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North Magnetic Dip Pole
JOURNEY TO THE TOP
(or - THE RELOCATED DIP)
The North Magnetic Pole - of interest to navigators for
centuries - but no one knew exactly where it was.
A study was done by the Department of Energy, Mines and Resources,
Geological survey of Canada, Geophysics Division, to determine the exact
location of the North Magnetic Dip Pole (NMDP). This is the location
where the north seeking end of the compass needle wants to point
straight into the ground. The study was published by the Canadian
Journal of Earth Sciences, Vol. 23, 1986. The study was authored by
L.R. Newitt and E.R. Niblett. This review is based on pages 1062
through 1067 of that study.
Back in 1831 a man by the name of J.C.ROSS (Ross 1834) was the first
person to plot where the NORTH MAGNETIC POLE was. Its rapid motion,
800 km in 150 years
(Barraclough and Malin 1981), has led to the
redetermination of its position several times since. It has
been customary for the Earth Physics Branch, Department of Energy,
Mines, and Resources, Canada, to redetermine its position approximately
once every decade.
The pole has moved approximately
750 km since 1904, an average of 9.4
km per year. From 1973, when the pole position was last determined,
to late 1983, the movement has been approximately 120 km, an average
of 11.6 km per year, only slightly more than the 80 year average. Its
present direction of travel is approximately northwest.
The North Magnetic Pole was found to be very active and elusive. When it was
approached by researchers, it would move. It was also found that the
pole was more active during the day than it was at night. Because of
this, several different methods and locations were used at the same time
to gather data. From all this information, the nature and the extent of
the movement of the NMDP could be plotted. The NMDP was tracked from
May 13 to May 18, 1984, and the information from all the methods and
sites used, was compiled into 6 hour intervals. During an active
cycle, it was found that the pole moved as much as 50 km from its mean
position. While in a quiet time, it only moved a maximum of about 12
km.
Because of this change, the
rate of declination
has changed, and the
line of 0° declination has moved to the west. It now passes through
the western most part of Hudson Bay (Churchill, Manitoba), through
Lake Superior, but now goes down the west side of Lake Michigan.
So where is the magnetic north pole you ask? At the end of 1983, the
magnetic north pole was north of Bathurst Island, south of King
Christian Island, and east by southeast of Lougheed Island at Latitude
77.0°N, longitude 102.3°W, and moving northwest at about 11.6 km per
year.
Editor's Note: The study "Relocation of the North Magnetic Dip Pole", used by permission (SARNEWS)
*** For an update (10 years later) see GSC North Pole Tracking the North Magnetic Pole.
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