Atmos. Chem. Phys. Discuss., 11, 6415-6455, 2011
www.atmos-chem-phys-discuss.net/11/6415/2011/
doi:10.5194/acpd-11-6415-2011
© Author(s) 2011. This work is distributed
under the Creative Commons Attribution 3.0 License.
Review Status
This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
Microphysical, macrophysical and radiative signatures of volcanic aerosols in trade wind cumulus observed by the A-Train
T. Yuan1,2, L. A. Remer2, and H. Yu2,3
1Joint Center for Earth Systems Technology, University of Maryland, Baltimore County, Baltimore, MD, USA
2Laboratory for Atmospheres, NASA Goddard Space Flight Center, Greenbelt, MD, USA
3Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD, USA

Abstract. Increased aerosol concentrations can raise planetary albedo not only by reflecting sunlight and increasing cloud albedo, but also by changing cloud amount. However, detecting aerosol effect on cloud amount has been elusive to both observations and modeling due to potential buffering mechanisms and convolution of meteorology. Here through a natural experiment provided by long-term degassing of a low-lying volcano and use of A-Train satellite observations, we show aerosols are associated strongly with modification of trade cumulus cloud fields including decreased droplet size, decreased precipitation efficiency and increased cloud amount. We also demonstrate that the observed microphysical and macrophysical changes cannot be explained by synoptic meteorology or the orographic effect of the Hawaiian Islands. The "total shortwave aerosol forcing", resulting from direct and indirect forcings including both cloud albedo and cloud amount, is almost an order of magnitude higher than aerosol direct forcing alone. The precipitation reduction associated with enhanced aerosol leads to large changes in the energetics of air-sea exchange. Our results represent the first observational evidence of large-scale increase of cloud amount due to aerosols in a trade cumulus regime, which can be used to constrain the representation of aerosol-cloud interactions in climate models. The findings also have implications for volcano-climate interactions and climate mitigation research.

Citation: Yuan, T., Remer, L. A., and Yu, H.: Microphysical, macrophysical and radiative signatures of volcanic aerosols in trade wind cumulus observed by the A-Train, Atmos. Chem. Phys. Discuss., 11, 6415-6455, doi:10.5194/acpd-11-6415-2011, 2011.
 
Search ACPD
Discussion Paper
    XML
    Citation
    Final Revised Paper
    Share