| Magnetic Variation |
| The important thing here is to remember that
a compass points not to true north (e.g. the north pole, the
geographical northernmost point of the Earth) but to magnetic
north (the magnetic north end of the Earth's 'bar magnet').
These two are not in the same position (indeed the position
of magnetic north varies with time).
The apparent position of magnetic north will vary according
to your location in the world (most importantly your latitude)
and you will need to know the difference between these two
positions (magnetic and true north) to take an accurate bearing.
Information on the deviation between the two will be found
on any (Ordnance Survey) map, and should not be assumed as
it can vary by a relatively large amount according to your
location.
If the deviation is not given you can find it from the Pole
Star or by using the watch method to point to north (see Tracking
- Direction Finding methods). Then lining up the compass with
the grid lines on the map you can discover the variation if
there is one.
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Darren Dowling
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Connected is a central area that provides links to obtain
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From here you can go on to websites related to your area of
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| Magnetic Variation |
Darren Dowling
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- Locate the information on your map that tells you about
the local magnetic variation. This can be found in the Key
and also on the map itself. For the time being let us learn
how to use the information on the key.

'Different' Norths
On a typical Landranger type map the information will
look like this
Reproduced by kind permission of the
Ordnance Survey. MC 99/ 91
Difference of true north from grid north at sheet corners
NW corner - 1° 20' (24 mils) E
NE corner - 0° 54' (16 mils) E
SW corner - 1° 19' (23 mils) E
SE corner - 0° 53' (16 mils) E
Magnetic north varies with place and time. The direction
for the centre of the sheet was about 4 ½°
(80 mils) W of grid north in 1990 decreasing by about
½ ° (9 mils) in the next three years.
To plot the average direction of magnetic north join
the point circled on the south edge of the sheet to the
point on the protractor scale on the north edge at the
angle estimated for the current year.
Note the last paragraph. This will be explained later.
- To compensate for the angular difference take note of
the average variation for the sheet (this is more than acceptable
for any sensible work. If you really want to be perfect,
take note of the difference between true north and grid
north too). In our example sheet above this would give us
a value of around 4° (4 ½° - ½°
as we are long past 1990). (Note: A difference of 4°,
if you walked in a straight line for 10 km would mean you
would be around 700m away from your intended destination.
So for most everyday uses of bearings the difference is
negligible over sensible distances)
- Measure your bearing as you would normally, ignoring
magnetic variation.
- When you have your bearing adjust the value by 4°.
In our case we would have to ADD
4° to our bearing value to get a 'true-to-life' direction.
If the diagram indicated that grid north lay to the left
of magnetic north, you would have to subtract the angle
from the bearing.
- You can now follow your compass bearing safe in the knowledge
that you will be heading in the correct direction.
Note: If you intend to reverse this
process...that is to take a bearing from the 'field' and read
it back onto the map then you will need to SUBTRACT
the 4°.
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| Plotting Variation on Ordnance
Survey Maps |
Darren Dowling
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Note the last paragraph in the map extract on magnetic variation
above. If you look carefully at your map, at the top and bottom
of the map (usually in the centre) will be the following information.

Extract from the top of the map

Extract from the bottom of the map
If you draw two lines connecting the circle at the bottom
to the two arrows at the top of the map you will have a large
version of the diagram in the first table going across your
map. This will illustrate how the magnetic variation becomes
increasingly important the further the distance you are travelling
in a straight line. Imagine travelling 40 km (40 grid squares)
along these lines, and then look at how far away from your
intended destination you will be (measure 40 km along each
line and compare the distance between the two end points).
This would be your error if you did not take magnetic variation
into account. (On this map the distance is almost exactly
4 km 'as the crow flies') As I have said earlier, if you think
about it this is not a great deal (in relation to other errors
and considering that we very rarely travel 40 km in a straight
line without any checks that is...of course 4 km on its own
IS a large error!), and for most situations we do not concern
ourselves with this correction, but in some work it may be
important, and it may be more important at your location.
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