If you use GM or breeding to boost aerosol levels it might be harmful.

A
On 27 Feb 2014 15:29, "Simone Tilmes" <[email protected]> wrote:

> VOC's are emitted from the forest and have an impact on climate, however,
> how much they really change with increasing CO2 levels is questionable and
> may go in both directions. To really change the amount of aerosols that
> build up over the forests, afforestation would be the way to go. That
> certainly would be a good way to "manipulate climate" because more forest
> increases the CO2 uptake and it maybe more important for climate than the
> change in aerosols. I don't see the health effect playing a role, is it
> unhealthy to walk through a forest?
>
> Simone
>
>>
>> Poster's note : I've been wondering about whether this mechanism can be
>> manipulated for geoengineering purposes. David Keith is concerned about
>> health effects, suggesting they will outweigh relative benefits.
>>
>> http://www.nature.com/nature/journal/v506/n7489/full/nature13032.html
>>
>> A large source of low-volatility secondary organic aerosol
>>
>> Mikael Ehn, Joel A. Thornton, Einhard Kleist, Mikko Sipilä, Heikki
>> Junninen, Iida Pullinen, Monika Springer, Florian Rubach, Ralf Tillmann,
>> Ben Lee,Felipe Lopez-Hilfiker, Stefanie Andres, Ismail-Hakki Acir, Matti
>> Rissanen, Tuija Jokinen, Siegfried Schobesberger, Juha Kangasluoma, Jenni
>> Kontkanen,Tuomo Nieminen, Theo Kurtén, Lasse B. Nielsen,Solvejg Jørgensen,
>> Henrik G. Kjaergaard, Manjula Canagaratna, Miikka Dal Maso et al.
>>
>> Nature 506, 476–479 (27 February 2014)doi:10.1038/nature13032
>>
>> Published online 26 February 2014
>>
>> Article tools
>>
>> Forests emit large quantities of volatile organic compounds (VOCs) to the
>> atmosphere. Their condensable oxidation products can form secondary organic
>> aerosol, a significant and ubiquitous component of atmospheric aerosol,
>> which is known to affect the Earth’s radiation balance by scattering solar
>> radiation and by acting as cloud condensation nuclei. The quantitative
>> assessment of such climate effects remains hampered by a number of factors,
>> including an incomplete understanding of how biogenic VOCs contribute to
>> the formation of atmospheric secondary organic aerosol. The growth of newly
>> formed particles from sizes of less than three nanometres up to the sizes
>> of cloud condensation nuclei (about one hundred nanometres) in many
>> continental ecosystems requires abundant, essentially non-volatile organic
>> vapours, but the sources and compositions of such vapours remain unknown.
>> Here we investigate the oxidation of VOCs, in particular the terpene
>> α-pinene, under atmospherically relevant conditions in chamber experiments.
>> We find that a direct pathway leads from several biogenic VOCs, such as
>> monoterpenes, to the formation of large amounts of extremely low-volatility
>> vapours. These vapours form at significant mass yield in the gas phase and
>> condense irreversibly onto aerosol surfaces to produce secondary organic
>> aerosol, helping to explain the discrepancy between the observed
>> atmospheric burden of secondary organic aerosol and that reported by many
>> model studies. We further demonstrate how these low-volatility vapours can
>> enhance, or even dominate, the formation and growth of aerosol particles
>> over forested regions, providing a missing link between biogenic VOCs and
>> their conversion to aerosol particles. Our findings could help to improve
>> assessments of biosphere–aerosol–climate feedback mechanisms, and the air
>> quality and climate effects of biogenic emissions generally.
>>
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>
>

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