It will be particularly interesting to see what effect no-till agriculture,
etc. have on this aerosol loading. There may be a trade-off between carbon
farming and incidental SRM.

Furthermore, CCN effect also needs to be considered

Andrew Lockley

On 11 May 2017 19:28, "Adrian Tuck" <[email protected]>
wrote:

> This paper seems relevant:
> Radiative forcing from anthropogenic sulfur and organic emissions reaching
> the stratosphere
>
> By:Yu, PF
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/OneClickSearch.do?product=UA&search_mode=OneClickSearch&SID=Q2QrOUagrE3RTYm6Klp&field=AU&value=Yu,%20PF&ut=1000455002&pos=1&excludeEventConfig=ExcludeIfFromFullRecPage>
>  (Yu,
> Pengfei)*[ 1
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/full_record.do?product=UA&search_mode=GeneralSearch&qid=14&SID=Q2QrOUagrE3RTYm6Klp&page=1&doc=5#addressWOS:000385357200064-1>,2
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/full_record.do?product=UA&search_mode=GeneralSearch&qid=14&SID=Q2QrOUagrE3RTYm6Klp&page=1&doc=5#addressWOS:000385357200064-2>
>  ] *
> ; Murphy, DM
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/OneClickSearch.do?product=UA&search_mode=OneClickSearch&SID=Q2QrOUagrE3RTYm6Klp&field=AU&value=Murphy,%20DM&ut=1000516534&pos=2&excludeEventConfig=ExcludeIfFromFullRecPage>
>  (Murphy,
> Daniel M.)*[ 1
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/full_record.do?product=UA&search_mode=GeneralSearch&qid=14&SID=Q2QrOUagrE3RTYm6Klp&page=1&doc=5#addressWOS:000385357200064-1>
>  ] *
> ; Portmann, RW
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/OneClickSearch.do?product=UA&search_mode=OneClickSearch&SID=Q2QrOUagrE3RTYm6Klp&field=AU&value=Portmann,%20RW&ut=2005476262&pos=3&excludeEventConfig=ExcludeIfFromFullRecPage>
>  (Portmann,
> Robert W.)*[ 1
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/full_record.do?product=UA&search_mode=GeneralSearch&qid=14&SID=Q2QrOUagrE3RTYm6Klp&page=1&doc=5#addressWOS:000385357200064-1>
>  ] *
> ; Toon, OB
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/OneClickSearch.do?product=UA&search_mode=OneClickSearch&SID=Q2QrOUagrE3RTYm6Klp&field=AU&value=Toon,%20OB&ut=80086915&pos=4&excludeEventConfig=ExcludeIfFromFullRecPage>
>  (Toon,
> Owen B.)*[ 3
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/full_record.do?product=UA&search_mode=GeneralSearch&qid=14&SID=Q2QrOUagrE3RTYm6Klp&page=1&doc=5#addressWOS:000385357200064-3>,4
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/full_record.do?product=UA&search_mode=GeneralSearch&qid=14&SID=Q2QrOUagrE3RTYm6Klp&page=1&doc=5#addressWOS:000385357200064-4>
>  ] *
> ; Froyd, KD
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/OneClickSearch.do?product=UA&search_mode=OneClickSearch&SID=Q2QrOUagrE3RTYm6Klp&field=AU&value=Froyd,%20KD&ut=2005364445&pos=5&excludeEventConfig=ExcludeIfFromFullRecPage>
>  (Froyd,
> Karl D.)*[ 1
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/full_record.do?product=UA&search_mode=GeneralSearch&qid=14&SID=Q2QrOUagrE3RTYm6Klp&page=1&doc=5#addressWOS:000385357200064-1>,2
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/full_record.do?product=UA&search_mode=GeneralSearch&qid=14&SID=Q2QrOUagrE3RTYm6Klp&page=1&doc=5#addressWOS:000385357200064-2>
>  ] *
> ; Rollins, AW
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/OneClickSearch.do?product=UA&search_mode=OneClickSearch&SID=Q2QrOUagrE3RTYm6Klp&field=AU&value=Rollins,%20AW&ut=1000590829&pos=6&excludeEventConfig=ExcludeIfFromFullRecPage>
>  (Rollins,
> Andrew W.)*[ 1
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/full_record.do?product=UA&search_mode=GeneralSearch&qid=14&SID=Q2QrOUagrE3RTYm6Klp&page=1&doc=5#addressWOS:000385357200064-1>,2
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/full_record.do?product=UA&search_mode=GeneralSearch&qid=14&SID=Q2QrOUagrE3RTYm6Klp&page=1&doc=5#addressWOS:000385357200064-2>
>  ] *
> ; Gao, RS
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/OneClickSearch.do?product=UA&search_mode=OneClickSearch&SID=Q2QrOUagrE3RTYm6Klp&field=AU&value=Gao,%20RS&ut=2005366899&pos=7&excludeEventConfig=ExcludeIfFromFullRecPage>
>  (Gao,
> Ru-Shan)*[ 1
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/full_record.do?product=UA&search_mode=GeneralSearch&qid=14&SID=Q2QrOUagrE3RTYm6Klp&page=1&doc=5#addressWOS:000385357200064-1>
>  ] *
> ; Rosenlof, KH
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/OneClickSearch.do?product=UA&search_mode=OneClickSearch&SID=Q2QrOUagrE3RTYm6Klp&field=AU&value=Rosenlof,%20KH&ut=1000579942&pos=8&excludeEventConfig=ExcludeIfFromFullRecPage>
>  (Rosenlof,
> Karen H.)*[ 1
> <http://apps.webofknowledge.com.iclibezp1.cc.ic.ac.uk/full_record.do?product=UA&search_mode=GeneralSearch&qid=14&SID=Q2QrOUagrE3RTYm6Klp&page=1&doc=5#addressWOS:000385357200064-1>
>  ]*
> View ResearcherID and ORCID
>
> GEOPHYSICAL RESEARCH LETTERS
>
> Volume: 43
>
>
> Issue: 17
>
>
> Pages: 9361-9367
>
> DOI: 10.1002/2016GL070153
>
> Published: SEP 2016
> View Journal Information
> Abstract
>
> Stratospheric aerosols cool the Earth by scattering sunlight. Although
> sulfuric acid dominates the stratospheric aerosol, this study finds that
> organic material in the lowermost stratosphere contributes 30-40% of the
> nonvolcanic stratospheric aerosol optical depth (sAOD). Simulations
> indicate that nonvolcanic sAOD has increased 77% since 1850. Stratospheric
> aerosol accounts for 21% of the total direct aerosol radiative forcing
> (which is negative) and 12% of the total aerosol optical depth (AOD)
> increase from organics and sulfate. There is a larger stratospheric
> influence on radiative forcing (i.e., 21%) relative to AOD (i.e., 12%)
> because an increase of tropospheric black carbon warms the planet while
> stratospheric aerosols (including black carbon) cool the planet. Radiative
> forcing from nonvolcanic stratospheric aerosol mass of anthropogenic
> origin, including organics, has not been widely considered as a significant
> influence on the climate system.
>
>

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