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Limits to the Aerosol Indirect Radiative Effect Derived from Observations of Ship Tracks

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Title Limits to the Aerosol Indirect Radiative Effect Derived from Observations of Ship Tracks
Names Coakley, James A., Jr. (creator)
Walsh, Christopher D. (creator)
Date Issued 2002-03 (iso8601)
Abstract One-kilometer Advanced Very High Resolution Radiometer (AVHRR) observations of the effects of ships on
low-level clouds off the west coast of the United States are used to derive limits for the degree to which clouds
might be altered by increases in anthropogenic aerosols. As ships pass beneath low-level clouds, particles from
their plumes serve as condensation nuclei around which new cloud droplets form. The increased droplet concentrations
lead to a decrease in droplet sizes. The change in sizes is manifested as an increase in the reflected
sunlight observed at 3.7 µm in satellite imagery data. Images at 3.7 µm are used in a semiautomated procedure
for identifying polluted portions of clouds and distinguishing them from the nearby unaffected portions. Radiances
at 0.64, 3.7, and 11 µm are used to determine visible optical depths, droplet effective radii, and cloud emission
temperatures for both the polluted and unpolluted portions. The analysis of several hundred 30-km segments of
ship tracks reveals that changes in visible optical depths are about half the values expected, given the changes
observed for the droplet radii and assuming cloud liquid water amount remains constant. Simple radiative transfer
calculations indicate that the shortfall in the optical depth change is unlikely to be due solely to the absorption
by the polluting particles. It is likely that polluted clouds lose liquid water. The equivalent loss is approximately
15%–20% of the initial cloud liquid water.
Genre Article
Identifier Coakley, James A., Christopher D. Walsh, 2002: Limits to the Aerosol Indirect Radiative Effect Derived from Observations of Ship Tracks. Journal of the Atmospheric Sciences, 59(3), 668–680.

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