Clik here to view.
![Himawari-8 Shortwave Infrared (3.9 µm, left) and Visible (0.64 µm, right) images [click to play animation]](http://www.rssing.com/inc2/img/tinyinf.webp)
Himawari-8 Shortwave Infrared (3.9 µm, left) and Visible (0.64 µm, right) images [click to play animation]
A 2-panel comparison of Himawari-8 Shortwave Infrared (3.9 µm) and Visible (0.64 µm) images (above) showed the “hot spot” (red pixels) associated with a large bush fire burning near Waroona (south of Perth) in Western Australia on 06 January 2016 (media report), along with smoke from the fire and the explosive development of a pyroCb cloud after about 0830 UTC. The variation in smoke transport was explained by the strong vertical wind shear profile seen on a plot of 12 UTC Perth rawinsonde data: easterly winds within the 800m-2000m layer were carrying smoke westward off the coast, while smoke transported to higher altitudes by the pyroCb cloud was drifting southeastward due to northwesterly flow aloft.
Himiwari-8 Infrared (10.4 µm) images (below) indicated that cloud-top IR brightness temperatures cooled to -40º C (bright green color enhancement) around 0830 UTC, eventually reaching a minimum of -56º C (darker orange color enhancement).
Clik here to view.
![Himawari-8 Infrared (10.4 µm) images [click to play animation]](http://www.rssing.com/inc2/img/tinyinf.webp)
Himawari-8 Infrared (10.4 µm) images [click to play animation]
During the nighttime hours following the initial pyroCb development, the fire raced westward as revealed by the spreading out of the red pixels on Himawari-8 Shortwave IR (3.9 µm) images and the light gray to brighter white pixels on Near-IR (2.3 µm) images (below).
Clik here to view.
![Himawari-8 Shortwave IR (3.9 µm) images [click to play animation]](http://www.rssing.com/inc2/img/tinyinf.webp)
Himawari-8 Shortwave IR (3.9 µm) images [click to play animation]
Clik here to view.
![Himawari-8 Near-IR (2.3 µm) images [click to play animation]](http://www.rssing.com/inc2/img/tinyinf.webp)
Himawari-8 Near-IR (2.3 µm) images [click to play animation]
On 07 January, two additional pyroCb clouds were seen to develop from the Waroona fire: the first after about 03 UTC, and the second after about 06 UTC. In this case, the pyroCb cloud material was transported rapidly eastward, as seen in Himawari-8 Infrared (10.4 µm) images (below), due to an increase in westerly winds aloft as seen in a plot of 00 UTC Perth rawinsonde data.
Clik here to view.
![Himawari-8 Infrared (10.4 µm) images [click to play animation]](http://www.rssing.com/inc2/img/tinyinf.webp)
Himawari-8 Infrared (10.4 µm) images [click to play animation]
A comparison of Suomi NPP VIIRS true-color images from 06 January and 07 January (below) showed an increase the thickness and areal coverage of smoke aloft over the region. (Note: the actual overpass times of the Suomi NPP satellite were between 06 and 07 UTC, as seen here and here)
Clik here to view.
![Suomi NPP VIIRS true-color images from 06 January and 07 January [click image to enlarge]](http://pyrocb.ssec.wisc.edu/wp-content/uploads/2016/01/160106-07_suomi_npp_viirs_truecolor_Waroona_Australia_fire_anim.gif)
Suomi NPP VIIRS true-color images from 06 January and 07 January [click image to enlarge]