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Clear skies over the Great Lakes

A clear night over the Great Lakes — associated with a large High Pressure System, shown below in the 0600 UTC Surface Analysis — allowed a high-resolution view of Lake Surface Temperatures. There are thin filaments of colder waters hugging different coastlines: the eastern shore of Lake Michigan, the western... Read More

NOAA-20 VIIRS Day Night Band visible (0.7) imagery over the Great Lakes, 0811 UTC on 26 July 2024 (Click to enlarge)

A clear night over the Great Lakes — associated with a large High Pressure System, shown below in the 0600 UTC Surface Analysis — allowed a high-resolution view of Lake Surface Temperatures. There are thin filaments of colder waters hugging different coastlines: the eastern shore of Lake Michigan, the western shore of the Upper Peninsula of Michigan, the southern shore of Manitoulin Island in northern Lake Huron. In these regions, off-shore winds are likely causing deeper (colder) sub-surface waters to upwell. The National Weather Service in Duluth noticed a similar event on 23 July (link to Twitter/X).

Do you think those surface temperatures are warmer than normal as a whole? The purple enhancement over Lake Superior shows temperatures cooler than 60oF. Michigan and Huron show temperatures around 70oF (green) except for Saginaw Bay, where it’s in the mid-70s. Western Lake Erie is 77-78 oF; Lake Ontario is around 75oF at its warmest point. GLERL maintains line plots of basin-wide averages: Superior, Michigan, Huron, Erie and Ontario. All five lakes are warmer on 25 July than the long-term average.

Surface Analysis, 0600 UTC on 26 July 2024 (Click to enlarge)

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Typhoon Gaemi and Taiwan

Typhoon Gaemi took a very unusual path on its route to a landfall along the eastern shore of Taiwan on 24 July 2024. HImawari-9 Clean Window infrared (Band 13, 10.4 µm) target scene imagery, below, (here is a shorter animation (animated gif) animation than the mp4 below) shows the storm... Read More

Typhoon Gaemi took a very unusual path on its route to a landfall along the eastern shore of Taiwan on 24 July 2024. HImawari-9 Clean Window infrared (Band 13, 10.4 µm) target scene imagery, below, (here is a shorter animation (animated gif) animation than the mp4 below) shows the storm moving northwest, then west, then south along the east coast of Taiwan before looping into the coast and making landfall. By the end of the animation (2252 UTC on 24 July), the storm has moved off the northwest coast of Taiwan. The unusually wobbly path is also very apparent in this radar animation (courtesy Brian McNoldy (Univ of Miami))

Himawari-9 Clean Window infrared imagery (Band 13, 10.4 µm), 0929 UTC 23 July 2024 – 2252 UTC 24 July 2024 (mp4 animation)

Microwave imagery at 0923 UTC on 24 July 2024, below, taken from the SSEC Tropical Weather Website, show a well-defined eye with rainbands surrounding the storm. Shear values (850-200 mb) are also plotted on the image and are small over the storm.

Total Precipitable Water fields (source) for the 24 hours ending at 1300 UTC on 24 July 2024 show Gaemi embedded within a region of rich moisture over the Western Pacific Ocean basin. However, by the end of the animation, dryer air from Asia is starting to wrap into the southern part of the storm circulation.

Hourly estimates of Total Precipitable Water, 1400 UTC 23 July – 1300 UTC 24 July 2024 (Click to enlarge)

Gaemi’s future path takes it over mainland China.

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How Small of a Rocket Signature can GOES “see”?

There are many examples of NOAA‘s GOES ABI detecting the spectral signatures of large rockets. These include GOES-S, GOES-T, GOES-U, GOES-U boosters, Starliner, Falcon 9, Ariane, Himawari-9, Antares, etc. If the rocket is large enough, there is often a signal in each of the 16 ABI bands. Of course the timing of the ABI scan... Read More

There are many examples of NOAA‘s GOES ABI detecting the spectral signatures of large rockets. These include GOES-S, GOES-T, GOES-U, GOES-U boosters, Starliner, Falcon 9, Ariane, Himawari-9, Antares, etc. If the rocket is large enough, there is often a signal in each of the 16 ABI bands. Of course the timing of the ABI scan needs to correspond to the times of the rocket’s brightest / hottest phases, which is more likely if there’s a meso-scale sector covering the area of interest, either at 1-min or 30-second cadence.

Smaller rockets, such as the Firefly, may be be an order of magnitude darker/cooler compared to a Falcon, given their very different maximum thrust. The Firefly maximum rocket thrust is approximately 165,000 lbf (pound-force) [736.1 kN] and the Falcon 9 is about 1,700,000 lbf [7,000 kN].

Firefly on July 4th

Late on July 3rd (local time, early July 4th UTC) there was a Firefly rocket launch from Vandenberg Air Force base.

Launched at 12:04 am EDT on July 5th.

