I've been doing some research on the fate of methane recently.  It appears
the chemistry is made substantially more complex by the interaction of
pollution and possible geoengineering.

I'm writing to ask if anyone has insights into this, or opinions on the
matter.

Particularly, if SRM with sulfur is used, it appears that the sulfur
precursors compete with methane for reagents. Has this effect been factored
into the calculations on the efficacy of SRM?  No use dumping sulfur up into
the stratophere if there's nothing left for it to react with, or if the
effect on the lifetime of methane outweighs the SRM effect.  ( useful link
http://www.sciencemag.org/cgi/content/abstract/326/5953/716 )

Furthermore, there is an added complexity in that the source of the radicals
needed to oxidise methane is ultimately ozone.  I understand that there is
still significant depletion of stratospheric ozone, and thus it may be the
case that the life of methane in the atmosphere is longer than was
historically the case.  As ozone is itself a GHG, does anyone have opinions
on using O3 production and addition to the atmosphere as a geoengineering
measure, with the aim of restoring the ozone layer and also encouraging the
degradation of methane?  Would the GWP of O3 outweigh that of the methane it
ultimately destroys?

Finally, I'm interested to know if anyone has particular opinions or
insights into the chemistry of radicals and reactive oxygen species in the
atmosphere.  I'm interested in the possibility of creating and using such
chemicals to degrade methane.  NOx may also offer options.  Can such
chemicals be easily and safely created on a large scale?  Can they be added
to the atmosphere safely, and left to diffuse?  I feel a little bit of a
dunce asking these questions, but my knowledge of atmospheric photochemistry
simply isn't good enough to avoid making basic mistakes in this regard.

I'd really appreciate any comments, ideas and assistance people are able to
offer.

Thanks!

A

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