Poster's note: relevant to MCB, and to an extent to cirrus stripping and
SAI rainout

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http://advances.sciencemag.org/content/1/6/e1500157.full-text.pdf+html
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Natural aerosols explain seasonal and spatial patterns of Southern Ocean
cloud albedo

Daniel T. McCoy
Susannah M. Burrows
Robert Wood1,
Daniel P. Grosvenor
Scott M. Elliott
Po-Lun Ma
Phillip J. Rasch
Dennis L. Hartmann

E-mail: [email protected] (D.T.M.); [email protected] (S.M.B.)

Science Advances 17 Jul 2015:
Vol. 1, no. 6, e1500157
DOI: 10.1126/sciadv.1500157

Abstract

Atmospheric aerosols, suspended solid and liquid particles, act as
nucleation sites for cloud drop formation, affecting clouds and cloud
properties—ultimately influencing the cloud dynamics, lifetime, water path,
and areal extent that determine the reflectivity (albedo) of clouds. The
concentration Nd of droplets in clouds that influences planetary albedo is
sensitive to the availability of aerosol particles on which the droplets
form. Natural aerosol concentrations affect not only cloud properties
themselves but also modulate the sensitivity of clouds to changes in
anthropogenic aerosols. It is shown that modeled natural aerosols,
principally marine biogenic primary and secondary aerosol sources, explain
more than half of the spatiotemporal variability in satellite-observed Nd.
Enhanced Nd is spatially correlated with regions of high chlorophyll a, and
the spatiotemporal variability in Nd is found to be driven primarily by
high concentrations of sulfate aerosol at lower Southern Ocean latitudes
(35o to 45oS) and by organic matter in sea spray aerosol at higher
latitudes (45o to 55oS). Biogenic sources are estimated to increase the
summertime mean reflected solar radiation in excess of 10 W m–2 over parts
of the Southern Ocean, which is comparable to the annual mean increases
expected from anthropogenic aerosols over heavily polluted regions of the
Northern Hemisphere.

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