IMAGE PROCESSING GALLERY
For those of you who have contributed – thank you! Your labors of love have illustrated articles about Juno, Jupiter and JunoCam. Your products show up in all sorts of places. I have used them to report to the scientific community. We are writing papers for scientific journals and using your contributions – always with appropriate attribution of course. Some creations are works of art and we are working out ways to showcase them as art.
If you have a favorite “artist” you can create your own gallery. Click on “Submitted by” on the left, select your favorite artist(s), and then click on “Filter”. For other tips about the gallery click on the “Gallery Organization” tab.
We have a methane filter, included for the polar science investigation, that is almost at the limits of our detector’s wavelength range. To get enough photons for an image we need to use a very long exposure. In some images this results in scattered light in the image. For science purposes we will simply crop out the portions of the image that include this artifact. Work is in progress to determine exactly what conditions cause stray light problems so that this can be minimized for future imaging.
The JunoCam images are identified by a small spacecraft icon. You will see both raw and processed versions of the images as they become available. The JunoCam movie posts have too many images to post individually, so we are making them available for download in batches as zip files.
You can filter the gallery by many different characteristics, including by Perijove Pass, Points of Interest and Mission Phase.
A special note about the Earth Flyby mission phase images: these were acquired in 2013 when Juno flew past Earth. Examples of processed images are shown; most contributions are from amateurs.
The spacecraft spin rate would cause more than a pixel's worth of image blurring for exposures longer than about 3.2 milliseconds. For the illumination conditions at Jupiter such short exposures would result in unacceptably low SNR, so the camera provides Time-Delayed-Integration (TDI). TDI vertically shifts the image one row each 3.2 milliseconds over the course of the exposure, cancelling the scene motion induced by rotation. Up to about 100 TDI steps can be used for the orbital timing case while still maintaining the needed frame rate for frame-to-frame overlap. For Earth Flyby the light levels are high enough that TDI is not needed except for the methane band and for nightside imaging.
Junocam pixels are 12 bits deep from the camera but are converted to 8 bits inside the instrument using a lossless "companding" table, a process similar to gamma correction, to reduce their size. All Junocam products on the missionjuno website are in this 8-bit form as received on Earth. Scientific users interested in radiometric analysis should use the "RDR" data products archived with the Planetary Data System, which have been converted back to a linear 12-bit scale.
PJ18, southern circumpolar cyclones 40 minutes forth and 40 minutes back, displayed together in 0.8 seconds
No, the storms on Jupiter aren't oscillating forth and back.
The animated gif is showing the southern cluster of Jupiter's circumpolar cyclones (CPCs). It is a 6000-fold timelapsed animation running forth and back in time, in order to look smoother for the human eye.
Four of the CPCs are well visible, two are located deep in the twilight zone, and difficult to resolve. Note the varying symmetrical properties of the CPC dynamics. Some rotate pretty rotational symmetric, others are struggling with embedded storm systems, some rotate like a solid body around their core, others rotate the higher frequency the closer to their center.
The gap between two of the CPCs has opened to more than 120 degrees, and it is now populated by a poorly resolved anticyclone close to the central CPC, and a small roundish filamentary folded region (FFR), candidate for a young CPC, which might eventually complete a CPC hexagon around the central southern CPC.
The southern cluster of CPCs is surrounded by many cyclonic and anticyclonic storms.
Note the shading of the bluish haze near the terminator moving with changing illumination.
Each of the 20 frames of the animation is a weighted mean of two images, each of which is stacked from three heavily processed equidistant azimuthal south polar maps. The image noise level varying with color was considered. The animation is based on a set of ten raw JunoCam images taken during Juno's Perijove-18 flyby.
The scale of the animated map is 60 pixels per planetocentric degree latitude.