Limits to Cloud Susceptibility
James A. Coakley, Jr.
Abstract:
1-km AVHRR, VIRS, and MODIS observations of ship tracks in low-
level clouds off the west coast of the U.S. will be used to derive
limits for the degree to which clouds might be altered by increases in
anthropogenic aerosols. The goal is to analyze several thousand ship
tracks to determine whether changes in droplet radii, visible optical
depths, and cloud top altitudes are consistent with the pre-existing
optical depths, radii, and altitudes as anticipated for fixed liquid
water paths. A unique feature of this study is that it will rely only
on observations for which the ~ 1-km field of view of the satellite
radiometer is overcast for both the portions of the cloud affected by
the ship and the nearby portions of the cloud that are unaffected. Use
of only the overcast pixels will greatly reduce the variability in the
observed radiances through which the effects due to the ships must be
extracted. Changes due to ships will be examined as functions of
distance from the start of the track to distinguish between freshly
contaminated clouds and clouds that have been affected for several
hours. By allowing for effects due to dispersion, the portions of the
tracks far from the ship should reflect influences, if any, of the
changes in droplet sizes and numbers on the interaction of the cloud
with its environment. The frequency with which ship tracks are found in
pixels overcast by marine stratus but the layer is broken in the nearby
surrounding region will be used as a measure of effects due to the
changes in droplet sizes. Regions where ship tracks intersect will be
analyzed to determine whether the changes in droplet sizes and numbers
reach saturation, based on the changes expected from analysis of the
changes in the separate tracks comprising the intersection. Previous
work has indicated that the retrieved optical depths and effective
droplet radii are likely to be sensitive to viewing geometry;
consequently, the sensitivity of the results to viewing geometry will
also be studied. Likewise, previous work has indicated that retrievals
of effective droplet radii may be sensitive to the near infrared
wavelengths used in the retrieval. Observations from VIRS and MODIS
will be analyzed to determine how the findings change with the
wavelengths of the near infrared radiances used in the retrievals.
For this project, desired input would be observations that could
assess the cloud properties retrieved from multispectral imagery data,
namely, in situ observations of droplet sizes, cloud liquid water
amount, and cloud top altitudes coincident with multispectral imagery
data. As output, the analysis of thousands of ship tracks is expected
to address issues such as:
1) the retention of liquid water by polluted
clouds;
2) whether the indirect effect saturates as the concentration of
particulates increases;
3) how clouds affected by ship plumes appear to
evolve in comparison with clouds that are unaffected.