Untitled Document
Future
settlers take note: Galoshes and umbrellas are a must on Saturn's moon Titan,
where mornings are eclipsed by dreary drizzles of methane.
Getting
drenched would be the least of your worries, however, as Saturn's largest
satellite plunges to a bone-chilling -297 degrees Fahrenheit (-183 degrees
Celsius) at the surface and its swirling orange
atmosphere is full of hydrocarbons, such as methane, which is natural gas—and
no oxygen.
"Crude
oil minus the sulfur is a decent estimate of what the haze is," said lead
author of a new study of Titan's weather, Mate Adamkovics, an astronomer at the
University of California, Berkeley. "Really we don't know for sure, but I
would describe it as tiny particles of wax that are really, really cold, or
waxy snowflakes."
Adamkovics
added that while scientists are not sure how toxic the particles are, the lack
of oxygen would be much more of a hazard.
Using
near-infrared images from Hawaii's W. M. Keck Observatory and Chile's Very Large Telescope, the team of astronomers reveals a nearly global cloud cover
at high elevations on Titan. They also found persistent morning drizzle made of
methane over the western foothills of Xanadu,
Titan's largest "continent."
Measuring
about 3,200 miles (5,150 kilometers) across, Titan is larger than Mercury and
Pluto and about 40 percent the diameter of Earth. It is the only moon in the
solar system with a dense, planet-like atmosphere (10 times denser than
Earth's).
As is the
case on Earth, where features like lakes and mountains can morph and direct
weather systems, Titan's terrain also could be a rain maker.
"Titan's
topography could be causing this drizzle," said study team member Imke de
Pater, an astronomy professor at UC Berkeley. "The rain could be caused by
processes similar to those on Earth: Moisture laden clouds pushed upslope by winds
condense to form a coastal rain."
Cloudy
observations
The new
findings, detailed in the Oct. 11 issue of Science Express, an online
version of the journal Science, provide strong evidence supporting past
cloud-cover observations and possible indicators of methane
drizzle over parts of Titan.
In 2005,
the Huygens probe that had been aboard NASA's Cassini spacecraft gathered data
supporting the existence of frozen methane clouds at higher elevations and
liquid methane clouds, with possible drizzle, lower in the atmosphere.
But the
extent of such clouds was unclear. "A single weather station like Huygens
cannot characterize the meteorology on a 'planet-wide' scale," said UC
Berkeley astronomer Michael Wong, who was part of the recent study.
And until
now, liquid rain was inferred from reports of lakes of liquid
hydrocarbon, which scientists presumed were filled by methane precipitation.
Dreary
Titan
Adamkovics
and his team analyzed infrared measurements throughout Titan's atmosphere. By
subtracting out the absorption and scattering due to aerosols low in the
atmosphere as well as light from the surface, they were left with a signal that
was due to actual droplets of liquid methane. Using a "radiative transfer
model," the scientists distinguished between miniscule drops inside clouds
and larger ones that form drizzle.
The results
paint a dreary picture with a global cloud of frozen methane hovering at a
height of about 16 to 22 miles (25 to 35 kilometers), liquid methane clouds
below 12 miles (20 kilometers) and drizzling methane at lower elevations.
"We
show that the solid cloud covers the globe and the drizzle happens
predominantly in the morning," Adamkovics told SPACE.com.
The methane
droplets inside Titan's clouds are estimated to be a thousand times larger than
those in terrestrial clouds. Yet, both contain similar moisture contents,
Adamkovics said. And if a cosmic cloud wringer were to empty out Titan's
clouds, about six-tenths of an inch (1.5 centimeters) of water would blanket
the moon's surface.
The drizzle
or mist appears to dissipate after about 10:30 a.m. local Titan time, which is
about three Earth days after sunrise. Titan takes nearly 16 Earth days to
rotate once.