Be cautious when using any geomagnetic declination information.  There are
both spatial and short-term temporal variations not accounted for by model
magnetic fields.  The r.m.s. value for a predicted declination is typically
better than 0.5 degrees but the actual error at a given location and time
could be larger and is influenced by local geology, cultural features and
activity, and ionospheric and magnetospheric processes.  While a compass might
be useful for initial orientation of a sundial, satellite dish, etc., final
alignment is best done using the "signal" itself whether it be a TV picture or
the sun's shadow.
-- Richard Langley
   Professor of Geodesy and Precision Navigation


On Thu, 12 Nov 1998, Fernando Cabral wrote:

>
>
>Peter Mayer wrote:
>
>> On 11/11/98 Greg Milsom wrote,
>> >Today I learned that one of the reasons my new dial was not as exact as
>> >I had hoped was because the magnetic variation I was using to align the
>> >dial was several years old and that magnetic variation does in fact
>> >change over time.
>
>You can get precise magnetic declination from several sites in the Internet.In
>the end of this message I put a message from Tom McHugh that
>points toward geomag, a DOS-based program that calculates the
>magnetic declination for several years, any coordenates.
>
>I think among the the URLs I used are: http://geomag.usgs.gov/
>
>On the other hand, I don't think I would use a magnetic compass
>to orient a sundial. I think it is too error prone. I would use the
>sun itself instead.
>
>I don't know your coordenates and I can not get any hints from your
>e-mail address (since it is not based on the ISO (country) schema).
>If you are in the Northen Hemisphere, this is a good season to
>find the North/South line using the sun since it is now approaching the
>tropic in the Southern Hemisphere (Capricorn) and it moon shadow
>in the Northen Hemisphere is quite long.
>
>Here is what I would do: use Luke's sun calculator to find
>the transit time at your longitude.http://www.gcstudio.com/suncalc.html
>
>Put a short, vertical gnomon. Make sure it is really vertical.
>With a precise watch mark the shadow at transit time. The
>sun will be due South, the shadow points towards the North.
>
>> Dear Greg,
>>         It does change, alas.  A while ago I created an Excel spreadsheet,
>> based on the equations in Meus' book which seemed to get correct answers.
>> I only set it up to calculate single days, but that could be modified.
>> Since it was created solely for my own amusement, it comes with little or
>> no documentation, but if you want to play with it, let me know (and what
>> encoding standard your e-mail browser uses) and I can try to send it to
>> you.
>>
>
>Peter
>
>I am interested in this Excel Spreadsheet. I am right now implementing
>fer j. de vries' algorithms (http://iaehv.nl/users/ferdv/definit.htm). One of
>the
>problems I have is checking every step.
>So, a spreadsheet like your may be useful for me to check the results of
>my program.
>
>
>>         Peter Mayer
>>
>> ----------------------------------------------------------------------
>> Peter Mayer                 | [EMAIL PROTECTED]
>> Politics Department         | 'phone:+61.8 8303 5606/5610
>> University of Adelaide      | FAX: (+61.8) 8303 3446
>> Adelaide, SA 5005           | Time Zone: GMT +9.5 hrs (April-October)
>> AUSTRALIA                   |            GMT +10.5 hrs(November-March)
>> ----------------------------------------------------------------------
>
>
>Subject:
>            Fw: Fw: Magnetic North Pole
>       Date:
>            Mon, 28 Sep 98 21:11:26 -0400 (EST)
>      From:
>            "Tom Mchugh" <[EMAIL PROTECTED]>
>        To:
>            [EMAIL PROTECTED]
> References:
>            1 , 2
>
>
>
>
>Fernando,
>
>I found these e-mails on the subject of magnetic north, dating
>from November last year (see quoted material below).  I hope
>this helps you
>
>Tom McHugh
>
>R. R. 1, Box 896
>Fort Fairfield, ME 04742
>USA
>
>46N45' 13"
>67W48' 42"
>
>
>
>****************************************************************************
>******************
>----------
>> Date: Saturday, November 08, 1997 15:25:45
>> From: Richard Langley
>> To: k.schwarzinger
>> Cc: Sundial List
>> Subject: Re: Fw: Magnetic North Pole
>>
>> On Sat, 8 Nov 1997, k.schwarzinger wrote:
>>
>> > Richard,
>> >
>> > thank you very much for your answer about the magnetic North
>> > Pole.
>> >
>> > It is very practically to found the magnetic declination for each
>> > point of the earth and every year.
>> >
>> > I have entered the geographical coordinates of my home :
>> > Latitude: 47 Degees 14 Min (North) and Longitude: -11 Degrees
>> > 27 Min (East) and the year 1997.
>> > I got the message :
>> >
>> > "The magnetic declination in 1997 at Latitude 47 Degees 14 Min
>> > N  and Longitude -11 Degrees 27 Min W (!) = 0 Degrees
>> > 40 Min E.
>> >
>> > Why  -11 W (West?) ! Why is 'East' not indicated ?
>> >
>> > Karl.
>> > [EMAIL PROTECTED]
>>
>> Karl:
>>
>> It is very common in North America (except in geodetic circles!) to treat
>west
>> longitudes as positive.  The software was written primarily for the use of
