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Mars
and Venus are surprisingly similar
Wednesday, March 5, 2008
Credits: ESA
(Animation by C. Carreau)
Using two ESA spacecraft,
planetary scientists are watching the atmospheres of Mars and
Venus being stripped away into space. The simultaneous
observations by Mars Express and Venus Express give scientists
the data they need to investigate the evolution of the two
planets’ atmospheres. Scientists call this
work comparative planetology. Mars Express and Venus Express are
so good at it because they carry very similar science
instruments. In the case of the Analyzer of Space Plasmas and
Energetic Atoms (ASPERA), they are virtually identical. This
allows scientists to make direct comparisons between the two
planets.
The new results probe directly into the magnetic
regions behind the planets, which are the predominant channels
through which electrically-charged particles escape. They also
present the first detection of whole atoms escaping from the
atmosphere of Venus, and show that the rate of escape rose by ten
times on Mars when a solar storm struck in December 2006.
By
observing the current rates of loss of the two atmospheres,
planetary scientists hope that they will be able to turn back the
clock and understand what they were like in the past. “These
results give us the potential to measure the evolution of
planetary climates,” says David Brain, Supporting
Investigator for plasma physics for Venus Express and
Co-Investigator for ASPERA on Mars and Venus Express at the
University of California, Berkeley.
(each image contains a HOT
spot to Full Caption and Hi-Res version)
Top: Mars Express Bottom:
Venus Express
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Credit: Top: ESA -
D. Ducros Bottom: ESA (Image by AOES Medialab)
The new observations show
that, despite the differences in size and distance from the Sun,
Mars and Venus are surprisingly similar. Both planets have beams
of electrically charged particles flowing out of their
atmospheres. The particles are being accelerated away by
interactions with the solar wind, a constant stream of
electrically charged particles released by the Sun.
At
Earth, the solar wind does not directly interact with the
atmosphere. It is diverted by Earth’s natural cloak of
magnetism. Neither Mars nor Venus have appreciable magnetic
fields generated inside the planet, so each planet’s
atmosphere suffers the full impact of the solar wind.
Interestingly, this full-on interaction does create a
weak magnetic field that drapes itself around each planet and
stretches out behind the night-side in a long tail. Venus’s
atmosphere is thick and dense, whereas that of Mars is light and
tenuous. Despite the differences, the magnetometer instruments
have discovered that the structure of the magnetic fields of both
planets are alike.
“This is because the density of
the ionosphere at 250 km altitude is surprisingly similar,”
says Tielong Zhang, Principal Investigator for the Venus Express
magnetometer instrument at Institut für Weltraumforschung
(IWF), Österreiche Akademie der Wissenschaften, Austria. The
ionosphere is the surrounding shell of electrically-charged
particles created by the impact of sunlight on the planet’s
upper atmosphere.
The proximity of Venus to the
Sun does create an important difference, however. The solar wind
thins out as it moves through space so the closer to the Sun it
is encountered, the more concentrated is its force. This creates
a stronger magnetic field, making the escaping atmospheric
particles move collectively like a fluid.
At Mars, the
weaker field means that the escaping particles act as
individuals. “This is a fundamental difference between the
two planets,” says Stas Barabash, ASPERA Principal
Investigator on both Mars Express and Venus Express, Swedish
Institute of Space Physics.
Another illuminating
difference between Mars and Venus is that Mars displays strong
small-scale magnetic fields locked into the crust of the planet.
In some regions, these pockets protect the atmosphere, in others
they actually help funnel the atmosphere into space.
The
complexity of the different processes revealed at Venus and Mars
means that planetary scientists do not yet have the full picture.
“There will be many more results to come,” says
Barabash.
There is a lot to do because there are many
different mechanisms that may cause the atmospheric particles to
escape. Untangling it all will take time. “The longer the
spacecraft work together, the longer we can watch and see what
really happens,” says Brain.
Source:
ESA

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