Nighttime images of Suomi NPP VIIRS Shortwave Infrared (3.9 µm), Longwave Infrared Window (11.45 µm), and Day/Night Band (0.7 µm) images at 0817 UTC on 25 January (below, courtesy of William Straka, SSEC) revealed the hot spot of the erupting volcano summit (orange pixels), and ample illumination from the Moon allowed the plume to be seen on the Day/Night Band image. The large areas of bright city lights from Mexico City and Pueblo (located northwest and southeast of Popocatépetl, respectively) are also very apparent on the Day/Night Band image.A legacy product for use in the detection of volcanic ash plumes is the Infrared “Split-Window” (11-12 µm) brightness temperature difference product (below), which showed the plume streaming eastward to northeastward during the 24-25 January period. Taking advantage of the multi-spectral imagery available from the MODIS and VIIRS instruments on the Terra/Aqua ans Suomi NPP satellites, quantitative products can be derived such as Ash Height, Ash Loading, Ash Effective Radius, and Ash Probability from the NOAA/CIMSS Volcanic Coud Monitoring (below).
A GOES-R volcanic ash height product (derived using Himawari-8 AHI data) from the SSEC Volcanic Cloud Monitoring site indicated that the plume reached heights of 10 km (dark blue color enhancement) at times during the 03-04 October period (below).McIDAS-V images of Suomi NPP VIIRS Day/Night Band (0.7 µm), near-IR (1.6 µm), shortwave IR (3.74 µm), and IR (11.45 µm) images (below, courtesy of William Straka, SSEC) showed the hot spot and nighttime glow of the summit of the Rinjani volcano at 1733 UTC on 04 November.
The corresponding GOES-13 infrared (10.7 µm) images (below; click image to play animation) showed that cloud-top IR brightness temperatures were as cold a -53º C (orange color enhancement) at 1915 UTC.The volcanic cloud features were also easily tracked on GOES-13 water vapor (6.5 µm) images (below; click image to play animation). In fact, note how the signature in the water vapor imagery is more distinctly seen for a longer period of time than on the 10.7 µm infrared imagery. The tan-colored volcanic ash cloud was also evident on Aqua MODIS and Suomi NPP VIIRS true-color Red/Green/Blue (RGB) imagery (below), as viewed using the SSEC RealEarth web map server. A comparison of Suomi NPP VIIRS visible (0.64 µm) and infrared (11.45 µm) images is shown below (courtesy of William Straka, SSEC). The coldest cloud-top IR brightness temperature was -72.7º C.
The Kuchinoerabu-jima volcano in Japan experienced a violent eruption beginning around 00:59 UTC on 29 May 2015 — the expanding volcanic cloud was captured by 0.5-km resolution Himawari-8 AHI 0.64 µm visible channel images (above; click image to play animation; also available as an MP4 movie file). A mid-layer volcanic cloud was seen moving to the west-northwest, while a high-altitude plume spread out as it moved east-southeastward.
About an hour after the eruption, Terra MODIS products at 0205 UTC from the SSEC Volcanic Cloud Monitoring site are shown below. Retrieved volcanic Ash Probabilities were very high for both cloud segments; for the southeastern cloud segment, the maximum volcanic Ash Height was in the 10-12 km range, volcanic Ash Loading was high, and the largest Ash Effective Radius values were in the 8-10 um range.