A comparison of AWIPS images of the 1-km resolution MODIS 0.65 µm visible channel (first shown with a map overlay and location of METAR sites) and the corresponding 1-km resolution MODIS 2.1 µm near-IR “snow/ice channel” (above) shows the areal coverage of flood waters across the region of the confluence of the Mississippi River and the Ohio River on 04 May 2011. Since water happens to be a strong absorber at the 2.1 µm wavelength, it shows up as a very dark feature on the MODIS “snow/ice channel” image — making it more useful for locating areas of flooding than just a simple visible channel image.

A similar near-IR channel will be on the ABI instrument of the future GOES-R satellite. 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.

MODIS True-color imagery from the SSEC MODIS Today website can be used to compare data from this year and last year, shown below. In the linked-to-images, the Mississippi River north of Memphis (located at the bottom edge of each image) meanders through the center part of the images. There are several former meanders of the river in Arkansas and Tennessee that are filled with water this year, but not last.

 

 

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A late-season blizzard produced as much as 14.0 inches of snowfall with winds gusting as high as 78 mph across western North Dakota (and 10.0 inches of snowfall across extreme eastern Montana) on 30 April 2011, causing power outages and the closure of Interstate 94 from Dickinson to the Montana border. On the following day (01 May 2011), AWIPS images of MODIS 0.65 µm visible channel data (above) displayed a mixture of fresh snow cover and cloudiness across parts of western North Dakota, far southeastern Saskatchewan, and southwestern Manitoba. However, in some areas it was difficult to visually separate the cloud features from the snow cover (although the edges of the snow pack that were quickly melting within the 102-minute time period between the 2 MODIS images were fairly obvious).

The corresponding pair of MODIS false color Red/Green/Blue (RGB) images (below) — created using MODIS bands 01/07/07 — allowed for the unambiguous discrimination between the fresh snow cover (which appeared darker red) and the various cloud features (supercooled water droplet clouds exhibited a much brighter appearance, while glaciated ice crystal clouds appeared as varying shades of pink). As much as 7 inches of snow remained on the ground that morning at Williston in northwestern North Dakota (station identifier KISN) as well as at a couple of stations in southwestern Manitoba. Also note that along the Missouri River there is a significant amount of ice remaining on much of the eastern half of Lake Sakakawea in the vicinity of Garrison, North Dakota (station identifier KN60).

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.

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A comparison of 250-meter resolution Aqua MODIS 0.65 µm and 0.87 µm visible channel images centered on Tuscaloosa, Alabama on 28 April 2011 (above) showed signatures of a few of the larger and longer tornado damage paths from the historic tornado outbreak (SPC storm reports) that occurred on 27 April 2011. A collection of GOES, POES AVHRR, and MODIS images of the tornado outbreak are available on a separate CIMSS Satellite Blog post.

A comparison of before (17 April 2011) and after (28 April 2011) 250-meter resolution MODIS true color Red/Green/Blue (RGB) images from the SSEC MODIS Today site (below) also showed a few of the tornado damage paths — though some of the damage paths were not as evident as they were on the single-channel visible images above. In addition, another long tornado track can be seen across western Georgia.

Below is the same before/after MODIS true color image comparison, viewed using Google Earth.

A comparison of AWIPS images of 1-km resolution MODIS 0.65 µm visible channel data and the corresponding 1-km resolution Normalized Difference Vegetation Index (NDVI) product (below) revealed that a few of the larger tornado damage paths were characterized by a slightly lower NDVI value (lighter green color), due to the downed trees and damaged vegetation.

One of the larger tornado damage tracks across northwestern Alabama was also apparent on GOES-13 0.63 µm visible channel imagery (below). An animation helps to confirm that the feature is not a contrail or some other type of linear cloud feature (which would be moving in an animation, rather than stationary). While the north-south spatial resolution of the GOES imager visible detectors is 1.0 km at the satellite sub-point (over the Equator), with the larger geostationary satellite viewing angle the north-south spatial resolution over northern Alabama is about 1.38 km.

It is interesting to note that the larger tornado damage path which can been seen across northwestern Alabama on the GOES-13 visible image is very difficult to identify on the corresponding GOES-12 0.65 µm visible image (below). This is due to a change is the spectral response function on the visible channel of the GOES-13 and later series of imagery instruments — for more details, see this CIMSS Satellite Blog post.

Update 29 April 2011: A Terra MODIS pass from late morning on April 29th shows the damage paths more clearly through central Alabama. As the churned-up vegetation within the damage path slowly browns, the contrast to undamaged vegetation outside the damage path should increase, allowing for a clearer picture of the damage path. The bowtie-corrected MODIS imagery for visible channel 1 (0.65 microns, below) and visible Channel 2 show three lines of damage through central Alabama. (Here is an animation of the two visible channels).

