Once Santa Claus concludes his yuletide deliveries on Christmas Eve, an essential journey back to the North Pole awaits him. This return trip presents a significant navigational quandary, particularly when dense snowfall obstructs the reindeer’s visibility.

While a compass could serve as a guide, a perplexing challenge arises: Santa must accurately pinpoint the correct North Pole.

Indeed, there are two distinct North Poles: the geographic North Pole, which appears on conventional maps, and the magnetic North Pole, upon which compasses depend. These two points are not congruent.

The Duality of North Poles

The geographic North Pole, also referred to as true north, represents the apex of the Earth’s axis of rotation.

Envision holding a tennis ball in your right hand, placing your thumb at the bottom and your middle finger at the top. Now, simulate rotation using your left hand’s fingers.

The points where your thumb and middle finger make contact with the spinning tennis ball delineate the axis of rotation. This axis traverses the center of the sphere, extending from the South Pole to the North Pole.


A compass with S, E, N, W and other markings
Compasses utilize a magnetized needle that aligns with the Earth’s magnetic field. To ascertain true north, a compass necessitates compensation for the local magnetic declination, which is the angular disparity between true north and magnetic north at a given locale. (Tim Reckmann/Wikimedia Commons, CC BY 4.0)

The Earth’s magnetic North Pole, however, presents a different scenario.

Centuries ago, seafarers pioneered the use of compasses, commonly fashioned from buoyant materials like cork or wood adorned with a magnetized needle, to navigate. The Earth is enveloped by a magnetic field that functions akin to a colossal magnet, with the compass needle orienting itself accordingly.

Modern navigational aids, such as smartphones, rely on the magnetic North Pole for orientation – and this pole is subject to continuous displacement.

The Dynamic Nature of the Magnetic North Pole

The migratory tendency of the magnetic North Pole is an intrinsic consequence of the Earth’s dynamically active core. The inner core, situated approximately 3,200 miles beneath the surface, exists in a solid state, subjected to such profound pressure that its material cannot liquefy. Conversely, the outer core is in a molten state, composed of liquefied iron and nickel.

Radiant heat emanating from the inner core fuels the convection currents within the molten iron and nickel of the outer core, analogous to the simmering of soup in a pot on a heating element. The agitation of this iron-rich fluid generates a magnetic field that permeates the entire planet.

As the molten iron within the outer core circulates, the magnetic North Pole undergoes a process of wandering.


Lines show how the magnetic pole has moved
The magnetic North Pole’s trajectory has been observed to wander since the late 16th century, with its rate of movement accelerating significantly in the last hundred years. The dates indicated reflect direct observations from expeditions. Other data points are derived from models, utilizing information from NOAA. The depicted map highlights the islands of northern Canada, with the edge of Greenland visible on the far right. (Cavit/Wikimedia Commons, CC BY 4.0)

For the majority of the preceding six centuries, the pole’s movement was primarily localized over northern Canada, progressing at a comparatively gradual pace of roughly 6 to 9 miles annually. This rate experienced a substantial escalation around 1990, increasing dramatically to approximately 34 miles per year.
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Approximately a century ago, it began a discernible shift towards the geographic North Pole. Terrestrial scientists attribute this phenomenon to alterations in the fluid dynamics within the outer core, though the precise causative factors remain subject to ongoing investigation.

Facilitating Santa’s Return Home

Given that Santa’s domicile is established at the geographic North Pole—an area situated in the ice-laden heart of the Arctic Ocean—the crucial question arises: how does he reconcile his compass readings when the two North Poles occupy disparate locations?

Regardless of the navigational instrument employed, be it a traditional compass or a sophisticated smartphone, both ultimately depend on magnetic north as a reference point for directional guidance.

While contemporary GPS systems provide precise locational data for journeys, they cannot accurately ascertain directional course without the device first discerning the orientation of magnetic north.


Lorenz King/Wikimedia Commons
In 1990, scientific personnel were stationed at a temporary research outpost near the Geographic North Pole. ([email protected]/Wikimedia Commons, CC BY 4.0)

For Santa’s utilization of a conventional compass, an adjustment for the divergence between true north and magnetic north is imperative. This necessitates knowledge of the magnetic declination pertinent to his precise location—the angular measurement separating true north from magnetic north. Such an adjustment ensures accurate course plotting. The National Oceanic and Atmospheric Administration offers an online tool designed to facilitate this calculation.

Should Santa opt for a smartphone, its integrated magnetometer automates this process. This component gauges the local intensity of the Earth’s magnetic field and subsequently consults the World Magnetic Model to refine navigational accuracy.

Irrespective of the method Santa employs, his reliance on magnetic north for both his inbound journey to your residence and his subsequent return voyage is highly probable. Alternatively, one might conjecture that the reindeer possess an innate sense of direction.The Conversation