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magazine / jf12

January/February 2012 issue


À LA CARTE

The laws of attraction
Mapping the pull of gravity reveals a Mr. Potato Head planet
By

The effect of gravity on sea levels
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The geoid model shows the effect of gravity on sea levels. Regions in blue, such as North America (CENTRE), experience a relatively weak gravitational force and low sea levels, while regions in yellow experience stronger gravitational force and higher sea levels. (European Space Agency/German Aerospace Center)
From space, the human eye sees Earth as a perfect sphere, but for scientists, the lumpy globe shown at right is closer to the truth. Produced in the spring of 2011 by the European Space Agency and the German Aerospace Center, using data from the GOCE satellite, this geoid is the best image yet of the effects of gravity on the planet.

Imagine Earth with its oceans at rest. Unaffected by currents, weather and tides, water would be free to redistribute evenly around the globe. The geoid is this resting surface, shaped only by gravity, and is a crucial reference for measuring ocean circulation, sea-level change and ice dynamics.

The fact that the geoid appears like a lumpy potato — and that the gravitational field is weak or strong — is due to the varying distribution of mass, in the form of mountains or valleys or mantle, that is more or less dense. Less mass means weaker gravity and a lower sea level.

In regions such as central Canada, where the land mass has been compressed by glaciers, gravitational pull is relatively weak. In areas such as Oceania, around Australia, where there is volcanic activity, dense magma sits close to a soft, less dense crust. This increases gravitational pull.

The latest gravity map gives scientists a more accurate sense of the Earth’s topography. Using such data, they can plot precise elevations with global positioning systems and better measure gravity changes, which is helping advance our knowledge of the processes that cause earthquakes.

In 2013, Natural Resources Canada (NRCan) plans to update its vertical reference system, replacing the one established in 1928 with a geoid-based reference.

“Using these kinds of space-based techniques allows us to get elevation data anywhere in Canada with similar accuracy,” says Denis Hains, director of NRCan’s Geodetic Survey Division. “This is particularly important in the North, where there are multiple reference systems.”


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