Hello All,
Since this is my first post here, I want to firstly thank you all for providing such an excellent, well-informed and well-moderated discussion forum. The "signal to noise ratio" of posts on UMSF is off the charts compared to anywhere else I've been, so I'll try to hold my posts to the same high standards of excellency I routinely see here; which is to say I probably won't be posting very much.
After going a few days without any new images from Rosetta, I turned my attention back to the most recent image release (Sept 19) and decided to see if I could resolve the jets any further:
http://i.imgur.com/44CuMci.jpgPlease excuse the amateurishness of this - I'm just learning image processing, and since it was pre-stitched I wasn't able to correct it with the dark frame helpfully posted a few pages back. I simply mapped the darkest greys in the image to a 3-color gradient to bring as much detail as possible out of the jets.
I purposely did not try to limit this to the outline of the comet, as I wanted to see if there were any visible foreground jets against the shadows. It definitely appears to me as if there is some jet material between the neck and the shadow on the larger lobe, as someone mentioned before. There also appears to be some activity seen off the edge of the larger lobe besides the obvious jets on the neck. One thing I'm curious about - the entire silhouette of the comet seems to have a bit of "fuzz" to it. Is this low level sublimation happening pretty much everywhere? Or maybe light scattering from a thin "atmosphere" of dust? Or just an artifact?
Additionally, I wanted to say that Phil Stooke's comment a few weeks ago regarding the mystery of why comet jets are collimated like this piqued my interest and revealed some good reading, if anyone else is interested:
http://www.chem.ucla.edu/~itkin/publicatio...ticle_crifo.pdf(The J. Crifo paper I think Phil was referring to, suggesting collimation as a result of dust being squeezed between two or more interacting gas cones)
http://www.lpl.arizona.edu/~yelle/eprints/Yelle04a.pdf(Formation of jets in 19/P Borrelly by subsurface geysers)
http://www.lpi.usra.edu/meetings/lpsc2012/pdf/2548.pdf(Perhaps confinement isn't necessary for collimation)
Finally, I have a sort of unrelated question which I'm hoping an expert out there may be able to answer: As I understand it, this paper[1] published earlier this year confirmed the longstanding hypothesis that solar wind bombardment of interplanetary silicate dust can form -OH and H2O due to H+ ions in the solar wind interacting with oxygen in the dust minerals. Is it possible/plausible that a significant amount of H2O content on comets could be a product of this "SW radiolysis" process? If so, would Rosetta have any way of determining this?
[1]
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3918814/ (Detection of solar wind-produced water in irradiated rims on silicate minerals - Bradley et al)