Thank you Stephen- 
I've posted a  very brief ( under 4 minute ) < a href 
="https://www.youtube.com/watch?v=y-0RRDf8vAI";> slideshow  illustrating 
some of these points:

https://www.youtube.com/watch?v=y-0RRDf8vAI</a>



On Wednesday, April 26, 2017 at 4:12:28 PM UTC-4, Stephen Salter wrote:
>
> Hi all
>
> The change from an untreated cloud to a treated one is much smaller than 
> that from a cloud to clear sky let alone day to night. The contrast change 
> needed to offset double CO2 with 18% low cloud cover is well below the 
> detection threshold of a human eye.  
>
> Stephen
>
> On 26/04/2017 17:40, Russell Seitz wrote:
>
> Andrew wrote    On Sunday, April 23, 2017 at 9:40:00 PM UTC-4: 
>
> I don't think hydrosols will behave like CNN, in terms of their radiative 
>> properties. As I understand it, CCN act to brighten existing cloud cover. 
>> They won't, therefore, work on cloudless days. Likely, relative efficacy 
>> will depend on whether acute or chronic thermal stress is most important. 
>> Furthermore, hydrosols will cause a lasting increase in diffuse radiation. 
>> In terrestrial models, this has impacted NPP. 
>>
>> I'm no expert on this niche - but that's my initial thoughts.
>>
>> Hope it helps
>>
>>
>> It will take field experiments and further modeling  to quantify  the Net 
> Photosynthetic Product  impact  of surface water brightening , but Andrew 
> should bear three things in mind
>
> 1. Backscattering light does not have the  same effect  as casting shade, 
> because most plankton  and algae can absorb light in all directions, 
>
> 2.  Hydrosols scatter the infalling light in all directions,  - they 
> change  the geometry of the euphotic zone in a diffferent manner than 
>  extensive cloud cover.
>
> 3. Doubling surface brightess at high sun angles , from  ~ 7%  to 14% 
> reduces the underwater light flux  by about 7%, which while obviously 
> significant, is a small reduction relative to  full cloud cover, which 
>  often reduces  surface light  more than twice as much, as white clouds in 
> the air can have an albedo of up to .55.- m
>
> It may l accordingly  take as much   NPP research to  sort out the 
> ecological meaning of the  physically uncontroversial cloudy day analogy 
>  as that of CCN shading of overheated seas , both triopical and 
>  circumpolar.
>
>
>
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