The Conversation] In a driverless future, it will be vital that our cars know exactly where they are on the road, down to the millimetre. We’ve found that our current methods of measuring location may not be up to scratch. Changes on Earth’s surface, including polar ice melt, may alter its centre of mass, throwing our calculations out of whack.
Accurately pinpointing a location with a global positioning system (GPS)
can only be done relative to Earth’s centre. Because we can’t reach the
centre ourselves, scientists have to use satellite sensing to
indirectly measure its location, and how it moves.
It’s a complicated task because the globe is not a perfect sphere nor
uniformly made of the same material. Significant changes on its
surface, such as melting snowpack, may also shift its centre of mass.
This means the centre of Earth essentially “wiggles”, but current
measurement methods don’t accurately measure season-to-season variations
that occur due to water movement. They also assume that its long-term
motion can be described by the fit of a straight line. We believe that
much more work needs to be done.
The centre of Earth’s mass may not necessarily be close to its geometric centre.
To put it another way, while a cannonball’s centre of mass will be at
its exact geometric centre, a pineapple’s centre of mass is closer to
its heavier end.
It’s the same for Earth’s centre of mass: it will be closer to heavier loads on the surface and within Earth itself.
Water can be a “heavier load”, both in the oceans, rivers and
atmosphere, and in its solid form as ice sheets, glaciers and snow. High
water levels in the Northern Hemisphere due to massive snowfall and
rain over Canada and Europe during the winter, for example, change as the seasons transition into summer.
This matters when measuring Earth’s centre of mass. Take a
ridiculously heavy cyclist, for example. As the cyclist travels over the
surface of the Earth, the centre of Earth’s mass moves, as a balancing
act. In the same way, as snow melts in the Northern Hemisphere spring
and flows into the oceans, the Earth’s centre of mass may move away from
the Northern Hemisphere.
As we monitor changes to land ice in Antarctica and Greenland, as
well as the smaller mountain glaciers, we can also see changes in the
motion of Earth’s centre of mass.
As some of this ice melt is due to human activity warming the
atmosphere and ocean, humans may be indirectly changing the centre of
mass of the entire planet. Read More