To summarise a short side thread between Alan and myself:

Foams would potentially have a broad range of impacts, principally by
limiting gas exchange, eg:
* lower CO2 uptake (leading to higher atmos CO2,esp locally)
* reductions in NPP
* reduced DMS output (esp if bubbles don't burst), etc.

Good opportunity for further study.

Additionally, this reminds me a bit of the "plastic sheets in deserts"
idea, which turned out to be problematic

A

On 13 January 2017 at 13:15, Alan Robock <[email protected]> wrote:
> Gabriel, Corey J., Alan Robock, Lili Xia, Brian Zambri, and Ben Kravitz,
> 2017: The G4Foam experiment: Global climate impacts of regional ocean albedo
> modification. Atmos. Chem. Phys., 17, 595-613, doi:10.5194/acp-17-595-2017.
>
> http://www.atmos-chem-phys.net/17/595/2017/
>
> Abstract. Reducing insolation has been proposed as a geoengineering response
> to global warming. Here we present the results of climate model simulations
> of 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
> gyres in the Southern Hemisphere. In theory, this could be accomplished
> using a stable, nondispersive foam, comprised of tiny, highly reflective
> microbubbles. Such a foam has been developed under idealized conditions,
> although deployment at a large scale is presently infeasible. We conducted
> three ensemble members of a simulation (G4Foam) from 2020 through to 2069 in
> which the albedo of the ocean surface is set to 0.15 (an increase of 150 %)
> over the three subtropical ocean gyres in the Southern Hemisphere, against a
> background of the RCP6.0 (representative concentration pathway resulting in
> +6 W m−2 radiative forcing by 2100) scenario. After 2069, geoengineering is
> ceased, and the simulation is run for an additional 20 years. Global mean
> surface temperature in G4Foam is 0.6 K lower than RCP6.0, with statistically
> significant cooling relative to RCP6.0 south of 30° N. There is an increase
> in rainfall over land, most pronouncedly in the tropics during the
> June–July–August season, relative to both G4SSA (specified stratospheric
> aerosols) and RCP6.0. Heavily populated and highly cultivated regions
> throughout the tropics, including the Sahel, southern Asia, the Maritime
> Continent, Central America, and much of the Amazon experience a
> statistically significant increase in precipitation minus evaporation. The
> temperature response to the relatively modest global average forcing of
> −1.5 W m−2 is amplified through a series of positive cloud feedbacks, in
> which more shortwave radiation is reflected. The precipitation response is
> primarily the result of the intensification of the southern Hadley cell, as
> its mean position migrates northward and away from the Equator in response
> to the asymmetric cooling.
>
> --
> 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
>
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