRS instrument on Suomi-NPP an unobstructed view of the surface waters.  Advanced Clear-Sky Processing for Oceans (ACSPO) Lake-surface temperatures, above, show the temperature distributions in the five lakes.  The warmest region is western Lake Erie where water temperatures are already in the 70s.  Saginaw Bay in Lake Huron (and Green Bay in Lake Michigan — although clouds at this time prevented a good view) are also in the 70s.  Much of Lake Superior remains around 40 F;  Lake Michigan is unusually warm — with a large region of 60+ — following an early-season heat wave (graph from GLERL’s Lake Statistics webpage).

Clear skies continued into the afternoon of the 16th;  the true-color image, below, derived from VIIRS data from NOAA-20 shows cloud over Lake Huron and some sun glint over Lakes Michigan and Superior. A zoomed-in view of Lake Erie (link) shows remarkable detail to the water color in the lake.

Suomi-NPP and NOAA-20 VIIRS data were downloaded at the CIMSS Direct Broadcast site and processed using CSPP software. Great Lakes SST fields and VIIRS imagery over CONUS are available via LDM feed to National Weather Service Offices. True-Color imagery can be found at VIIRS Today and at the CIMSS direct broadcast ftp site.

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True-color imagery derived from GOES-16, above, shows a low-level cyclonic circulation associated with then Tropical Depression #2 to the east of Cape Hatteras over the western Tropical Atlantic. The satellite imagery suggests strong southwesterly shear: ongoing deep and vigorous convection is far removed to the east and northeast of the near-surface circulation visible in the imagery. Indeed, a shear analysis from the CIMSS Tropical page, below, shows values in excess of 50 knots over the storm. Despite the strong shear, this depression was upgraded to Tropical Storm Bill at 0300 UTC on 15 June 2021.

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Scatterometry winds helped with the intensity determination.  The 2328 UTC 14 June overpass, below, shown in a toggle with the ABI Band 13 infrared imagery, shows the circulation with 40-knot winds on the south side.  Included in the image is the 1056 UTC 15 June image, showing the quick northeastward progress of the storm, and also showing the degradation in the storm’s symmetry.

Suomi-NPP overflew the storm at 0626 UTC on 15 June. The Day Night Band imagery, below, overlain on top of derived ACSPO SSTs and toggled with the VIIRS I05 11.45 µm window channel imagery (obtained from the Direct Broadcast site at the University of Wisconsin-Madison), show evidence of lightning northeast of the storm center. SSTs within the core of the Gulf Stream are 81 F.  The core of the storm at 0626 UTC as depicted in the infrared imagery below is far more symmetric than in either of the two times, 2326 UTC on 14 June, and 1056 UTC 15 June, in the toggle above.

Refer to the National Hurricane Center website for more information on Bill.

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GOES-16 (GOES-East) “Red” Visible (0.64 µm), Shortwave Infrared (3.9 µm), Fire Power and Fire Temperature derived products (above) showed the dark black smoke plume and thermal signature of a fire from an explosion at the Lubrizon Corporation Chemtool facility at Rockton in far northern Illinois on 14 June 2021. The thick smoke plume obscured the satellite’s view of the fire point source much of the time, preventing the continuous derivation of Fire Power and Fire Temperature products (and masking the thermal anomaly in the Shortwave Infrared images).

However, a comparison of Shortwave Infrared images from GOES-17 (GOES-West) and GOES-16 (below) revealed that the western satellite’s viewing angle allowed the thermal anomaly of the fire source (hot black-enhanced pixel) to be seen for a longer time period — even after the dark smoke plume had become well established.

GOES-16 Near-Infrared “Vegetation” (0.86 µm) images with plots of pilot reports (below) indicated that the smoke existed at altitudes of 2500 to 3000 feet, but was not restricting the surface visibility at sites that were downwind of the fire.

Closer views of GOES-16 Near-Infrared “Vegetation” images created using Geo2Grid (below) showed the southward transport of dark smoke as the fire continued to burn into the afternoon hours.

Due to the very dark character of this particular smoke plume, it showed up much better against the more reflective surface in 0.86 µm imagery (compared to 0.64 µm “Red” Visible imagery), as seen in the image toggle below.

The dark smoke plume was also evident in various GOES-16 RGB combinations, such as True Color, Day Land Cloud, and Day Snow Fog (below). True Color RGB images showed that the smoke eventually drifted over far western Indiana.

 

 

#Sentinel2 was in the perfect place and time to capture some very hires images of the #RocktonFire #ChemToolFire / explosion yesterday. You can even see some of the bright flames. @UWCIMSS @CIMSS_Satellite @NWSChicago pic.twitter.com/ENykAY4Paf

— Remy Mermelstein | WeatherInTheHud (@WeatherInTheHud) June 15, 2021

Here is a look a the radar imagery of the chemical fire in Rockton, IL. The fire started around 7:25am this morning with a rather large explosion at roughly 9:35AM, which shows up very well with some very high reflectivities. #wiwx #swiwx pic.twitter.com/tu1yaLM7eG

— NWS Milwaukee (@NWSMilwaukee) June 14, 2021

 

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Synthetic Aperture Radar (SAR) winds from RCM1 (RADARSAT Constellation Mission 1) over the south Pacific Ocean, from this site, show a gradient in wind speeds between 165 W and 168 W. Are there other ways to view this type of wind change over the open ocean?

GOES-17 Derived Motion wind vectors, below, showing 0500 UTC wind speeds between 950 and 800 mb (a different level than the near-surface winds from the SAR data), from Real Earth, below, do not clearly show the difference in winds over this same domain.

GOES-17 Shortwave infrared imagery from the same time in that region, below, shows consistent westward motion at low levels (it’s hard to distinguish from this animation if the low-level wind speeds change across the domain; the cloud motions are all similar) with eastward motion aloft (that, is: considerable shear!)

SAR winds can give information over the open ocean that is difficult to find in other places.

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