GOES-11 6.7 µm (left) and GOES-15 6.5 µm (right) water vapor channel images (click image to play animation)

McIDAS images of 8-km resolution GOES-11 6.7 µm and 4-km resolution GOES-15 6.5 µm water vapor channel data (above) demonstrated the advantage of improved spatial resolution for the detection of features and gradients in the water vapor imagery associated with a weak upper level low moving eastward across the southwestern US on 14 September 2010. GOES-15 is scheduled to replace GOES-11 as the operational GOES-West satellite in December 2011.

AWIPS images of the GOES-11 sounder Convective Available Potential Energy (CAPE) product (below) showed that the atmosphere was destabilizing in advance of the upper low, with CAPE values in the 1000-2000 J/kg range.

GOES-11 sounder Convective Available Potential Entegy (CAPE)

With the increasing instability and large scale lift ahead of the upper low, areas of thunderstorms developed over parts of Nevada, Arizona, and Utah, as seen on a MODIS 11.0 µm IR image with an overlay of cloud-to-ground lightning strikes (below). About an hour after the time of the MODIS image, one of these storms produced 1.0-inch diameter hail that covered the ground near Munds in northern Arizona (SPC storm reports).

MODIS 11.0 µm IR image + cloud-to-ground lightning strikes

CIMSS participation in GOES-R Proving Ground activities includes making a variety of MODIS and additional GOES Sounder images and products available for National Weather Service offices to add to their local AWIPS workstations. Currently there are 49 NWS offices receiving MODIS imagery and products from CIMSS.

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GOES Water Vapor Imagery and turbulence reports

Clear Air Turbulence can be a significant aircraft hazard, occasionally causing injuries and long delays. (See, for example, here and here for two recent examples. The second example resulted in a 6-hour delay (Link))

At the upper-tropospheric boundary between air masses, vertical shearing at the jet stream combined with the ageostrophic convergence of polar, subtropical and stratospheric air produces a region known for its potential for clear air turbulence called a “tropopause fold.” These features are evident in satellite-observed upper tropospheric water vapor by the large-scale spatial gradients in brightness temperature, which define boundaries between the air masses. The tropopause fold extends from this boundary to a limited distance into and underneath the wetter air mass.

Thus, water vapor imagery can be used to infer large changes in vertical motion that can herald the presence of turbulence in the atmosphere. For example, in the region of turbulence shown in the water vapor imagery above, the yellow enhancement — warm brightness temperatures — suggest water vapor concentrated lower in the atmosphere (subsidence); bluer enhancements — colder brightness temperatures — suggest water vapor that is concentrated higher in the atmosphere (rising motion).

The Tropopause Folding Turbulence Prediction (TFTP) product locates these regions in the atmosphere and identifies the sections most likely to produce turbulent flight conditions for aircraft. The upper-tropospheric water vapor channel of the GOES-R Advanced Baseline Imager (primary: channel 8, backup: channel 9) is the source for resolving gradients that reveal the horizontal distribution of tropopause folds. An ancillary numerical weather model constrains these features vertically in the atmosphere. The four key output products consist of two fields that define the lower and upper bounds of the turbulent volumes of air, and two fields that define the two flight directions that are the most susceptible to moderate or greater turbulence. For now, the GOES-East (or MODIS) water channels can be used as a proxy.

GOES Water Vapor Imagery and turbulence reports

The animated gif above shows the predicted tropopause fold (green), model results that show the tropopause (yellow, the 1-2 PV Unit surface) for a turbulence event that occurred in September 2011 (link). Note that the strongest turbulence (red airplane icon) occurred as the plane traversed the fold.

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

The animation of water vapor imagery (above) centered on the time of the turbulence includes some key features. For example, the gradient in the water vapor field between the colder brightness temperatures over the Atlantic Ocean south of New England and the warmer brightness temperatures off the coast of New Jersey is tightening with time. There is also evidence of a jet feature propagating northeastward along the gradient from east of the mouth of Chesapeake Bay at the start of the loop to south of Long Island at the end of the loop. Both of these features are suggestive of an evolving tropopause fold.

