The GOES-14 satellite was in Super Rapid Scan Operations for GOES-R (SRSOR) mode, providing images at 1-minute intervals over the southeastern US on 21 August 2014. An animation of 0.63 µm visible channel images (above; click to play YouTube movie) showed the development of numerous large thunderstorms, many of which were focused along surface boundaries such as the sea breeze and other convective outflow boundaries. The YouTube video is best viewed in Full Screen mode, using the “Gear” icon to select 1080p HD resolution.
The GOES-14 satellite was in Super Rapid Scan Operations for GOES-R (SRSOR) mode, providing images at 1-minute intervals over the central US on 20 August 2014; an animation of 0.63 µm visible channel images (Animated GIF | MP4 movie | YouTube) showed the dissipation of river valley fog that had formed during the previous night over the Mississippi River and adjacent portions of southwestern Wisconsin, southeastern Minnesota, and northeastern Iowa. The 3 panels show images every 15 minutes (today’s current routine schedule), every 5 minutes (available during Rapid Scan Operations), and every 1 minute (which will be available from the ABI instrument on the next-generation GOES-R satellite).
Along the Wisconsin River valley, fog restricted the surface visibility to 0.15 mile at Prairie Du Chien KPDC and Boscobel KOVS, and 0.25 mile at Lone Rock KLNR (images with map and station location overlays).
The GOES-14 satellite was in Super Rapid Scan Operations for GOES-R (SRSOR) mode, providing coverage of Tropical Storm Lowell in the East Pacific Ocean on 19 August 2014; an animation of 0.63 µm visible channel images (Animated GIF | MP4 movie file | YouTube) showed a gradual increase in the organization of a convective banding structure during the day. At 12 UTC Tropical Storm Lowell was located several hundred miles southwest of Baja California, with a center at 15.5º North latitude, 119.5º West longitude.
GOES-15 10.7 µm IR channel images with an overlay of Metop ASCAT surface scatterometer winds from the CIMSS Tropical Cyclones site (below) showed the the strongest winds (40.0-49.9 knots, yellow barbs) were in the southeastern quadrant of Lowell at 17:11 UTC.
A comparison of the 16 UTC GOES-15 10.7 µm IR channel image with the corresponding DMSP SSMIS 85 GHz microwave image (below) indicated that the highest rainfall rates were associated with the convective banding (and coldest cloud tops) within the southern semicircle of the storm.
The GOES-14 satellite was in Super Rapid Scan Operations for GOES-R (SRSOR) mode providing 1-minute imagery over the eastern US on 18 August 2014. From the late morning into the afternoon hours, 0.63 µm visible channel images (above; click image to play animation; also available as an MP4 movie file or a YouTube video) revealed a large and well-defined mesoscale convective vortex (MCV) propagating eastward across northern Mississippi. This MCV was spawned from a thunderstorm which rapidly developed over far southwestern Arkansas during the preceding nighttime hours (beginning around 06:15 UTC: GOES-13 IR images).
A comparison of Suomi NPP VIIRS 11.45 µm IR channel images (below) showed the rapid growth of the parent thunderstorm from 07:18 UTC to 08:59 UTC. The coldest cloud-top IR brightness temperatures were -80º C.