Today marks the 50th anniversary of the launch of ATS-1 on 06 December 1966. ATS-1 was the first meteorological satellite to be placed into a geostationary orbit — an example of one of the first ATS-1 visible images is seen below, and QuickTime movies are available which show animations of some early ATS-1 images. More information is available from SSEC and NOAA/NESDIS.
A closer view of the GMS-4 Infrared Window (11.5 µm) images (below) revealed interesting characteristics of the volcanic plume which penetrated the tropopause (which was at an air temperature of around -83º C, according to nearby rawinsonde reports) during the 3-8 hours following the onset of the 0227 UTC eruption. Note the initial appearance of a small area of very warm IR cloud-top IR brightness temperatures (-21.6º C at 0631 UTC, and -25.7º C at 0730 UTC) which then blossomed outward and became a westward-moving stratospheric plume that was notably warmer than the majority of the cold volcanic cloud canopy (which exhibited IR brightness temperatures in the -80º to -90º C range, denoted by the violet to yellow color enhancement).
———————————————————————————————————-A higher-resolution (1.1-km) view of the post-eruption cloud was provided by NOAA-10 AVHRR images at 1034 UTC on 15 June (above). Even though it was just past sunset over the Philippines, the narrow stratospheric plume could be seen towering above the canopy of the main volcanic cloud (the plume was at a high enough altitude — estimated at a maximum of 40 km (reference 1 | reference 2) — to still be illuminated by sunlight). The summit of Pinatubo is located 8.7 miles/14 km west-southwest of what was then Clark Air Force Base (station identifier RPLC). On the 10.8 µm Infrared Window image, cloud-top gravity waves could be seen propagating radially outward from the overshooting top located above the volcano (which exhibited a minimum IR brightness temperature of -86º C, violet color enhancement). Note the much warmer IR brightness temperatures (as warm as -31º C, green color enhancement) associated with the stratospheric plume just off the west coast of Luzon. A closer view is available here.
About 10 hours prior to the climactic eruption, a volcanic ash cloud from one of the earlier eruptions was captured by NOAA-10 AVHRR images at 2329 UTC on 14 June (below). Around this same time it can be seen that Yunya was making landfall as a minimal-intensity typhoon along the eastern coast of Luzon. A closer view is available here.
GOES-3 started service on 16 June 1978 and was the operational GOES-West satellite until the late 1980s. Having lost imaging capabilities, it started a second long life as a communications satellite; GOES-3 is currently the oldest operating satellite. Decommissioning will begin on 8 June and run for 15 days. If final decommissioning happens as planned on 23 June, GOES-3’s service life will be 38 years, 7 days.
GOES-3’s arguably most famous imagery occurred during the eruption of Mount St. Helens on 18 May 1980, shown above (click here for an animation of the eruption, courtesy of Barry Roth, SSEC; Tim Schmit, NOAA/ASPB also provided longer visible animations: MP4 | animated GIF).
A comparison of GOES-3 Visible (0.65 µm) and Infrared Window (11.5 µm) images, below, showed that a large portion of the volcanic cloud exhibited IR brightness temperatures of -60º C (dark red color enhancement) or colder as the feature moved rapidly eastward during the first 10 hours following the eruption. It is interesting to note that an “enhanced-V” or cold/warm (-65º/-47º C) thermal couplet signature was evident on the initial 1545 UTC Infrared image (zoom), as the volcanic ash cloud rapidly rose to an estimated altitude of 12 to 16 miles (20 to 27 km) above sea level.Some early examples of full disk GOES-3 images (on 20 November 1978) are shown below, courtesy of Tim Schmit, NOAA/ASPB.
GOES-8 Infrared (10.7 µm, 4-km resolution) images (below; also available as a 111-Mbyte animated GIF) showed that cloud-top IR brightness temperatures began to cool into the -50 to -60º C range (orange to red color enhancement) over large portions of the Upper Midwest and Great Lakes regions during the day on 02 January. As the bulk of the storm energy moved northeastward over Canada on 03-04 January, evidence of clouds associated with a TROugh of Warm air ALoft (TROWAL) persisted across parts of Minnesota and Wisconsin.Even though some patches of clouds remained in the aftermath of the blizzard on 04 January, the extent of snow cover across much of the eastern US could be seen — from northern Arkansas to Minnesota, and from the Dakotas and Nebraska to Ohio — on GOES-8 Visible (0.65 µm, 1-km resolution) images (below; also available as a 15 Mbyte animated GIF). Bands of lake effect snow were also evident over each of the Great Lakes, as very cold arctic air flowed across the ice-free waters in the wake of the storm. In the Upper Midwest region, storm total snowfall amounts included: 28.0 inches in South Haven, Michigan; 26.8 inches in Plymouth, Indiana; 23.0 inches in Dalton, Wisconsin; and 19.6 inches a Chicago O’Hare, Illinois. Chicago recorded 18.6 inches of snow on 02 January — their largest single-day snowfall on record. In Canada, Toronto, Ontario’s Pearson International Airport was closed by the storm, where 16.0 inches of snow fell. With deep snow cover and a cold post-storm arctic air mass in place, the all-time record low temperature for the state of Illinois (-36º F) was set at Congerville on 05 January.