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Hello again, Mars: Opportunity comes callingBy Dan Vergano, USA TODAY
Opportunity will knock twice on Mars — and then
some — when another NASA rover makes a bouncing landing on the Red
Planet early Sunday.
Set on course by rocket firings last week,
Opportunity is scheduled to arrive on Mars at 12:05 a.m. ET, promising
plenty of landing drama, slow-motion unpacking and views of a grayish
plain "fundamentally different" from anything glimpsed by previous Mars
explorers, says the Jet Propulsion Laboratory's Matthew Golombek.
Opportunity's landing target is Meridiani
Planum, an equatorial plain laced with veins of gray hematite, an
iron-oxide mineral associated with hot springs on Earth. It lies on the
opposite side of Mars from Gusev Crater, where the rover Spirit landed
Jan. 3.
As of Thursday, however, the Spirit stopped
transmitting data for more than 24 hours, said NASA managers, who call
the situation an "extremely serious anomaly."
Public interest in Mars remains high. JPL
officials in Pasadena, Calif., home of NASA's rover missions, reports
2.5 billion hits on the lab's Web page since Spirit's landing.
And with President Bush's call this month for
more exploration of the moon and Mars, the space agency hopes
Opportunity garners the same attention as Spirit.
The mission of the $820 million Mars Exploration
Rover is to "follow the water." Pictures and instruments suggest that
water — considered a fundamental requirement for life — once carved
Mars' surface, perhaps within the past few million years, and still
lurks below the ground. To test these notions, Opportunity will rove
over what is suspected to be a 3.8-billion-year-old seabed.
Compared with the red deserts seen by every
previous lander, "Meridiani is going to have a completely different
look and feel," Golombek says. It's smoother than Gusev Crater's
interior with no hills and a few "fossil" craters, ancient features
with sanded-off rims.
That smooth surface and less windy conditions
make Meridiani a relatively safe bet for a landing, mission controllers
say, but they still warn that a bad bounce could be trouble. "The
question," JPL project manager Pete Theisinger says, "is always what
you hit and how hard you hit it."
With minor modifications, the descent will
follow the heat shield, parachute, braking rocket and airbag landing
plan carried out by Spirit.
On impact, Spirit bounced 28 times to nearly
30-foot heights and traveled about 1,000 feet from its impact point in
Gusev Crater.
Remote sensing instruments suggest Meridiani is
only about 5% covered with rocks, but the possibility that a rock could
puncture a bouncing airbag remains a worry.
At best, orbiters can pick up surface details
only 6 feet to 30 feet across, which leaves some uncertainty about the
landing site. And random bounces aren't events designed for an
engineer's comfort.
"You never know. You shouldn't be
overconfident," says Rob Manning, JPL's entry, landing and descent
manager. If Spirit had landed on the now-famous hills about 2 miles
east of its resting spot, it might have been a disaster, he says. "It
doesn't take too many bounces and you fall off a cliff."
Meridiani is flatter than Gusev Crater and rests
nearly one-third of a mile higher, so the air is thinner. Thin air also
can affect the landing. Because dust storms thinned the air over Gusev,
Spirit popped its parachute nearly 1 mile closer to the surface than
expected. Meridiani looks less dusty, but if weather reports call for
it, the team could direct Opportunity to pop its chute sooner,
Theisinger says.
"The Spirit landing was very successful; it
showed there was enough robustness in all the systems to handle
conditions somewhat different from anticipated," says atmospheric
scientist Paul Withers of Boston University.
Opportunity for science
Much of the excitement over Spirit seems derived
from NASA having a success, especially after the British Beagle 2 Mars
lander disappeared during Christmas, says astronomer Phil Plait of
Sonoma State University in Rohnert Park, Calif. But many people who
contact his badastronomy.com Web site, which is dedicated to correcting
public misconceptions about astronomy, have genuine science questions
about Mars.
"People do get that it's another planet, and that's intrinsically fascinating," he says.
Scientists are far from immune to that
fascination. Viewed as a dry desert planet for decades, Mars has
enjoyed a revival of interest.
In 2000, NASA's Mars Observer revealed signs of
water-carved features. In 2002 another probe found evidence of enough
water just under the surface to fill Lake Michigan twice, leading to
the possibility that more could be hidden deeper.
"Both landing sites are about finding out
whether the early environment on Mars kept liquid water stable,"
Golombek says. "We try not to have biases, but I'm very excited to see
Meridiani."
Unlike Spirit, which scientists hope to drive
about 800 feet to explore the rock layers within a small crater,
Opportunity should land on top of its target, an ellipse 53 miles long
and nearly 7 miles wide.
Gray hematite covers as much as 20% of Meridiani. Depending on Opportunity's findings:
• Layers of sedimentary rock may indicate that an iron-rich lake or ocean formed the mineral layer.
• Hot springs, which are considered a favorable habitat for microbes, might have bubbled up and deposited veins of hematite.
• Weathering of small amounts of water on iron-rich rocks can create a veneer of hematite, which the rover should reveal.
• Lava, indicated by volcanic rocks residing solely at the landing site, also can create hematite.
On the lava possibility, Golombek says that "the jury is still out" on the lake bed theory.
Others are more optimistic that the area is a lake bed.
William Hartmann of the Planetary Science
Institute in Tucson suspects that Meridiani Planum is part of an
antique region once covered with iron-rich waters that formed a layer
of gray hematite and was exposed by wind erosion within the past 10
million years.
"Remember that we've discovered dry riverbeds
all over Mars. There must have been occasional liquid water on the
surface in ancient times," Hartmann says. "Apparently it soaked into
the ground and froze, like in Canadian winters. ... There is probably
much more underground ice on Mars today than had been thought."
That's promising, because on Earth many soils
once thought to be sterile actually hide microbes. Examples are the
Mars-like dry, cold areas of Antarctica and the Atacama Desert in Chile.
Long-term questions
Some of the interest in Mars springs from a 1996
report, which was widely doubted by scientists outside NASA, of
fossilized Martian microbes discovered inside an Antarctic meteorite
judged to be about 3.6 billion years old.
Perhaps similar microbes exist in rocks Opportunity will explore or in rocks examined by future explorers.
Golombek predicts both rovers will outlast their
expected lifetimes of 90 days of battery power. The 1997 Sojourner
lasted three times its design life.
"I expect we'll go at least twice as long this time."
That's good news for scientists, who view the rover missions as brief windows on a distant world.
And though they admire the "ground truth"
collected by rover instruments, even the most hardheaded data geeks are
mindful of the big questions about life in other places than Earth that
Mars might be able to answer.
"If we do find life, it's the first time we know life can start on other planets and that we aren't alone," Hartmann says.
"Or, if we find no life ever started there,
maybe we are more alone in the universe than we thought. Maybe there is
something wrong with our theories about the origins of life. It's an
exciting adventure for humanity either way."
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