Effects of Sea Salt Aerosol Emissions for Marine Cloud Brightening on Atmospheric Chemistry: Implications for Radiative Forcing-Reference-Cited by-同舟云学术

Effects of Sea Salt Aerosol Emissions for Marine Cloud Brightening on Atmospheric Chemistry: Implications for Radiative Forcing

Published:2020-02-10 Issue:4 Volume:47 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophysical Research Letters

Author:

Horowitz Hannah M.¹²³^ORCID,Holmes Christopher⁴^ORCID,Wright Alicia²,Sherwen Tomás⁵⁶^ORCID,Wang Xuan⁷⁸^ORCID,Evans Mat⁵⁶^ORCID,Huang Jiayue²,Jaeglé Lyatt²^ORCID,Chen Qianjie²⁹^ORCID,Zhai Shuting²^ORCID,Alexander Becky²

Affiliation:

1. JISAO University of Washington Seattle WA USA

2. Department of Atmospheric Sciences University of Washington Seattle WA USA

3. Department of Civil and Environmental Engineering University of Illinois at Urbana‐Champaign Urbana IL USA

4. Department of Earth, Ocean and Atmospheric Science Florida State University Tallahassee FL USA

5. Department of Chemistry University of York York UK

6. Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry University of York York UK

7. School of Energy and Environment City University of Hong Kong Hong Kong

8. John A. Paulson School of Engineering and Applied Sciences Harvard University Cambridge MA USA

9. Department of Chemistry University of Michigan Ann Arbor MI USA

Funder

National Aeronautics and Space Administration

National Science Foundation

Washington Space Grant Consortium

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL085838

Reference54 articles.

1. Marine cloud brightening – as effective without clouds

2. Isotopic constraints on the formation pathways of sulfate aerosol in the marine boundary layer of the subtropical northeast Atlantic Ocean

3. Sulfate formation in sea-salt aerosols: Constraints from oxygen isotopes

4. Sea‐salt injections into the low‐latitude marine boundary layer: The transient response in three Earth system models

5. Sensitivity to deliberate sea salt seeding of marine clouds – observations and model simulations

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