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MODIS true color and false color RGB images (11 September)

MODIS true color and false color RGB images (12 September)

250-meter resolution MODIS true color and false color Red/Green/Blue (RGB) images from the SSEC MODIS Today site (above) showed the very large pyrocumulus and smoke plume from the Pagami Creek wildfire that was burning in the Boundary Waters Canoe Area Wilderness region of northeastern Minnesota on 11 September 2011 and 12 September 2011. The wildfire “hot spot” appears as the large red-colored feature on the false color images.  Other options for viewing this MODIS imagery include the SSEC Web Mapping Service and WisconsinView sites: WMS MODIS image | WisconsinView: Terra and Aqua MODIS images.

A comparison of AWIPS images of 1-km resolution MODIS 0.65 µm visible channel, 3.7 µm shortwave IR channel, and 11.0 µm IR window channel data (below) revealed the very large fire “hot spot” on the shortwave IR image (red to yellow to black color enhancement) — and also note that the resulting pyrocumulus cloud just east of the fire hot spot exhibited a cloud top 11.0 µm IR window brightness temperature of -70º C (black color enhancement), which was just as cold as that associated with the thunderstorms farther to the north in Ontario, Canada!

MODIS 0.65 µm visible, 3.7 µm shortwave IR, and 11.0 µm IR images

AWIPS images of GOES-13 3.9 µm shortwave IR data (below) showed the diurnal changes to the size and intensity of the fire hot spot. Early in the animation during the overnight and morning hours, the hot spot was smaller and less intense as the wind speeds became very light– however, once strong southwesterly winds began to increase during the afternoon hours in advance of an approaching cold front, the hot spot was seen to dramatically increase in size as the fire quickly grew.

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

A comparison of the 4-km resolution GOES-13 3.9 µm and the 1-km resolution MODIS 3.7 µm shortwave IR images (below) demonstrated the advantage of better spatial resolution for more accurate location of the fire hot spot boundaries. In addition, the MODIS image revealed another small fire hot spot could be seen to the north, just across the Minnesota/Ontario border — this small fire was not seen on the GOES-13 image.

MODIS 3.7 µm and GOES-13 3.9 µm shortwave IR images

===== 13 September Update =====

A significant amount of smoke was transported southeastward across Wisconsin on 13 September 2011, as seen on GOES-13 0.63 µm visible channel images (below). The surface visibility was reduced to 2 miles at Milwaukee (station identifier KMKE), and 3 miles at Chicago O’Hare (station identifier KORD). Special Weather Statements were issued by the National Weather Service forecast offices at Milwaukee/Sullivan and Chicago/Romeoville to advise the public about the potential harmful effects of the smoke.

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

The smoke feature was even more apparent on the afternoon MODIS true color Red/Green/Blue (RGB) image (below), and this smoke produced an elevated signal on the MODIS Aerosol Optical Depth (AOD) product from the IDEA site.

MODIS true color Red/Green/Blue (RGB) image

CIMSS participation in GOES-R Proving Ground activities includes making a variety of MODIS images and products available for National Weather Service offices to add to their local AWIPS workstations. Currently there are 49 NWS offices receiving MODIS imagery and products from CIMSS.

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GOES-13 10.7 µm IR images

GOES-13 10.7 µm IR images from the CIMSS Tropical Cyclones site (above) showed increasing convective banding within the eastern semicircle of Tropical Storm Nate as the system was undergong a period of intensification on 10 September 2011.

Deep layer wind shear was light over the region (below), which was a factor that aided in the intensification of the tropical cyclone.

GOES-13 IR image + 200-850 hPa deep layer wind shear product

A TRMM 85 GHz microwave image from 16:12 UTC (below) showed the band of deep convection withn the southeastern quadrant of Nate.

TRMM 85 GHz microwave image

The GOES-13 satellite had been placed into Super Rapid Scan Operations (SRSO), providing bursts of 1-minute interval imagery. A sample of GOES-13 0.63 µm visible channel SRSO images (below; click image to play animation) showed the development of the convective bands wrapping around the center of the tropical cyclone. Early in the animation, you can also see the hazy appearance of the water to the east of Nate (off the west coast of the Yucatan Peninsula of Mexico) — this enhanced turbidity was the result of persistent strong southerly winds across those waters as Nate developed and moved very slowly across the region.

GOES-13 0.65 µm visible channel SRSO images (click image to play animation)

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