Since this day was less cloudy than the previous, here is a better before (17 April) versus after (29 April) comparison of 250-meter resolution MODIS true color images from the SSEC MODIS Today site (below, viewed using Google Earth).

Update 30 April 2011: A few of the tornado damage paths across northern Alabama were also evident on an AWIPS image of the 1-km resolution MODIS Land Surface Temperature (LST) product (below). The LST values within the damage paths were in the low to middle 80s F (darker red color enhancement), compared to surrounding LST values in the upper 70s F (orange color enhancement), indicating that the damage paths with destroyed vegetation and tornado debris were able to heat up a few degrees more than the adjacent undisturbed vegetation. The urban areas of the cities of Tuscaloosa (KTCL) and Birmingham (KBHM) also exhibited warmer LST values (darker red) than the surrounding less urbanized, more densely forested areas.

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.

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The tornado outbreak that affected much of the Southeast US on 27 April 2011 was one of historic proportions, in terms of the number of strong to violent tornadoes produced and the number of resulting fatalities. McIDAS images of 1-km resolution GOES-13 0.63 µm visible channel data (above; click image to play animation; also available as a QuickTime movie) showed the multiple clusters of severe thunderstorms that developed across the region during the day. The GOES-13 satellite had been placed into Rapid Scan Operations (RSO), supplying imagery as frequently as every 5-10 minutes. Zoomed-in versions of GOES-13 RSO 0.63 µm visible images covering the period of the long-track (80 mile) EF-4 Tuscaloosa (KTCL) / Birmingham (KBHM) tornado are available here, which show that the storms exhibited a number of distinct overshooting tops during the time period between 20:40 UTC and 23:25 UTC.

AWIPS images of 4-km resolution GOES-13 10.7 µm IR channel data with overlays of severe weather reports (below; click image to play animation) showed the first round of large storms with cold cloud top IR brightness temperatures (red to black to white color enhancement) that moved through the area during the pre-dawn hours (which produced mainly damaging wind reports), followed by the development later in the afternoon and early evening hours of the stronger storms that produced numerous reports of large hail and strong tornadoes ahead of an advancing cold front (SPC storm reports). Zoomed-in versions of GOES-13 RSO 10.7 µm IR images covering the period of the long-track (80 mile) EF-4 Tuscaloosa (KTCL) / Birmingham (KBHM) tornado are available here — cloud top IR brightness temperature values during the 20:40 UTC to 23:25 UTC time period were as cold as -75ºC at 22:25 UTC.

With the higher 1-km spatial resolution of the POES AVHRR IR imagery (below), more detail could be seen in the cloud top IR brightness temperature structure, and much colder cloud top temperatures could be detected in the vicinity of the strongest overshooting tops (as cold as -83ºC, violet color enhancement). Other similar 1-km resolution POES AVHRR IR and MODIS IR image examples (with overlays of storm reports) are available at 16:28 UTC, 18:10 UTC, 18:12 UTC, 18:35 UTC, 19:48 UTC, 19:52 UTC, 20:13 UTC, 00:01 UTC, and 03:34 UTC.

Although there was widespread cloudiness across much of the Southeast US, hourly GOES-13 Sounder Convective Available Potential Energy (CAPE) derived product images (below) were still able to provide some indication as to the instability of the air mass that was feeding northward into the region that morning.

Another important ingredient was the approach of a strong trough aloft, along with an associated strong mid-level jet streak as seen in a comparison of 1-km resolution MODIS 6.7 µm water vapor imagery and CRAS model 500 millibar (hPa) wind speeds (below).

CIMSS participation in GOES-R Proving Ground activities includes making a variety of POES AVHRR, MODIS, and additional GOES Sounder images and products available for National Weather Service offices to add to their local AWIPS workstations. The VISIT training lessons “POES and AVHRR Satellite Products in AWIPS”, “MODIS Products in AWIPS“, and “Water Vapor Imagery and Potential Vorticity Analysis” are available to help users understand these products and their applications to weather analysis and forecasting.

To prepare for the upcoming GOES-R era, new products are being developed and tested at CIMSS using the current generation of satellite data — in fact, some of these new products are now being distributed to and evaluated by a few NWS Offices. Specially-tailored products such as Convective Initiation, Overshooting Tops, and Enhanced-V will allow for the automatic detection of the various developmental stages of convection.

Slide the “Set Fade Level” button located under examples of these images (above) to fade between the CIMSS Convective Initiation (CI) and CIMSS Overshooting Tops (OT) products (derived from satellite observations), along with Cloud-to-Ground (CG) lightning strikes observed from ground-based sensors. Note that there is good agreement between the locations of the satellite-derived CI and OT products and the SPC storm reports for the day (below).

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