The vertical structure of Titan's atmosphere and
surface composition
can be probed spectroscopically and usually involves integrating data
over the entire disk. Spatial variations in surface contrast, atmospheric
haze and clouds can be measured by
adaptive optics imaging
with narrowband filters. Below are results combining these two techniques.
With spatially-resolved spectroscopy the atmospheric structure and surface
albedo can be determined at various locations on the disk of Titan. These
data have been particularly useful in determining the magnitude and altitude
of the seasonal enhancement of tropopause haze near the Southern pole.