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Starts With A Bang

Throwback Thursday: Exactly where you are

How to figure out your location on Earth with only the most primitive tools.

“And you may find yourself in another part of the world.
And you may find yourself behind the wheel of a large automobile.
And you may find yourself in a beautiful house, with a beautiful wife.
And you may ask yourself, ‘Well, how did I get here?’” –
Talking Heads

Imagine that you wake up one day, and find yourself in completely unfamiliar surroundings. You don’t know what day it is, what year it is, where you are or how you got here.

Image credit: ©2010–2015 SamuraiSunshine; photography from deviantART.

You could literally be anywhere.

All you have at your disposal is the elements of nature itself. Is there any way, without any other information, that you could figure out exactly where in the world you were?

=Image credit: World Map from

We typically describe our location on Earth by two coordinates: a latitude and a longitude. Latitude, your distance (either north or south) from the equator, in degrees, is actually very easy to figure out, assuming you know your astronomy and have some basic measuring tools.

All you have to do is find either the North (or South) Celestial Pole, depending on what hemisphere you’re in.

Image credit: R. L. McNish, retrieved from

Even though the Earth orbits the Sun, traveling a distance of 940 million kilometers a year, all while orbiting on its axis, the North Celestial Pole and South Celestial Pole always appear in the exact same position from any given latitude on Earth.

Look up at the night sky — on a good, clear night — and if you’re in the Southern Hemisphere, you should be able to see the following set of stars and what appear to be permanent, unmoving “clouds.”

Image credit: Fraser Gunn of New Zealand.

Along the band of the Milky Way, there’s the (true) Southern Cross, which you can tell apart from the false cross by the fifth star in the “left hip” position, as well as the two very bright pointer stars, Alpha (yellow/white) and Beta (blue) Centauri. Off the band of the Milky Way are two faint but prominent clouds, the Large and Small Magellanic Clouds, small satellite galaxies of our own, each over a hundred thousand light years away.

And if you can find these objects in the sky, you should have no problem finding the location of the South Celestial Pole, even though there isn’t a good star to mark the spot. Here’s how.

Image still by Fraser Gunn, additions by me.

Draw an imaginary line down the long axis of the cross, and also draw one perpendicular to (and from the middle of) the two pointer stars. Where those lines intersect is (approximately) the location of the South Celestial Pole.

Want to do a little better? The location of the Pole also makes an equilateral triangle with the two Magellanic Clouds; using these two methods together, you should easily be able to locate the South Celestial Pole to less than one degree.

Of course, if you’re in the Northern Hemisphere, things are even easier, because there are prominent stars to help you out.

Image credit: Wally Pacholka, via

Not only that, but one of them happens to be situated less than one degree from the North Celestial Pole itself! Simply follow the last two stars in the Big Dipper‘s “cup” up to the edge of the Little Dipper’s handle — the North Star — and you simply can’t miss it.

As the video below shows, the night sky will appear to rotate around the Pole Star, with a period of just under 24 hours, no matter what your location on Earth is. (And note the North Star in the upper-left corner.)

However many degrees your celestial pole appears to be above the horizon is exactly equal to your latitude. So if you’re in the northern hemisphere and the North Star is 40 degrees above the horizon, your latitude is 40° north. If the celestial pole is directly overhead (at 90° above the horizon), then you’re exactly at the pole itself. And if the celestial pole appears on the horizon itself, you’re at the equator: 0° latitude.

Image credit: Bob King, better known as Astrobob.

So that takes care of latitude: the easy one. But longitude is a very big problem. Unlike latitude, where different locations actually lead to significant differences in observable phenomena, longitude is arbitrary.

So if you want to measure your longitude, it’s going to be relative to some agreed-upon point. In other words, for a location to mean something you need some sort of prior knowledge. The easiest way to achieve this is to identify some place as zero degrees longitude, use what you know about astronomy to calculate when the Sun (or any star) rises and sets at different latitudes, and then carry a timepiece with you.

Image credit: Wikipedia user Ruryk.

And the easiest way to keep accurate time, as Christiaan Huygens discovered in the 17th Century, is with a pendulum clock. At any given location on Earth, an ideal pendulum — that is, a heavy mass connected to a fixed point by a massless string — has its period determined solely by two things: the acceleration due to gravity and the length of that pendulum.

