GOES-13 0.63 µm visible channel images (click to play animation)

McIDAS images of GOES-13 0.63 µm visible channel data (above; click image to play animation) revealed a well-defined mesovortex moving southeastward across the southern part of Lake Superior during the day on 15 December 2013. As the feature approached the Upper Peninsula of Michigan, a secondary mesovortex could be seen to the east-southeast of the larger primary mesovortex. These mesovortices produced bands of heavy snowfall and strong winds (with gusts as high as 60 mph offshore at Stannard Rock, and 46 mph inland at Marquette), which reduced surface visibility to less than 0.1 miles at times. Farther to the south, another item of interest seen in the imagery was the slow eastward drift of ice floes in the northern portion of Green Bay.

During the preceding night-time hours, an AWIPS image of Suomi NPP VIIRS 0.7 µm Day/Night Band data at 07:24 UTC or 2:24 AM local time (below) showed cloud bands starting to wrap around the mesovortex as it was beginning to form in the northern part of Lake Superior (northeast of Isle Royale). This example highlights the “visible image at night” capability of the VIIRS Day/Night Band (given sufficient illumination by moonlight — in this case, the Moon was in the Waxing Gibbous phase, at 98% of full). An overlay of the 07 UTC RTMA surface wind field confirmed the presence cyclonic flow around the developing mesovortex.

Suomi NPP VIIRS 0.7 µm Day/Night Band image, with RTMA surface winds

During the morning hours, the circulation of the primary mesovortex could be seen on Metop ASCAT scatterometer surface winds at 15:28 UTC or 10:28 AM local time (below).

GOES-13 0.63 µm visible channel image, with Metop ASCAT scatterometer surface winds

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MODIS 0.65 µm visible channel images, with METAR surface and buoy reports

Cloud features associated with the pair of mesovortices could be seen in detail on 16:58 UTC (11:58 AM local time) and 18:40 UTC (1:40 PM local time) 1-km resolution MODIS 0.65 µm visible channel images (above) and 11.0 µm IR channel images (below). Cloud-top IR brightness temperatures on the MODIS IR images were in the -30ºC to -40ºC range (dark blue to green color enhancement), indicating significant vertical development of some of the banding structure.

MODIS 11.0 µm IR channel images, with METAR surface and buoy reports

Even greater detail can be seen using 250-meter resolution Terra and Aqua MODIS true-color Red/Green/Blue (RGB) images from the SSEC MODIS Today site (below). Regarding the ice in Green Bay, there was a news story discussing the impact of this early ice formation on shipping.

Terra and Aqua MODIS true-color RGB images

Another indication of the vertical extent of some of the mesovortex banding features was the strong illumination of the southern sides of the bands by the low mid-December sun angle, as seen in a comparison of the 18:48 UTC (1:48 PM local time) Suomi NPP VIIRS 0.64 µm visible channel image with the corresponding VIIRS false-color “snow-vs-cloud discrimination” RGB image (below). In this RGB image, surface snow and ice (as well as glaciated cloud tops) appear as varying shades of red — in contrast, supercooled water droplet clouds appear as shades of white.

Suomi NPP VIIRS 0.63 µm visible and false-color RGB images

Signatures of the twin mesovortices were evident on NWS Marquette, Michigan radar base reflectivity (below). Additional radar imagery can be seen the WeatherMatrix Blog.

Marquette, Michigan radar base reflectivity

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GOES-13 0.63 µm visible channel images (click to play animation)

On the morning of 14 December 2013, GOES-13 0.63 µm visible channel images (above; click image to play animation) showed what appeared to be a plume of re-suspended volcanic ash moving northward from the region of the Cordón Caulle volcano in Chile. As the airborne ash plume begain to disperse later in the day, it then began to move in a more northeasterly direction. Since no volcanic ash advisories were issued by the Beunos Aires Volcanic Ash Advisory Center (VAAC), it was assumed that this was a case of re-suspended ash that covered the ground following previous eruptions.

Although there is not always a thermal anomaly or “hot spot” seen on shortwave IR satellite images accompanying a volcanic eruption, no such hot spot was seen on the corresponding GOES-13 3.9 µm shorwave IR imagery (below; click image to play animation). The higher terrain of the Cordón Caulle volcano complex — located in the center of the images — initially appeared cooler (lighter gray) prior to sunrise, but then their higher-elevation surfaces begain to warm (darker gray pixels) after sunrise. The plume of re-suspended volcanic ash also exhibited a darker appearance after sunrise, due to the reflection of solar radiation off the small particles.

