The corresponding GOES-16 “Clean” Infrared Window (10.35 µm) images (below) indicated that cloud-top infrared brightness temperatures were frequent as cold as -70 to -80ºC (black to white to violet enhancement) with the more vigorous thunderstorms.
One interesting aspect of this line of deep convection is that it was effectively blocking the upstream southwesterly flow, creating a band of gravity waves along its western edge — these waves were very evident in GOES-16 Low-level (7.3 µm), Mid-level (6.9 µm) and Upper-level (6.2 µm) Water Vapor images (below). GOES-16 Split Window Difference (10.3-12.3 µm) images (below) displayed the yellow signature of blowing dust in the vicinity of a cold front that was moving eastward across southeastern New Mexico and southwestern Texas. During the subsequent overnight hours, these thunderstorms produced heavy rainfall from northern Oklahoma into southern Kansas, causing flash flooding — and rising rivers across that region on the following day were captured by the Suomi NPP VIIRS Flood Detection Product (below).from CIMSS Satellite Blog http://cimss.ssec.wisc.edu/goes/blog/archives/33284
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