A satellite is record
variations in Earth's significance gives us a different view of our planet from
space looks like a potato. And yet, the information provided by this model is
the sharpest view we have of how gravity varies across the Earth. The device
was released by the team working on the European satellite GOCE.
It's a highly
exaggerated view, but illustrates well how the gravitational attraction
manifests from the mass of rock under our feet is not the same everywhere. Gravity
is strongest in yellow areas and weaker in the blue. Scientists say that the
information generated by the super-fast spacecraft is bringing a major change
in our understanding of the force that pulls us down and how it is reshaping some
key processes on Earth.
The higher of these new
approaches is a clearer view of how the oceans are moving and how they
redistribute the heat of the sun around the world, information that is
essential for climate studies. People interested in earthquakes are also poring
over the Goce results. The violent shocks that hit Japan last month, and Chile,
in 2010, occurred because there was a massive movement of rock. Antarctica is a
land that has broad information needs its gravitational field. Goce should provide
a three dimensional view of what was happening within the Earth.
"Even if these
earthquakes were caused by large shifts in the Earth, at the altitude of the
satellite signals are very small. But we should still see them in the
information," said Dr Johannes Bouman, the German Geodetic Research
Institute (DGFI, by its acronym in English). Technically speaking, the model
used is what the researchers defined as the geoid. It is one of the simplest
concepts, but essentially describes the surface "level" of an
idealized world.
Examine a potato and
irregularities. Put simply, the surface containing these pieces and projections
is where gravity is the same. Described another way, if you put a ball on this
potato, the ball would roll not because, from their perspective, there is no
"up" or "down" on the undulating surface. According to this
slightly odd way of looking at things, a boat off the coast of Europe (bright
yellow) can be placed 180 meters "higher" than a boat in the middle
of the Indian Ocean (dark blue) and continue in the same plane level.
GOCE results also have
application to seismology
However, this is the
trick gravity plays on Earth you as the space rock on which we live is not a
perfect sphere and its mass is distributed evenly. Enjoyment, an acronym that
means Ocean Circulation Explorer and Gravity, was released in March 2009. It
flies pole to pole at an altitude of only 254.9 km, the lowest orbit of any
research satellite currently in operation.
The spacecraft carries
three pairs of blocks of high precision platinum within its gradiometer
instrument that detects the accelerations that are as small as 1 part in
10,000,000,000,000 of the earth gravity experienced. This is what allows you to
design a map with the most noticeable differences in the gravitational pull
exerted by the mass of the planet from one place to another, from the great
mountain ranges to the deepest ocean cracks.
Two months of initial
observations were transformed into a geoid which was released in June last
year. The latest version, released in Munich at a workshop for Goce scientists,
includes an addition of four months of data. Each update should produce an
improvement in quality. "The more information you add, less blah-blah will
on solutions, and errors will start to decline," says Dr. Rune
Floberghagen, the GOCE mission manager for the European Space Agency. "And,
of course, best known as the geoid, better knowledge will be acquired using the
geoid"
He adds: "We are
witnessing the emergence of new information in areas such as the Himalayas, the
Andes mountain chain, and particularly in Antarctica. Entire continent is eager
to have more information about the gravitational field, which now we are
providing. " The mission has funding until 2012, when - as all missions of
Earth Observation European Space Agency - must find its own funding between
member states.
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