MadSci Network: Earth Sciences |
The earth's magnetic field can be viewed as if the earth were a very big bar magnet (this is a simplification, but one that works fine for most purposes). Magnets produce forces on other magnets and on magnetic materials. Magnets also have directions and every magnet has a north pole and a south pole. You can see this in action if you get a couple of refrigerator magnets and play with them. The forces produced will tend to attract magnetic materials to the magnet and will tend to both attract and repel other magnets in such a way that the magnets end up stuck together north pole touching south pole ___________ ___________ |_S_______N_||_S_______N_| So far, so simple, however magnets have three dimensional effects. The forces are most often described by a "field". This field is typically shown by lines that loop outward from the poles. Again, to oversimplify a little, these lines lie along the directions in which the magnetic force is acting. On the earth, the field loops run from south magnetic pole to north magnetic pole (more about poles in a bit). You can see a nice diagram of the field around a bar magnet and the earth at: http://liftoff.msfc.nasa.gov/academy/space/mag_field.html Near the equator (which has no significance for the magnetic field, it's just a marker halfway between the geographic poles) the field lines run north-south and are essentially parallel to the surface. By the time you reach the mid lattitudes, the lines still run north-south, but they are now at a significant angle to the surface. This angle is the magnetic inclination. Approaching the poles, the field lines get even steeper, until they are vertical at the pole itself. Looking from the side: -- -- \ \ | | _______ _\__\__ __|_|___ equator mid-latitude at pole The compass needle works because it's a small magnet in a big field and it is pushed by the forces between the earth and itself until it lines up with the earth's field lines. However, as you point out, the way we use a compass only uses two of the three dimensions of the field. If your compass needle were free to move in any direction, it would point north end down toward the ground as well as toward north. In fact, you can soemtimes see this downward deflection and some sophisticated compasses have adjustable weights on the south end of the needle to compensate for it and keep the needle level so that it swings freely. There are also compasses designed to swing only in a vertical plane that are specifically used to measure the inclination. These are called "dip needles" since they measure the dip, or downward angle, of the field. If you take a standard compass to the magnetic pole, then the needle, which swings in a horizontal plane is trying to align itself with a vertical field. The result is that the alignment of the needle is meaningless. In practical terms, the needle will probably swing wildly in response to any slight movements of the compass. If you want to know when you have found the magnetic pole, a compass is the worng instrument, what you need is a dip needle. When it goes completely vertical, you know you are there. A compass normally responds to earth's field, which is not very strong (if it were strong, you would have a hard time moving your fridge magnets around). Any magnets or magnetic materials will cause changes in that field or will completely overwhelm it, which is why compasses do not work well when held too near to steel belt buckles, Boy Scout kerchief holders, car bodies, or even rocks with magnetic minerals in them. If you wanted to see how a compass would behave at the north pole, you could get a good strong bar magnet and hold it vertically, then place your compass directly over the north pole end of the magnet. You also asked about the magnetic and geographic poles. They are different. The geographic pole is defined by the spinning of the earth and it is in the same spot all the time. This pole is the one that sits directly below Polaris, the north star. This is usually what people mean when they talk about the earth's poles. The magnetic north pole is defined by the earth's magnetic field, which is in turn defined by swirling currents within the liguid iron outer core. The magnetic pole is roughly aligned with the geographic pole, but wobbles around it, getting up to about 10 degrees away. This variation is what produces the magnetic declination, the difference between true north (geographic) and magnetic north. Declination varies from place to place and year to year as the magnetic pole wobbles. If you look at the positions of the pole over tens to hundreds of thousands of years, then the _average_ magnetic pole will be the same as the geographic pole. All of what I have said about the north pole is true also of the south pole, except there the north end of your compass needle would want to point straight up instead of straight down. A google.com search on the words magnetic field turned up the following, where you can find more information: http://lep694.gsfc.nasa.gov/lepedu/lepedu_hp.html http://csep10.phys.utk.edu/astr161/lect/earth/magnetic.html I hope this helps. David Smith, Ph.D. Geology, Environmental Science, and Physics, La Salle University, Philadelphia
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