Marine cloud brightening

Author:

Latham John12,Bower Keith2,Choularton Tom2,Coe Hugh2,Connolly Paul2,Cooper Gary3,Craft Tim4,Foster Jack3,Gadian Alan5,Galbraith Lee6,Iacovides Hector4,Johnston David6,Launder Brian4,Leslie Brian6,Meyer John6,Neukermans Armand6,Ormond Bob6,Parkes Ben5,Rasch Phillip7,Rush John6,Salter Stephen3,Stevenson Tom3,Wang Hailong7,Wang Qin6,Wood Rob8

Affiliation:

1. National Centre for Atmospheric Research, Boulder, CO 80301, USA

2. School of Earth and Atmospheric Sciences, University of Manchester, Manchester M13 9PL

3. Department of Engineering, University of Edinburgh, Edinburgh EH9 3JL, UK

4. MACE, University of Manchester, Manchester M13 9PL, UK

5. NCAS, SEE, University of Leeds, Leeds LS2 9JT, UK

6. FICER, CA, USA

7. Climate Science, Pacific Northwest National Laboratory, Richland, WA 99352, USA

8. Department of Atmospheric Sciences, University of Washington, Seattle, WA 98105, USA

Abstract

The idea behind the marine cloud-brightening (MCB) geoengineering technique is that seeding marine stratocumulus clouds with copious quantities of roughly monodisperse sub-micrometre sea water particles might significantly enhance the cloud droplet number concentration, and thereby the cloud albedo and possibly longevity. This would produce a cooling, which general circulation model (GCM) computations suggest could—subject to satisfactory resolution of technical and scientific problems identified herein—have the capacity to balance global warming up to the carbon dioxide-doubling point. We describe herein an account of our recent research on a number of critical issues associated with MCB. This involves (i) GCM studies, which are our primary tools for evaluating globally the effectiveness of MCB, and assessing its climate impacts on rainfall amounts and distribution, and also polar sea-ice cover and thickness; (ii) high-resolution modelling of the effects of seeding on marine stratocumulus, which are required to understand the complex array of interacting processes involved in cloud brightening; (iii) microphysical modelling sensitivity studies, examining the influence of seeding amount, seed-particle salt-mass, air-mass characteristics, updraught speed and other parameters on cloud–albedo change; (iv) sea water spray-production techniques; (v) computational fluid dynamics studies of possible large-scale periodicities in Flettner rotors; and (vi) the planning of a three-stage limited-area field research experiment, with the primary objectives of technology testing and determining to what extent, if any, cloud albedo might be enhanced by seeding marine stratocumulus clouds on a spatial scale of around 100×100 km. We stress that there would be no justification for deployment of MCB unless it was clearly established that no significant adverse consequences would result. There would also need to be an international agreement firmly in favour of such action.

Publisher

The Royal Society

Subject

General Physics and Astronomy,General Engineering,General Mathematics

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