THE JOHN C. LINDSAY MEMORIAL LECTURE
GODDARD SPACE FLIGHT CENTER 2011 John C. Lindsay Award Winner |
|
"Titan's Dynamic Atmosphere"
Planetary atmospheres
are complex systems. Studies of extraterrestrial
atmospheres have drawn on the much more extensive data and
analysis of Earth, but its atmosphere is only one
realization in the range of possibilities. Efforts
to understand other atmospheres and predict their behavior
must be closely tied to observations. The
atmospheres in the solar system are large-scale natural
laboratories with different “external” drivers (e.g.,
planetary rotation, solar forcing, internal heat
fluxes). Examining their response to these different
conditions is an important step toward understanding the
physical processes that govern them.
This talk focuses on one such laboratory, Saturn’s giant
moon Titan, which has been explored through
Cassini-Huygens and earlier Voyager spacecraft
measurements, as well as from ground-based
observations. Titan’s atmosphere is an intriguing
blend in the planetary line-up. In several respects,
it resembles Earth’s. Its atmosphere is primarily
N2, and its surface pressure is about 50% larger.
The second most abundant constituent is not O2 but CH4,
and there is evidence for a hydrological cycle involving
CH4. Titan’s winter stratosphere has different
chemistry than on Earth, but it has an analog to the ozone
hole, with strong circumpolar winds, condensate ices, and
anomalous concentrations of organic gases near the
pole. However, Titan is a much slower rotator than
Earth: its “day” is 15.95 Earth days. In this
regard, it is more like Venus, another slow rotator, and
it provides the second example in the solar system of an
atmosphere with global super-rotation, i.e., its winds
whip around the body in much less time than a Titan
day. Because of Saturn’s large axial tilt relative
to its orbital plane, Titan is a Venus with seasons.
The origin and maintenance of the strong winds on Venus
and Titan are poorly understood, and the seasonal changes
in Titan’s winds and temperatures—observations from the
Cassini spacecraft are already showing them—provide clues
for understanding these systems.
About the Speaker
Michael Flasar has been at the Goddard Space Flight Center
since 1975. His primary research is the dynamic meteorology
of planetary atmospheres, including those of Mars, the giant
planets, and Saturn’s moon Titan. Since 1990 he has
been active in the Cassini-Huygens Mission to the Saturn
system, both as a member of the Radio Science team and as an
investigator on the Composite Infrared Spectrometer (CIRS)
experiment. He has been the CIRS Principal
Investigator since 2002. He was also a member of the
Radio Propagation Team on the Galileo Mission to Jupiter and
an investigator on the infrared spectroscopy experiment
(IRIS) on the Voyager spacecraft, which flew past Jupiter,
Saturn, Uranus, and Neptune from 1979 to 1989. Before
coming to Goddard, Dr. Flasar was a Research Fellow at
Harvard University. He received both his B. S. (1967)
and Ph.D. (1972) degrees in Physics from Massachusetts
Institute of Technology. He has published more than
100 papers in peer-reviewed scientific journals, and he is a
member of the American Geophysical Union, the American
Astronomical Society, the AAS/Division for Planetary
Sciences, and the American Meteorological Society.