Once this was understood, it became relatively straightforward to construct a seconds pendulum, or a pendulum where every swing, from one side to the other, took a time of (practically) exactly one second.

Image credit: Wikipedia user Lookang.

If you have a clock with you, and you know your latitude, and you also know when any astronomical body (i.e., the Sun) should be rising or setting, you can figure out your longitude with no problem at all!

Except, there are two problems with that. The first is that, as you move to different latitudes and elevations on Earth, the acceleration due to gravity changes!

Image credit: NASA/JPL/University of Texas Center for Space Research.

The Earth bulges at the equator and is compressed at the poles due to its rotation, making the acceleration due to gravity slightly larger at higher latitudes and slightly lower closer to the equator. Additionally, higher elevations mean you’re farther from the center of the Earth, and so gravity will be slightly higher at sea level and slightly lower at high altitudes.

Image credit: Adam Equipment, retrieved from Cole-Parmer.

This has been measured incredibly precisely by today’s standards, but this effect has been known (and accounted for) since the 1670s, by Jean Richer. Anyone traveling — and in possession of this knowledge — could lengthen or shorten their seconds pendulum slightly, dependent on their latitude and altitude, to keep the period constant. Once you know how to account for changes in gravity, you can calculate your longitude as you move without fear that those effects will throw you off.

But something else happens as you travel, something that is much harder to account for, and virtually impossible to control.

Image credit: James Weddell, retrieved from Linda Hall Library.

Temperature changes! As the temperature heats up or cools down, your pendulum will expand or contract along with the temperature change; that’s what virtually all materials do when you change their temperature!

But that would be terrible for your pendulum! If its length gets shorter, so does the period of one pendulum swing, and if the length gets longer, your swing time lengthens as well. If you don’t know to take this into account, unlike the gravimetry problem, above, a plunge into below-freezing temperatures can throw your clocks off by a minute or two per day, where every missed minute means an error in longitude of up to 28 kilometers. (Although this, too, is dependent on your latitude.) Since temperatures change all the time, and these errors are cumulative, using a simple pendulum clock could, over the course of a few months, lead to errors in your calculated longitude of thousands of kilometers, or a significant chunk of the Earth. All because, as the mesmerizing video below shows, pendulums of different lengths have different periods.

So how, then, could you avoid this problem? How can you overcome the perils of your material expanding/contracting in changing temperatures? How do you keep the length of your pendulum constant?

The answer, discovered not by Newton or Galileo but by the virtually unknown commoner, John Harrison, was simultaneously simple and brilliant. Here’s the concept applied to a pendulum.

Image credit: Wikipedia user Leonard G.

Use a combination of two different metals in your pendulum! Different elements expand by different amounts as the temperature changes, so you can take a material like iron, with a modest coefficient of thermal expansion, and a material like zinc, with a much higher coefficient of thermal expansion and make them work against each other. For the purposes of simplicity to illustrate this, let’s assume zinc expands three times as much as iron.

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Build two parallel iron rods that extend three-quarters of the way down the pendulum, two zinc rods that extend half the original length back up, and one more iron rod that’s three-quarters of the original length. Now, attach them together as shown in figure B, above, and let the temperature change!

What’s going to happen? As the temperature drops, the iron and zinc both contract. Sure, the zinc contracts three times as much, but the total iron is three times as long as the total amount of zinc! Since the zinc provides a negative distance but the iron a positive one, they — in effect — cancel each other out! If the temperature rises instead, the iron and zinc both expand, with the iron making the pendulum longer and the zinc making it shorter by amounts that, once again, cancel each other out! In other words, the temperature can change to anything it wants, and the overall length of the pendulum will stay the same, insensitive to temperature!

Image credit: screenshot from the Wikipedia page on pendula.

It’s a remarkable study in contrasts: the ease with which you can find your latitudes anywhere, but the incredible difficulty of longitude. For the latter, it not only takes some hard work, at the end of the day, it still takes a reference point to mean anything!

Still, how clever and simple is that temperature-compensation trick, to use different elements with different thermal expansion properties in combination, keeping the overall length constant! There’s a great book that tells this story in tremendous detail, but no matter what, I hope you remember to thank the stars for giving us the heavy elements needed to tackle this problem!

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