First let me congratulate you --the  2011 *Climatic Change * paper you 
kindly cite:
https://dash.harvard.edu/bitstream/handle/1/4737323/Seitz_BrightWater.pdf?sequence=1
 called for just such for model intercomparisons as you present:

>
> "To determine the priority appropriate for study and potential deployment 
> of hydrosols, a comparison is needed of advantages and disadvantages with 
> respect to other approaches, such as stratospheric aerosol deployment, 
> augmentation of cloud cover , and direct steps to reduce or reverse 
> increases in the CO2 concentration .


However, I must point out that  while your results are presented as 


"  a "unique Geoengineering Model Intercomparison Project Testbed 
> experiment to investigate the benefits and risks of a scheme that would 
> brighten certain oceanic regions. The National Center for Atmospheric 
> Research CESM CAM4-Chem global climate model was modified to simulate a 
> scheme in which the albedo of the ocean surface is increased over the 
> subtropical ocean.... " 


"Unique" means singular,  and previous  NCAR model simulations have 
examined  the climate impact of  air bubble  modulation of surface water 
albedo, witness the 2011 paper you cite:

>
> "To calculate the potential effects of microbubble injection, the CAM 3.1 
> global
> circulation model developed at the National Center for Atmospheric Research
> (University Consortium on Atmospheric Research 2008) has been used to 
> simulate
> the climate’s response to an increase in global ocean albedo. Baseline 
> simulations
> were conducted the CO2 concentration at preindustrial (280 ppmv), current
> (390 ppmv), and double current (780 ppmv) levels. Using the doubled CO2 
> case
> (780 ppmv) as the control, hydrosol simulations were conducted to examine 
> the
> counter-balancing effects of increasing ocean albedo by 0.01 and 0.05 
> above its
> present average value"



You also  note " A cooler ocean would increase the net carbon sink."

Can you  please quantify  this?  Dan Schrag has told me  carbonate 
buffering in sea water would  minimize the carbon sequestration  impact of 
 lowering SST  with microbubbles.


>

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