TY - JOUR
T1 - Titan's north-south asymmetry from HST and Voyager imaging
T2 - Comparison with models and ground-based photometry
AU - Lorenz, Ralph D.
AU - Smith, Peter H.
AU - Lemmon, Mark T.
AU - Karkoschka, Erich
AU - Lockwood, G. W.
AU - Caldwell, John
N1 - Funding Information:
We thank Martin Tomasko for the use of the proposal 6030 images. RDL thanks Mary Guerrieri, Carolyn Porco, and Vance Haemmerle for assistance with retrieving and processing Voyager images. We also acknowledge the contributions of Steve Croft and Dhananjay Mahajan. Caitlin Griffith and an anonymous referee made comments which significantly improved the paper: we particularly acknowledge the diligent close attention of anonymous referee II who provided two sets of 10 single-spaced pages of comments. This work is based in part on observations with the NASA/ESA Space Telescope, and partial support was provided by NASA through Grant G0-5508.01-93A from the STScI, which is operated by AURA, Inc., under NASA Contract NAS 5-2655.
PY - 1997/5
Y1 - 1997/5
N2 - New measurements of Titan's hemispheric brightness asymmetry from HST images from 260 to 1040 nm show that the contrast is strongest near 450 nm (blue) and, with the opposite sign, at 889 nm (methane band). Comparison with a full Titan year of disk-integrated albedo data indicates that the seasonal cycle in asymmetry is smooth, but is insufficient to explain the variation in albedo, and a twice-per-year global albedo enhancement 50% larger than the hemispheric asymmetry amplitude is required, as noted by other workers. We also report measurements of limb-darkening (strongest at red wavelengths) and note that the transition zone between the "hemispheres" lies in the northern, brighter hemisphere at present. Comparison of models to the HST data set indicates that a change in aerosol number density above 70 km, and largely below 120 km, is the likely mechanism and is probably driven by aerosol transport by meridonal and vertical winds.
AB - New measurements of Titan's hemispheric brightness asymmetry from HST images from 260 to 1040 nm show that the contrast is strongest near 450 nm (blue) and, with the opposite sign, at 889 nm (methane band). Comparison with a full Titan year of disk-integrated albedo data indicates that the seasonal cycle in asymmetry is smooth, but is insufficient to explain the variation in albedo, and a twice-per-year global albedo enhancement 50% larger than the hemispheric asymmetry amplitude is required, as noted by other workers. We also report measurements of limb-darkening (strongest at red wavelengths) and note that the transition zone between the "hemispheres" lies in the northern, brighter hemisphere at present. Comparison of models to the HST data set indicates that a change in aerosol number density above 70 km, and largely below 120 km, is the likely mechanism and is probably driven by aerosol transport by meridonal and vertical winds.
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U2 - 10.1006/icar.1997.5687
DO - 10.1006/icar.1997.5687
M3 - Article
AN - SCOPUS:0031139010
SN - 0019-1035
VL - 127
SP - 173
EP - 189
JO - Icarus
JF - Icarus
IS - 1
ER -