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Title: Marine cloud brightening – as effective without clouds

Journal Article · · Atmospheric Chemistry and Physics (Online)
 [1];  [2]; ORCiD logo [3]; ORCiD logo [4]; ORCiD logo [5];  [4]
  1. Stockholm Univ., Stockholm (Sweden); Univ. of Oslo, Oslo (Norway)
  2. Met Office Hadley Centre, Exeter (United Kingdom)
  3. Univ. of Oslo, Oslo (Norway); Center for International Climate and Environmental Research - Oslo (CICERO), Oslo (Norway)
  4. Univ. of Oslo, Oslo (Norway)
  5. Pacific Northwest National Lab. (PNNL), Richland, WA (United States)

Marine cloud brightening through sea spray injection has been proposed as a climate engineering method for avoiding the most severe consequences of global warming. A limitation of most of the previous modelling studies on marine cloud brightening is that they have either considered individual models or only investigated the effects of a specific increase in the number of cloud droplets. Here we present results from coordinated simulations with three Earth system models (ESMs) participating in the Geoengineering Model Intercomparison Project (GeoMIP) G4sea-salt experiment. Injection rates of accumulation-mode sea spray aerosol particles over ocean between 30°N and 30°S are set in each model to generate a global-mean effective radiative forcing (ERF) of –2.0 W m–2 at the top of the atmosphere. We find that the injection increases the cloud droplet number concentration in lower layers, reduces the cloud-top effective droplet radius, and increases the cloud optical depth over the injection area. We also find, however, that the global-mean clear-sky ERF by the injected particles is as large as the corresponding total ERF in all three ESMs, indicating a large potential of the aerosol direct effect in regions of low cloudiness. The largest enhancement in ERF due to the presence of clouds occur as expected in the subtropical stratocumulus regions off the west coasts of the American and African continents. However, outside these regions, the ERF is in general equally large in cloudy and clear-sky conditions. Lastly, these findings suggest a more important role of the aerosol direct effect in sea spray climate engineering than previously thought.

Research Organization:
Pacific Northwest National Laboratory (PNNL), Richland, WA (United States)
Sponsoring Organization:
USDOE
Grant/Contract Number:
AC05-76RL01830
OSTI ID:
1416676
Report Number(s):
PNNL-SA-126314; 453040135; TRN: US1800958
Journal Information:
Atmospheric Chemistry and Physics (Online), Vol. 17, Issue 21; ISSN 1680-7324
Publisher:
European Geosciences UnionCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 31 works
Citation information provided by
Web of Science

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Cited By (6)

Comparison of the Fast and Slow Climate Response to Three Radiation Management Geoengineering Schemes journal November 2018
Evaluating climate geoengineering proposals in the context of the Paris Agreement temperature goals journal September 2018
The climate effects of increasing ocean albedo: an idealized representation of solar geoengineering journal January 2018
Climate engineering and the ocean: effects on biogeochemistry and primary production journal January 2017
Complementing CO2 emission reduction by solar radiation management might strongly enhance future welfare journal January 2019
Response to marine cloud brightening in a multi-model ensemble journal January 2018

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