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2004 has seen two more Mars rovers exploring the planet. Opportunity and Spirit,
vital components of the Mars Exploration Rover mission have acted like robotic
human field geologists. They have travelled over 0.6km climbing 25° rocky slopes
on their way, used abrasion tools to drill into various rocks, returned images
of the rock surfaces using on-board microscopes and taken (together with the lander)
coloured stereo panoramas of their surroundings
Spirit landed in the 140-km diameter Gusev Crater and the returned data clearly
show that this was once a lake. Data from Opportunity indicates that its landing
site, Meridiani Planum, was once a salty swamp. The climate of Mars has changed
drastically over time mainly due to slow variations in the eccentricity of the
orbit and the angle of inclination of the spin axis to the orbital plain. It is
quite likely that it will again become warm and wet some time in the future.
One of the next steps in Martian exploration, midway between a lander and an orbiter
is NASA’s proposed remote controlled ‘model’ aeroplane ARES
(short for Aerial Regional-scale Environmental Survey). This will fly around searching
for possible sources of methane, trying to check whether they are volcanic or
biotic.
Landing on Venus has always been a well-known problem ever since the USSR’s
Venera 7 touched down in December 1970. Concentrated sulphuric acid from the all-enveloping
cloud layers corrode any descending space probe and it quickly becomes inoperable.
The last probes to land there were Vega 1 and Vega 2 in June 1985. No samples
have been returned and no Venusian meteorites are known. It is certainly time
to try again. Modern technology should surely be able to shield a space probe
during descent. That said, with a surface temperature of about 460°C and a
surface pressure 92 times that at the surface of Earth there are still serious
challenges.
Landing on Mercury is also a job for the future. The lander that was to be part
of the joint European / Japanese mission to the planet has been cancelled due
to lack of funds.
Landers are important. They can be used to monitor atmospheric pressure, composition,
winds and weather. It is also very important to have networks of landers scattered
over planetary surfaces. Atmospheric parameters clearly vary with latitude and
longitude and time of day and year. And having seismometers at different places
enable the source and strength of planet-quakes to be monitored. Even though it
is relatively easy to see what is on the surface of a planet, the interiors remain
extremely mysterious and our knowledge of the composition and volumes of planetary
cores is extremely rudimentary.
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