Hi, Peter,

The evaporation reduction due to cooler environment would balance the
effect of the reduced precip to some extent. The change of
evapotranspiration may help. I think more studies are needed to work on all
the details.

Lili

On Thu, Feb 11, 2016 at 6:38 PM, Peter Irvine <[email protected]> wrote:

> Interesting study Lili! One surprise for me was the large increases in
> productivity in the amazon - do you think that the temperature reduction
> and reduced evaporative demand more than make up for the reduced precip?
>
> I'm looking forward to the next-gen of nitrogen-limited models getting
> into this debate, they produced a different sign of change in Susanne's
> study. Cooler was worse for productivity in the tropics rather than better,
> despite the factors you identify in your study due to the greater
> availability of nitrogen in the warmer soils. This effect is obviously
> missing from models without interactive nitrogen cycles
>
> Pete
>
> Pete
>
> Peter J. Irvine
>
> Postdoctoral Fellow
> Harvard University
> John A. Paulson School of Engineering and Applied Sciences (SEAS)
> One Brattle Square, Office 492, Cambridge, MA 02138, USA
>
> Email: [email protected] <[email protected]>
> https://scholar.google.de/citations?user=7asLSCEAAAAJ&hl=en
>
> On 11 February 2016 at 15:35, Lili Xia <[email protected]> wrote:
>
>> Hi, Peter,
>>
>> I think there are couples things which make the results different: (1) G1
>> doesn't have diffuse radiation increasing; (2) CLM in Xia et al. is CLM-SP
>> instead of CLM-CN; (3) the climate forcing is quite different.
>>
>> Lili
>>
>> On Thu, Feb 11, 2016 at 12:11 PM, p.j.irvine <[email protected]>
>> wrote:
>>
>>> Hi,
>>>
>>> I wouldn't be so sure that this is a forcing difference. There are VERY
>>> large differences in the model response to high CO2 scenarios, with much
>>> smaller differences between SRM and no-SRM scenarios. These arise because
>>> different factors act to limit vegetation productivity in the different
>>> models. In Susanne Glienke's paper the only models which included a
>>> nitrogen cycle in GeoMIP, a version of CLM, found the opposite trend to
>>> that reported in Xia et al. They found greater tropical productivity in the
>>> non-SRM scenario than the SRM scenario and only a small CO2 fertilization
>>> effect, likely arising from the fact that nitrogen is the limiting factor
>>> in these regions and it is recycled more rapidly in warmer soils boosting
>>> NPP.
>>>
>>> I think it's still early days in the study of the vegetation response to
>>> SRM.
>>>
>>> cheers,
>>>
>>> Pete
>>>
>>> On Thursday, 11 February 2016 08:44:01 UTC-5, Alan Robock wrote:
>>>>
>>>> Dear Bala,
>>>>
>>>> Actually in our paper we say:
>>>>
>>>> Kalidindi et al. (2015) showed that with a 20 Tg sulfate aerosol
>>>> (SO4) stratospheric loading to balance the radiative forcing
>>>> of 2 xCO2, broadband diffuse radiation would increase
>>>> by 11.2 Wm-2 compared with the reference run. However
>>>> they used a very unrealistic stratospheric aerosol distribution,
>>>> with a very small effective radius of 0.17 μm and uniform
>>>> geographical distribution.
>>>>
>>>> So we did different experiments, and we used a much more "realistic"
>>>> aerosol size and space distribution.  I think the differences in the
>>>> results are because of the forcing and not the models.
>>>>
>>>> Alan
>>>>
>>>> Alan Robock, Distinguished Professor
>>>>   Editor, Reviews of Geophysics
>>>> Department of Environmental Sciences             Phone: +1-848-932-5751
>>>> Rutgers University                                 Fax: +1-732-932-8644
>>>> 14 College Farm Road                  E-mail: [email protected]
>>>> New Brunswick, NJ 08901-8551  USA     http://envsci.rutgers.edu/~robock
>>>> ☮ http://twitter.com/AlanRobock
>>>> Watch my 18 min TEDx talk at http://www.youtube.com/watch?v=qsrEk1oZ-54
>>>>
>>>> On 2/10/2016 10:32 PM, Govindasamy Bala wrote:
>>>>
>>>> Interesting result. The conclusions seem to depend on model
>>>> configurations.
>>>>
>>>> Our paper published last year in Climate Dynamics (attached) did not
>>>> find any such benefit from the enhanced diffused radiation because of the
>>>> offset from a reduction in direct light. In fact we found a net reduction
>>>> in GPP of about 1 PgC
>>>>
>>>> Looks like Multi-model intercomparison would be needed to resolve this
>>>> issue.
>>>>
>>>> On Wed, Feb 10, 2016 at 7:39 PM, Alan Robock <[email protected]
>>>> > wrote:
>>>>
>>>>> Our most recent paper has just been published:
>>>>>
>>>>> Xia, L., Robock, A., Tilmes, S., and Neely III, R. R.: Stratospheric
>>>>> sulfate geoengineering could enhance the terrestrial photosynthesis rate,
>>>>> Atmos. Chem. Phys., 16, 1479-1489, doi:10.5194/acp-16-1479-2016, 2016.
>>>>>
>>>>> http://www.atmos-chem-phys.net/16/1479/2016/
>>>>>
>>>>> --
>>>>> Alan Robock
>>>>>
>>>>> Alan Robock, Distinguished Professor
>>>>>   Editor, Reviews of Geophysics
>>>>> Department of Environmental Sciences             Phone:
>>>>> +1-848-932-5751
>>>>> Rutgers University                                 Fax:
>>>>> +1-732-932-8644
>>>>> 14 College Farm Road                  E-mail:
>>>>> [email protected]
>>>>> New Brunswick, NJ 08901-8551  USA
>>>>> <http://envsci.rutgers.edu/%7Erobock>http://envsci.rutgers.edu/~robock
>>>>> ☮ http://twitter.com/AlanRobock
>>>>> Watch my 18 min TEDx talk at
>>>>> http://www.youtube.com/watch?v=qsrEk1oZ-54
>>>>>
>>>>> --
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>>>>> For more options, visit https://groups.google.com/d/optout.
>>>>>
>>>>
>>>>
>>>>
>>>> --
>>>> With Best Wishes,
>>>>
>>>> -------------------------------------------------------------------
>>>> G. Bala
>>>> Professor
>>>> Center for Atmospheric and Oceanic Sciences
>>>> Indian Institute of Science
>>>> Bangalore - 560 012
>>>> India
>>>>
>>>> Tel: +91 80 2293 3428; +91 80 2293 2505
>>>> Fax: +91 80 2360 0865; +91 80 2293 3425
>>>> Email: [email protected]; [email protected]
>>>> Web:http://caos.iisc.ernet.in/faculty/gbala/gbala.html
>>>> -------------------------------------------------------------------
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>>>>
>>>> --
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>>>
>>
>>
>

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