Is the Earth’s Magnetic Field Heading for a “Big Flip”? Probably Not (Right Now).

By Erik Klemetti | March 13, 2018 7:56 am
Aurora over the Earth. JPL.

Aurora over the Earth. JPL.

Before we get started, let’s have a cheer for Earth’s magnetic field! I would guess most of you never give it a second thought, unless you’re watching the Northern Lights or maybe using a compass. However, things would be very different on Earth if we didn’t have a magnetic field. However, some people fear that the Earth’s magnetic field might be headed for a big change that could bring chaos to modern society … but we likely don’t need to worry about it just yet.

So, what generates the Earth’s magnetic field anyway? It is a dynamo!

Computer simulation of the magnetic field lines in the Earth's dynamo, generated by the convecting outer core. Wikipedia - Dr. Gary A. Glatzmaier - Los Alamos National Laboratory - U.S. Department of Energy.

Computer simulation of the magnetic field lines in the Earth’s dynamo, generated by the convecting outer core. Wikipedia – Dr. Gary A. Glatzmaier – Los Alamos National Laboratory – U.S. Department of Energy.

The Earth’s interior is layered and the innermost layers are the solid iron-nickel inner core and the liquid iron-nickel outer core. That outer core isn’t sitting still, no, it convects thanks to temperature and density differences across the outer core along with the rotation of the Earth. This generates cells of motion in outer core … moving liquid metal! What happened when you pass a current through liquid, moving metal? You generate a magnetic field! That initial current comes from the fact that charged particles from the sun (called the solar winds) generated a magnetic field when interacting with the Earth early in its history and started the dynamo. Since then, it has been self-sustaining as long as that outer core keeps on convecting.

That magnetic field generates the Earth’s magnetosphere (below), the volume around the planet where our awesome magnetic field prevails. This keeps most of the solar winds from getting any closer than maybe 4 Earth radii from the surface other than at the poles, where the magnetic field lines intersect the surface of the Earth. Those solar wind particles that sneak through and make it to the poles are what generates aurora in our atmosphere.

Other planets aren’t so lucky. Venus, which is very similar to Earth in size, seems to lack a convecting liquid core – instead, the entire core is liquid, so no thermal gradient exists. This means Venus only has a weak magnetic field caused by solar winds interacting with the thick Venutian atmosphere. Mars also lacks a strong magnetic field and that may be a major reason its atmosphere lost oxygen and carbon dioxide as the solar winds buffeted the planet.

A diagram of the Earth's magnetosphere, showing where our magnetic field runs the show. Wikipedia.

A diagram of the Earth’s magnetosphere, showing where our magnetic field runs the show. Wikipedia.

Now, the Earth’s magnetic field hasn’t always been stable. It goes through two types of changes: reversals and excursions. During a reversal, the polarity of the magnetic field flips, so your compass needle would point towards the South Pole. An excursion is just a period when the magnetic field gets wonky, so compass needles might not even work that well at all. Geologists and geophysicists don’t really know why the magnetic field on Earth (and elsewhere) flips beyond the idea that something in the outer core changes occasionally. There isn’t even a real pattern to the reversals — some are brief while others can last tens of millions years. The current “normal” configuration we’re in is one of the longer ones – only 14% have been longer – and we’ve been in it for the last 780,000 years.

When reversals do happen, the magnetic field gets all weird. Looking at the record of magnetic field variations recorded in rocks (called “paleomagnetism“), it appears that for maybe centuries to millennia before and after a reversal, the magnetic field drops in strength to maybe 10% of what we have today. The poles also more or less go away as the field switches from its current northern polarity to southern polarity. In a sense, the Earth’s shields go down for a while.

Why is that bad? First off, the lack of protection from the solar winds and cosmic rays generated in deep space means higher radiation on the Earth’s surface. Combine that with erosion of the ozone layer, letting in more ultra-violet rays from the sun and we’re taking higher rates of skin cancer and potential for other mutations. Now, there is no known mass extinction directly tied to a reversal, but there is evidence that tiny sea creatures called radiolaria have died out during some reversals, which could impact marine ecosystems.

Beyond the biological impact, the loss of a strong magnetic field would leave our modern society vulnerable to the charged particles in the solar wind. Satellites would be disabled and destroyed, the electrical grid could fail during solar flares, communication lines could be broken, including cellular and wired lines. Combine the loss of possibly GPS satellites and a magnetic North Pole and navigation becomes that much more complicated – back to using the stars? That sort of potential for global disruption in communication and power would likely means many deaths and who knows what else.

So today, things are good, right? Well, that’s where it gets tricky. Measurements of the strength and location of the Earth’s magnetic field imply that it has been changing a lot over the past 1000 years or more. First, it seems that the strength of the field has diminished by 50% over the last millennium. Second, over the last century, the magnetic North Pole has moved a lot – sometimes as much as 40 kilometers per year to the north! This “polar wander” means that compasses aren’t pointing to the same place they were 30 years ago. Does this mean the magnetic field is entering one of these periods of instability prior to a reversal?

Probably not. The magnetic field may have decreased in strength, but comparatively speaking, it is still over twice has high as it has been in other periods, so we’re not approaching any dire lack of protection. What we might be seeing is an excursion rather than a reversal, where the magnetic field gets more unstable and possibly weaker for hundreds to thousands of year, but then returns to its previous configuration. And although our current polarity has been around for quite a long time, we’re not “due” for a reversal because we don’t even know how often they occur.

That being said, the magnetic field will reverse at some point. Although it might not be a geologic hazard we tend to think about often, it is something that we might need to consider as an event that would bring global chaos. However, for now, we’re still safe in our magnetic bubble generated by our dynamic Earth.

References

CATEGORIZED UNDER: Rocky Planet, Science, Science Blogs
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Rocky Planet

Rocky Planet covers all the geologic events that made and will continue to shape our planet. From volcanoes to earthquakes to gold to oceans to other solar systems, I discuss what is intriguing and illuminating about the rocks beneath our feet and above our heads. Ever wonder what volcanoes are erupting? How tsunamis form and where? What rocks can tell us about ancient environments? How the Earth might change in the future? You'll find these answers and more on Rocky Planet.
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