Eastern Pacific Emitted Aerosol Cloud Experiment

Author:

Russell Lynn M.1,Sorooshian Armin2,Seinfeld John H.3,Albrecht Bruce A.4,Nenes Athanasios5,Ahlm Lars1,Chen Yi-Chun3,Coggon Matthew3,Craven Jill S.3,Flagan Richard C.3,Frossard Amanda A.1,Jonsson Haflidi6,Jung Eunsil4,Lin Jack J.7,Metcalf Andrew R.8,Modini Robin1,Mülmenstädt Johannes1,Roberts Greg9,Shingler Taylor10,Song Siwon4,Wang Zhen10,Wonaschütz Anna11

Affiliation:

1. Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California

2. Department of Chemical and Environmental Engineering, and Department of Atmospheric Sciences, University of Arizona, Tucson, Arizona

3. California Institute of Technology, Pasadena, California

4. Rosenstiel School of Marine and Atmospheric Sciences, University of Miami, Miami, Florida

5. School of Earth and Atmospheric Sciences, and School of Chemical and Biomolecular Engineering, Georgia Institute of Technology, Atlanta, Georgia

6. Center for Interdisciplinary Remotely-Piloted Aerosol Studies, Marina, California

7. School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia

8. California Institute of Technology, Pasadena, California. *CURRENT AFFILIATION: Combustion Research Facility, Sandia National Laboratories, Livermore, California

9. Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California, and Groupe d'études de l'Atmosphère Météorologique, Centre National de la Recherche Scientifique, Toulouse, France

10. Department of Chemical and Environmental Engineering, University of Arizona, Tucson, Arizona

11. Department of Atmospheric Sciences, University of Arizona, Tucson, Arizona

Abstract

Aerosol–cloud–radiation interactions are widely held to be the largest single source of uncertainty in climate model projections of future radiative forcing due to increasing anthropogenic emissions. The underlying causes of this uncertainty among modeled predictions of climate are the gaps in our fundamental understanding of cloud processes. There has been significant progress with both observations and models in addressing these important questions but quantifying them correctly is nontrivial, thus limiting our ability to represent them in global climate models. The Eastern Pacific Emitted Aerosol Cloud Experiment (E-PEACE) 2011 was a targeted aircraft campaign with embedded modeling studies, using the Center for Interdisciplinary Remotely-Piloted Aircraft Studies (CIRPAS) Twin Otter aircraft and the research vessel Point Sur in July and August 2011 off the central coast of California, with a full payload of instruments to measure particle and cloud number, mass, composition, and water uptake distributions. EPEACE used three emitted particle sources to separate particle-induced feedbacks from dynamical variability, namely 1) shipboard smoke-generated particles with 0.05–1-μm diameters (which produced tracks measured by satellite and had drop composition characteristic of organic smoke), 2) combustion particles from container ships with 0.05–0.2-μm diameters (which were measured in a variety of conditions with droplets containing both organic and sulfate components), and 3) aircraft-based milled salt particles with 3–5-μm diameters (which showed enhanced drizzle rates in some clouds). The aircraft observations were consistent with past large-eddy simulations of deeper clouds in ship tracks and aerosol– cloud parcel modeling of cloud drop number and composition, providing quantitative constraints on aerosol effects on warm-cloud microphysics.

Publisher

American Meteorological Society

Subject

Atmospheric Science

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