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While the magnetic field is created largely by an ocean of superheated, swirling liquid iron in the planet’s outer core, other factors, like magnetised rocks in the crust and the flow of the ocean, also affect the field.

We wouldn’t normally think of seawater as being a source of magnetism, but it does make a tiny contribution.

When salty ocean water flows through Earth’s magnetic field, an electric current is generated, and this, in turn, induces a magnetic signal.

However, the field generated by tides is tiny and extremely difficult to measure – but Swarm has done just this in remarkable detail.

The animation above shows how the tidal magnetic signal changes over 24 hours.

Nils Olsen, from the Technical University of Denmark, said, “We have used Swarm to measure the magnetic signals of tides from the ocean surface to the seabed, which gives us a truly global picture of how the ocean flows at all depths – and this is new.

“Since oceans absorb heat from the air, tracking how this heat is being distributed and stored, particularly at depth, is important for understanding our changing climate.

“In addition, because this tidal magnetic signal also induces a weak magnetic response deep under the seabed, these results will be used to learn more about the electrical properties of Earth’s lithosphere and upper mantle.”

As well as shedding this new light on magnetic tides, Swarm has also yielded a new map of the magnetic field generated by Earth’s crust. Read more here: Magnetic lithosphere detailed

Download the comic: Scanning Earth with the tides