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It's on the move!
Earth's north magnetic pole is on the move, unpredictably lurching away from the Canadian Arctic and toward Siberia. It's wandered so much, that the current representation of the entire globe's magnetic field, just updated in 2015, is now out of date. And so, geologists have come up with a new model.
This updated model, called the World Magnetic Model, was supposed to be published Jan. 15, but it's now been delayed to Jan. 30, on account of the government shutdown.
Once it's made public, the new model will inform a wide array of navigation, including those directing airplanes and ships to people checking Google Maps on their smart devices.
The World Magnetic Model is one of a handful of models — another is called the International Geomagnetic Reference Field — that track so-called declination, or the difference between true, or geographic, north (that is, the North Pole) and magnetic north (the point where your compass needle points). Knowing that declination for points across the globe allows one to convert between a magnetic bearing and a true bearing, according to a report on the 2015 model. In that way, ships, aircraft, antennas, drilling equipment and other devices can be oriented.
The latest World Magnetic Model was designed to last until 2020, but magnetic north's rapid and unexpected surge toward Siberia was so great, that researchers had to amend the model early, Arnaud Chulliat, a geomagnetist at the University of Colorado Boulder and the National Oceanic and Atmospheric Administration's (NOAA's) National Centers for Environmental Information, told Nature.
News of the magnetic north's meanderings isn't exactly new. Researchers figured out in the 1800s that magnetic north tended to drift. Then, in the mid-1990s, it began moving faster, from just over 9 miles (15 kilometers) a year to about 34 miles (55 km) annually, Nature reported. In 2018, magnetic north skipped over the International Date Line and entered the Eastern Hemisphere.
Earth's Magnetic Pole Is Wandering, Lurching Toward SiberiaCore message
The North Pole’s erratic movements are largely the result of Earth's liquid-iron outer core, known as the core field. (Other factors play a role, too, including magnetic minerals in the crust and upper mantle, as well as electric currents created by the flow of seawater, but these influences are small compared to those from the