>> Canadians hence the sign bias. The geodetic convention is to treat east
>> longitudes as positive.  Of course, then North Americans would have -66
>E! :-)
>>
>>
>> By the way, there is another geomagnetic field program that can be
>accessed on
>> the Internet.  It's hosted by the U.S. Geological Survey and is available
>via
>> telnet: neis.cr.usgs.gov. Log in ID is QED.  This software is not
>> "North-American-centric."
>>
>> Here's the information on how to run the on-line program:
>>
>> GEOMAG provides values of the elements and parameters of the Earth's
>magnetic
>> field.  The values are estimates based on mathematical models.  Values of
>the
>> following elements and their rates of change are available:
>>
>>     D - Declination (also called compass variation; east declination is
>>           considered positive, west declination negative)
>>     I - Inclination (also called dip; downward inclination is considered
>>           positive, upward inclination negative)
>>     H - Horizontal intensity
>>     X - North component
>>     Y - East component
>>     Z - Vertical intensity (considered positive downward, negative upward)
>>     F - Total intensity
>>
>> Positions of the Magnetic Poles and parameters of the centered and
>eccentric
>> geomagnetic dipoles are also available.
>>
>> You will be prompted to select a field model and to enter the date and
>> geographic coordinates (latitude, longitude, and elevation) of locations
>of
>> interest.  If you are unsure of how to respond to any prompt, enter a
>question
>> mark (?) to get help.  If you would like the program to back up to the
>> previous prompt, enter a caret (^) (that is, the SHIFTed-6 key, not the
>> UP-ARROW key).  If a default response (shown in brackets) is available
>and is
>> suitable, you may select it simply by pressing RETURN.  To quit the
>program,
>> press CTRL-Z (hold down the Control key and press Z).
>>
>> (Reminder:  Enter <?> for help, <^> to back up, <CTRL-Z> to quit.)
>>
>> Options:
>>   1 = Field Values (D, I, H, X, Y, Z, F)
>>   2 = Magnetic Pole Positions
>>   3 = Dipole Axis and Magnitude
>>   4 = Magnetic Center
>>
>> -- Richard Langley
>>    Professor of Geodesy and Precision Navigation
>>
>
>>
>>
>============================================================================
>==
>> =
>>  Richard B. Langley                         Internet: [EMAIL PROTECTED] or
>[EMAIL PROTECTED]
>>
>>  Geodetic Research Laboratory               BITnet:   [EMAIL PROTECTED] or 
>> [EMAIL PROTECTED]
>
>>
>>  Dept. of Geodesy and Geomatics Engineering Phone:    (506) 453-5142
>
>>
>>  University of New Brunswick                FAX:      (506) 453-4943
>
>>
>>  Fredericton, N.B., Canada  E3B 5A3         Telex:    014-46202
>
>>
>>       Fredericton?  Where's that? See: http://www.city.fredericton.nb.ca/
>>
>============================================================================
>==
>> =
>>
>>
>****************************************************************************
>********************************************************
>
>****************************************************************************
>********************************************************
>>On Fri, 7 Nov 1997, k.schwarzinger wrote:
>
>>> Dear all,
>>>
>>> is there in the INTERNET a website, which gives informations
>>> about the curent value from the declination of the magentic
>>> North Pole ?
>>>
>>> Are there still informations about the situation of the magnetic
>>> North Pole ( INTERNET or literature ) ?
>>>
>>> Thanks for any help.
>>>
>>> Regards
>>> Karl.
>
>>http://www.geolab.nrcan.gc.ca/geomag/e_cgrf.html
>
>
>>===========================================================================
>====
>> Richard B. Langley                         Internet: [EMAIL PROTECTED] or
>[EMAIL PROTECTED]
>> Geodetic Research Laboratory               BITnet:   [EMAIL PROTECTED] or 
>> [EMAIL PROTECTED]
>
>> Dept. of Geodesy and Geomatics Engineering Phone:    (506) 453-5142
>
>> University of New Brunswick                FAX:      (506) 453-4943
>
>--
>Fernando Cabral                         Padrao iX Sistemas Abertos
>mailto:[EMAIL PROTECTED]              http://www.pix.com.br
>                                        mailto:[EMAIL PROTECTED]
>Fone: +55 61 321-2433                   Fax: +55 61 225-3082
>15? 45' 04.9" S                         47? 49' 58.6" W
>19? 37' 57.0" S                         45? 17' 13.6" W
>
>
>

                                                                                
=============================================================================== 
 Richard B. Langley                            E-mail: [EMAIL PROTECTED]  
 Geodetic Research Laboratory                  Web: http://www.unb.ca/GGE/
 Dept. of Geodesy and Geomatics Engineering    Phone:    +1 506 453-5142      
 University of New Brunswick                   Fax:      +1 506 453-4943      
 Fredericton, N.B., Canada  E3B 5A3        
     Fredericton?  Where's that?  See: http://www.city.fredericton.nb.ca/
=============================================================================== 

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