Valentina Zharkova is very well known for publishing bogus science on the 
connection between solar activity and climate.
Her last paper in SciRep was retracted one week after publication 
https://www.nature.com/articles/s41598-020-61020-3

The one article linked is an editorial in a journal whose scientific scope is “ 
medical physiology of body temperature regulation,”

Further, there is plenty of discussion of the relationship between the Maunder 
Minimum and the little ice age (which was also most likely a local, NH 
phenomena), as the onset of the MM happened in the middle of the ice age. See 
for instance this study discussing the causes of the LIA.

https://news.agu.org/press-release/unusual-volcanic-episode-rapidly-triggered-little-ice-age-researchers-find/

So no, the Sun is very, very unlikely to be able to save us from our own mess.



> On 14 Mar 2021, at 08:11, SALTER Stephen <[email protected]> wrote:
> 
> 
> Hi All
>  
> I got this from Wikipedia
>  
> <image001.jpg>
>  
>  
>  
>  
> Stephen Salter
> Emeritus Professor of Engineering Design
> School of Engineering
> Mayfield Road  EH9 3 DW
> University of Edinburgh
> Scotland.
> Tel 0131 662 1180
>  
> From: NORTHCOTT Michael <[email protected]> 
> Sent: 14 March 2021 12:02
> To: SALTER Stephen <[email protected]>; [email protected]; 
> geoengineering <[email protected]>; 
> [email protected] <[email protected]> 
> <[email protected]>
> Cc: Alan Gadian <[email protected]>
> Subject: Re: [geo] Grand Solar Minimum 2020-2050 ends case for geo engineering
>  
> Hi all
>  
> Seeing that sunspots are down 77% 2019-20 and a paper has already been 
> published in the journal Temperature indicating that a new Grand Solar 
> Minimum has begun and will cause cooling of 1 degree C until 2050 the case 
> for geoengineering is surely over. The last GSM ended in 1821 after causing 
> glaciers to advance and giving rise to famines because of significantly 
> reduced crop production. See Valentina Zharkova, ‘Modern Grand Solar Minimum 
> will lead to
> terrestrial cooling’ Temperature 7.3 2020. 
>  
> https://doi.org/10.1080/23328940.2020.1796243
>  
> Michael Northcott
> Emeritus Professor of Ethics
> University of Edinburgh
>  
> From: [email protected] <[email protected]> on 
> behalf of SALTER Stephen <[email protected]>
> Sent: Saturday, March 13, 2021 00:20
> To: [email protected]; geoengineering; 
> [email protected] <[email protected]>
> Cc: Alan Gadian
> Subject: RE: [geo] The response of terrestrial ecosystem carbon cycling under 
> different aerosol-based radiation management geoengineering
>  
> Hi All
>  
> Like several previous workers the authors of the paper, use the 
> accumulation-mode spread of aerosol size between latitudes 45 N and 45 S all 
> the time at a rate to offset RCP 8.5.  
>  
> The effort or cost needed for marine cloud brightening is in proportion the 
> volume of water that we have to filter and spray.  The value of what the 
> spray does depends on the number of successful nucleations.
>  
> We think that the right size of aerosol salt particle has a mass of 10^ -14 
> grams.  If it was a completely dry sphere its diameter would be about 200 
> nanometres but it is more likely to be a brick shape in strong brine.
>  
> The graph below from Wikipedia shows that 200 nanometres is at the bottom of 
> the slope of the accumulation mode. The top of the accumulation mode is at 
> about 1.2 microns.  The cube of the ratio of diameters is 216. This means 
> that using the full spread of the accumulation mode will involve making some 
> condensation nuclei far bigger, and so more expensive, than we actually need.
>  
> <image003.jpg>
>  
> As second reason is that the Stokes drag tending to accelerate a drop in 
> turbulent flow on depends on diameter not projected area while the inertia 
> opposing acceleration depends on the cube.  If drops of spray in a turbulent 
> air stream have a wide spread of inertias they will also have a wide spread 
> of relative velocities and so more chance of coalescence.
>  
> A third reason in favour of a monodisperse spray is that heavier condensation 