GOES-13 3.9 µm shortwave IR images (click to play animation)

Quantitative products derived from Terra MODIS imagery (below) indicated that the plume had a maximum height of around 5-6 km, with ash/dust loading in the 4-5 g/m2 range, and a mean particle effective radius as large as 4-6 µm.

Terra MODIS Ash Height product

Terra MODIS Ash/Dust Loading product

Terra MODIS Ash Particle Effective Radius product

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GOES-13 6.5 µm water vapor channel images, with surface analysis and METAR surface reports

A large and strong cyclone was intensifying in the North Atlantic Ocean just south of Greenland on 12 December 2013. GOES-13 6.5 µm water vapor channel images with 06 UTC, 12 UTC, 18 UTC, and 00 UTC surface analyses and surface reports (above) showed that the central pressure of the storm deepened to 942 hPa at 18 UTC — and the strong pressure gradient between the low and a 1032 hPa high situated over northern Greenland was forecast to produce a broad region of hurricane-force winds.

EUMETSAT Metop ASCAT scatterometer surface winds at 22:41 UTC (below) highlighted 3 areas over the water which contained a number of remotely-sensed winds of 50 knots or higher (red barbs). The strongest wind velocity within this ASCAT swath was 54 knots, located in the largest area of red wind barbs south of the storm center.

GOES-13 6.5 µm water vapor image and ASCAT scatterometer surface winds

Near the time of the 22:41 UTC ASCAT data, surface winds were a steady 50 knots from the north-northwest at Cape Dyer, Nunavut, Canada (station idendifier CWFD) — and the peak wind gust at that station was 56 knots several hours prior at 18 UTC. In southern Greenland, the peak wind gust at Narsarsuaq (station identifier BGBW) was 71 knots, occcurring earlier in the day at 13 UTC (below).

Time series of meteorological data at Cape Dyer, Nunavut, Canada

Time series of meteorological data at Narsarsuaq, Greenland

GOES-13 6.5 µm water vapor images at 30-minute intervals (below; click image to play animation) displayed an interesting range of signatures as moisture wrapped around the very large storm.

GOES-13 6.5 µm water vapor channel images (click to play animation)

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GOES-13 0.63 µm visible channel images (click to play animation)

The GOES-13 (GOES-East) satellite was placed into Super Rapid Scan Operations (SRSO) mode on 11 December 2013, to provide bursts of imagery at 1-minute intervals in support of the OWLeS project. McIDAS images of GOES-13 0.63 µm visible channel data (above; click image to play animation) showed multiple lake-effect snow (LES) bands over Lake Superior, Lake Michigan, and Lake Huron (with a larger dominant band over the northern portion of Lake Huron). Large single-band LES features had also formed farther to the east over Lake Erie and Lake Ontario, but their presence was masked by bands of layered high clouds over that region.

Prior to the beginning of the SRSO period, a comparison of the 18:23 UTC Suomi NPP VIIRS 0.64 µm visible channel image with the corresponding false-color “snow-vs-cloud discrimination” Red/Green/Blue (RGB) image (below) could be used to get a qualitative indication of which LES bands might be glaciating — snow and ice on the ground (as well as clouds whose tops were comprised of ice crystals) appeared as varying shades of red on the false-color image. Surface METAR data showed that cold surface air was flowing southeastward and eastward over the still-unfrozen waters of the western Great Lakes.

Suomi NPP VIIRS 0.64 µm visible channel and false-color RGB images

A comparison of the 18:23 UTC Suomi NPP VIIRS 0.64 µm visible channel and 11.45 µm IR channel images (below) indicated that many of the cloud bands exhibited IR brightness temperatures in the -20 to -30º C range (cyan to dark blue color enhancement), with the coldest IR brightness temperatures of -35º C associated with the most organized bands in eastern Lake Superior and northern Lake Huron. The patches of layered high clouds farther east over Lake Erie and Lake Ontario had cloud tops as cold as -40º C (green color enhancement).

Suomi NPP VIIRS 0.64 µm visible channel and 11.45 µm IR channel images

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