Earth's
poles are shifting
Climate
change is causing the North Pole's location to drift, owing to subtle
changes in Earth's rotation that result from the melting of glaciers
and ice sheets. The finding suggests that monitoring the position of
the pole could become a new tool for tracking global warming.
13
December, 2013
Computer
simulations
had suggested that the melting of ice sheets and the consequent rise
in sea level could affect the distribution of mass on the Earth's
surface. This would in turn cause the Earth's axis to shift, an
effect that has been confirmed by measurements of the positions of
the poles.
Now,
Jianli
Chen
of the University of Texas at Austin and colleagues have shown that
melting due to our greenhouse-gas emissions is making its own
contribution to the shift.
The
wobble in Earth's axis of rotation is a combination of two major
components, each with its own cause. One is called the Chandler
wobble and is thought to arise because the Earth is not rigid.
Another is the annual wobble, related to Earth's orbit around the
sun.
Additional
wobble
Remove
these wobbles, and you are left with an additional signal. Since
observations began in 1899, the North Pole has been drifting
southwards 10 centimetres per year along longitude 70° west – a
line running through eastern Canada.
This
drift is due to the changes in the distribution of Earth's mass as
the crust slowly rebounds after the end of the last ice age. But
Chen's team found something surprising. In 2005, this southward drift
changed abruptly. The pole began moving eastwards and continues to do
so, a shift that has amounted to about 1.2 metres since 2005.
To
work out why the pole changed direction, Chen's team used data from
NASA's GRACE satellite, which measures changes in Earth's gravity
field over time. The data allowed them to calculate the
redistribution of mass on Earth's surface due to the melting of the
Greenland and Antarctic ice sheets and mountain glaciers, and the
resulting rise in sea level. It correlated perfectly with the
observed changes in the mean pole position (MPP).
"Ice
melting and sea level change can explain 90 per cent of the [eastward
shift]," says Chen. "The driving force for the sudden
change is climate change."
Greenland
thaw
Chen's
team calculated that the biggest contribution is coming from the
melting of the Greenland ice sheet, which is losing about 250
gigatonnes of ice each year. Another big factor is the melting of
mountain glaciers, which contributes about 194 gigatonnes per year.
The contribution from Antarctica adds up to 180 gigatonnes per year,
but there is considerable uncertainty here because changes in the
gravity field due to Earth's crust rebounding are less well
understood over Antarctica than elsewhere.
Since
the MPP can be accurately measured using multiple independent
techniques, its position and drift can be used to gauge the extent of
ice sheet melting, especially in between the end of the ageing GRACE
mission and the launch of the next generation of
gravity-field-measuring satellites, says Chen.
Jean
Dickey
of NASA's Jet Propulsion Laboratory in Pasadena, California, who was
not associated with the study, agrees. "It's a way to monitor
climate change by continuing to measure the deviation [of the MPP]
from what we have seen in the past," she says.
Chen
presented his findings this week at the annual
meeting of the American Geophysical Union
in San Francisco.
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