Given the smaller rocket size, a fair question is if it can be seen by the GOES ABI. Often the “Meso 1” sector from GOES-West covers most of California (the default location for this sector). This was the case on July 3, into July 4, 2024. A first look at the 16 spectral bands on the ABI, using default enhancements, shows no discernible rocket plume signature. (The signal of the explosion on the maiden Firefly rocket flight was seen by each band of the ABI.)

The 16 bands of the GOES-18 ABI with 1-min imagery on July 4, 2024. (Click to Play)

Yet, a highly-enhanced (stretched) ABI band 5 (1.61 micrometers) showed a glimpse of the rocket launch. (Some instrument noise is also seen.)

Animation of NOAA’s GOES-18 ABI highly enhanced Band 5 (1.6 micrometer) on July 4, 2024. (Click to Play)

The rocket signature is more evident in the nighttime micro-physics RGB combination. Watch near the coast for the first signature.

GOES-18 nighttime micro-physics RGB on July 4, 2024.

While it’s hard to tell, there may be some indication of the plume in the 11-12 micrometer split window difference from the CONUS sectors.

H/T

The GOES ABI data was accessed via the UW/SSEC Data Services. McIDAS-X, geo2grid and AWIPS software were used to generate the images. More UW/CIMSS Satellite Blogs associated with rocket signatures. T. Schmit works for NOAA/NESDIS/STAR and is stationed in Madison, WI.

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VIIRS [added: and GOES!] estimates of smoke over the central United States

As noted here, CSPP software now includes the ability to show reprojected values of Aerosol Optical Depth, in this case within AWIPS. The AOD from the NOAA-20 afternoon pass on 21 July shows extensive smoke over the Plains of Canada and the northern Plains of the USA. Clean air is confined to the Upper Peninsula (UP) of Michigan. The Day Night band imagery at the same time... Read More

NOAA-20 True Color imagery, Day Night band visible (0.7 µm) imagery, and Aerosol Optical Depth (AOD) on 1925 UTC, 21 July 2024 (Click to enlarge)

As noted here, CSPP software now includes the ability to show reprojected values of Aerosol Optical Depth, in this case within AWIPS. The AOD from the NOAA-20 afternoon pass on 21 July shows extensive smoke over the Plains of Canada and the northern Plains of the USA. Clean air is confined to the Upper Peninsula (UP) of Michigan. The Day Night band imagery at the same time is more distinct over the UP as well. Note, for example, how easy it is to see Lake Superior compared to Lake of the Woods on the Minnesota/Canada border, or Lake Manitoba.

AOD computation with VIIRS data requires visible bands that give no information at night (the ATBD for VIIRS AOD is here). Day Night Band imagery — with a near-full moon — gives information on smoke distribution based on, as above, how well surface features can be viewed.

NOAA-20 VIIRS Day Night Band visible (0.7 µm) imagery, 0745 and 0902 UTC on 22 July 2024 (Click to enlarge)

VIIRS data from the CIMSS Direct Broadcast site — the source of these AWIPS images — can also be viewed online here.


VIIRS AOD from the afternoon overpass on 22 July 2024, below, shows a general increase in AOD values over the midwest as the region of relatively clean air over the western Great Lakes shrinks.

VIIRS AOD from NOAA-20, 1905 UTC on 22 July 2024 (Click to enlarge)

Earth-based observations at Madison from this site show the evolution of the particulate matter from 17-22 July. There is an increase an lowering in the particulates over the course of time. In particular, a defined layer near 4 km becomes apparent by 19 July 2024.

Aerosol backscatter at Madison WI, 17-22 July 2024 (Click to enlarge)

The smoke layer is also apparent in the series of small plots shown below, starting high in the atmosphere on 18 July, and descending to around 4 km on 19 July. A lower-layer of particulates was also present on 19-21 July 2024; showers on the 21st likely removed that lower layer.

Aerosol Backscatter, 13-22 July 2024 (Click to enlarge)

GOES-R Satellites also produce the Level 2 product Aerosol Optical Depth. The animation below shows GOES-derived values from 1756-2201 UTC on 22 July. The data are produced every 5 minutes, and the extensive smoke pall is captured.

GOES-16 Aerosol Optical Depth, 1756 – 2201 UTC on 22 July 2024 (Click to enlarge)

Four VIIRS overpasses occurred during the 5 hour animation shown above. The four toggles below compare the VIIRS and GOES-R AOD. The VIIRS product on this day shows more coverage. This is likely related to the different cloud masks.

Aerosol Optical Depth estimates ca. 1841 UTC on 22 July 2024 from VIIRS and from GOES-16 ABI (Click to enlarge)
Aerosol Optical Depth estimates ca. 1906 UTC on 22 July 2024 from VIIRS and from GOES-16 ABI (Click to enlarge)
Aerosol Optical Depth estimates ca. 2031 UTC on 22 July 2024 from VIIRS and from GOES-16 ABI (Click to enlarge)
Aerosol Optical Depth estimates ca. 2056 UTC on 22 July 2024 from VIIRS and from GOES-16 ABI (Click to enlarge)

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