MODIS true color RGB image + MODIS false color RGB image

A comparison of a MODIS true color Red/Green/Blue (RGB) image with the corresponding MODIS false color RGB image of Hudson Bay, Canada on 15 December 2011 (above) revealed the following: (1) most of the northern and western portions of Hudson Bay were ice-covered (the ice appeared bright white on the true color image, and darker shades of red on the false color image) and (2) thee false color image made it easier to discriminate between the ice (darker red) and a diverging pattern of supercooled water cloud streets (white to cyan colored features) which were aligned in the direction of strong boundary layer winds in the wake of a cold frontal passage. The horizontal convective rolls that created these cloud streets may have also contained significant amounts of blowing snow.

AWIPS images of MODIS false color RGB images with overlays of METAR surface reports (below) showed that winds were gusting as high as 33 to 38 knots at stations along the western edge of Hudson Bay.

MODIS Red/Green/Blue (RGB) false color images

McIDAS images of GOES-13 0.63 µm visible channel data (below) showed that the strong winds were acting to move large portions of the ice, which according to the Canadian Ice Service was still fairly young “gray” (5-15 cm thick) to “gray-white” (15-30 cm thick) ice.

GOES-13 0.63 µm visible channel images

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1-km resolution MODIS vs 4-km resolution GOES-13 fog/stratus product images

The National Weather Service forecast office in Mobile, Alabama mentoned their use of the MODIS fog/stratus product during the pre-dawn hours on 14 December 2011:

AREA FORECAST DISCUSSION
NATIONAL WEATHER SERVICE MOBILE AL
1140 PM CST TUE DEC 13 2011

.AVIATION UPDATE (14/06Z ISSUANCE)…LOW CIG AND VSBY CONDITIONS CONTINUE. GOES IMAGER 11-3.9 AND MODIS POLAR ORBITER CONTINUE TO INDICATE A LOW STRATUS DECK WITH LOW VISIBILITY IN A LAYER WHOSE EDGE OVERLAYS A LINE FROM NEAR FOLEY TO BAY MINETTE AND ON UP TO CAMDEN. POINTS WEST OF SAID LINE ARE PRETTY WELL SOCKED IN AND PRETTY CLEAR ELSEWHERE. HAVE THEREFORE KEPT REDUCED PREVAILING GROUP TO A QUARTER MILE AND VV001 FOR BFM AND MOB.

A comparison of AWIPS images of the 1-km resolution MODIS vs the corresponding 4-km resolution GOES-13 fog/stratus product (above) demonstrated the advantage of using higher spatial resolution data to more accurately locate the eastern edge of the fog.

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MODIS true color Red/Green/Blue (RGB) image (displayed using Google Earth)

A 250-meter resolution MODIS true color Red/Green/Blue (RGB) image from the SSEC MODIS Today site (above) showed the areal coverage of lake-effect snow cover downwind of Lake Erie on 11 December 2011. Snow depths across this particular region were generally small, in the 1 to 4 inch range.

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MODIS fog/stratus product + METAR surface reports

AWIPS images of the 1-km resolution MODIS fog/stratus product (above) showed areas of freezing fog that were persisting across parts of the Pacific Northwest region of the US during the pre-dawn hours on 10 December 2011. This freezing fog was causing a few traffic accidents on roadways across the region.

On the previous day (09 December), an NPP VIIRS true color image (below; courtesy of Liam Gumley, CIMSS) showed the daytime coverage of the fog and stratus features that were trapped beneath a strong temperature inversion with stagnant high pressure in place over the region.

NPP VIIRS true color image (courtesy of Liam Gumley, CIMSS)

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