> nuclei will nucleate at a lower relative humidity than lighter ones.  This 
> will suck water vapour from the surrounding air and so reduce its relative 
> humidity and make it harder for the small ones to nucleate.  The transfer 
> rate of water vapour depends of vapour pressure difference and surface area.  
>  Being big earlier than rival nuclei gives a further advantage.  This is the 
> same with wolves and hyenas.
>  
> It might be convenient for climate modellers to use the wide spread of 
> standard, naturally-occurring aerosol built into modelling software but 
> please, please, please could somebody try monodisperse spray to avoid errors 
> of 200.
> Please also give us  an opinion about whether 10 ^ -14 grams is the right 
> choice.  Can we reduce coalescence even further with electrostatic charge?
>  
>  
> Stephen Salter
> Emeritus Professor of Engineering Design
> School of Engineering
> Mayfield Road  EH9 3 DW
> University of Edinburgh
> Scotland.
> Tel 0131 662 1180
>  
> From: [email protected] <[email protected]> On 
> Behalf Of Andrew Lockley
> Sent: 11 March 2021 21:14
> To: geoengineering <[email protected]>; 
> [email protected] <[email protected]> 
> <[email protected]>
> Subject: [geo] The response of terrestrial ecosystem carbon cycling under 
> different aerosol-based radiation management geoengineering
>  
> This email was sent to you by someone outside the University.
> You should only click on links or attachments if you are certain that the 
> email is genuine and the content is safe.
> 
> https://esd.copernicus.org/articles/12/313/2021/
>  
> Earth Syst. Dynam., 12, 313–326, 2021
> https://doi.org/10.5194/esd-12-313-2021
> © Author(s) 2021. This work is distributed under the Creative Commons 
> Attribution 4.0 License.
>  
> Research article | 11 Mar 2021
>  
> The response of terrestrial ecosystem carbon cycling under different 
> aerosol-based radiation management geoengineering
> Hanna Lee et al.
> Show author details
> Received: 20 Jul 2020 – Discussion started: 31 Jul 2020 – Revised: 09 Feb 
> 2021 – Accepted: 10 Feb 2021 – Published: 11 Mar 2021
> Abstract
> Geoengineering has been discussed as a potential option to offset the global 
> impacts of anthropogenic climate change and at the same time reach the global 
> temperature targets of the Paris Agreement. Before any implementation of 
> geoengineering, however, the complex natural responses and consequences of 
> such methods should be fully understood to avoid any unexpected and 
> potentially degrading impacts. Here we assess the changes in ecosystem carbon 
> exchange and storage among different terrestrial biomes under three 
> aerosol-based radiation management methods with the baseline of RCP8.5 using 
> an Earth system model (NorESM1-ME). All three methods used in this study 
> (stratospheric aerosol injection, marine sky brightening, cirrus cloud 
> thinning) target the global mean radiation balance at the top of the 
> atmosphere to reach that of the RCP4.5 scenario. The three radiation 
> management (RM) methods investigated in this study show vastly different 
> precipitation patterns, especially in the tropical forest biome. 
> Precipitation differences from the three RM methods result in large 
> variability in global vegetation carbon uptake and storage. Our findings show 
> that there are unforeseen regional consequences under geoengineering, and 
> these consequences should be taken into account in future climate policies as 
> they have a substantial impact on terrestrial ecosystems. Although changes in 
> temperature and precipitation play a large role in vegetation carbon uptake 
> and storage, our results show that CO2 fertilization also plays a 
> considerable role. We find that the effects of geoengineering on vegetation 
> carbon storage are much smaller than the effects of mitigation under the 
> RCP4.5 scenario (e.g., afforestation in the tropics). Our results emphasize 
> the importance of considering multiple combined effects and responses of land 
> biomes while achieving the global temperature targets of the Paris Agreement 
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