If the variances are minimal then I don't really need them. All I am doing
is providing an automatically calculated magnetic declination for any
location in NZ. I know that the total variance across the country is only
about 2-3 degrees (although this can be quite significant over long
distances), but wasn't sure of the scale of local anomalies.

Is the IGRF model very different from the WMM model? I had a quick look at
the IGRF coefficients and they look fairly similar.

Cheers,
Phil.
----- Original Message ----- 
From: "Phil Scadden" <[EMAIL PROTECTED]>
To: "NZ Borland Developers Group - Delphi List" <[EMAIL PROTECTED]>
Sent: Tuesday, April 20, 2004 11:37 AM
Subject: Re: [DUG] Converting some code from C


> > When you say that you can calculate for any year, surely those
calculations
> > are dependent on coefficients that are only valid for the current epoch
(or
> > for past epochs). The coefficients are recalculated every 5 years
because
> > simple extrapolation is too innacurate. Haven't looked at the IGRF
files,
> > but assumed that they also work of coefficients. Is that the case?
>
> The IGRF files contain coefficients for each 5 year epoch. "any" year
sorry
> means any year within that range.
>
> > The WMM-2000 model is a Low-Resolution model - you don't happen to have
a
> > high resolution model for NZ do you?
>
> Now this is an issue as to what you are trying to achieve. The global
> magnetic model is supposed to represent the mantle-modified main field,
> free of crustal effects. You map crustal effects by comparing what you
> actually measure at an xy point and subtract the global model. This leaves
> you with magnetic anomaly map which is what geophysicists are extremely
> interested in because it highlights crustal differences. I coded the IGRF
> model precisely for this purpose - so I can produce anomaly maps from
> all the total field measurements I have to hand.
>
> Now higher-resolution total-field maps (the actual magnetic field at xy)
do
> exist for NZ but I would be very curious as to why you would want one. The
> local anomalies differ from IGRF by amounts so small that a good
> magnetometer is needed to detect them.
>
> > Cheers,
> > Phil.
> >
> > ----- Original Message ----- 
> > From: "Phil Scadden" <[EMAIL PROTECTED]>
> > To: "NZ Borland Developers Group - Delphi List" <[EMAIL PROTECTED]>
> > Sent: Tuesday, April 20, 2004 9:10 AM
> > Subject: Re: [DUG] Converting some code from C
> >
> >
> > > > where the m is not used in the loop and should have just been
> > initialised
> > > > outside it! There's more, but you get the idea. </rant> It also
doesn't
> > help
> > > > that I'm translating code that carries out calculations that are
well
> > above
> > > > my comprehension (calculates the 2000 Epoch World Magnetic Model for
a
> > given
> > > > Lat, Long, Altitude, and Year using spherical-harmonic Gauss
> > coefficients -
> > > > whatever they are). Cheers, Phil.
> > >
> > > Well those calculations are also available in Fortran if you prefer. I
> > > translated those earlier in the year into VBA for ArcGIS, but was
using
> > the
> > > IGRF files so can calculate for any year, any lat/long.
> > >
> > > ----------------------------------------------------------
> > > Phil Scadden, Institute of Geological and Nuclear Sciences
> > > 764 Cumberland St, Private Bag 1930, Dunedin, New Zealand
> > > Ph +64 3 4799663, fax +64 3 477 5232
> > >
> > > _______________________________________________
> > > Delphi mailing list
> > > [EMAIL PROTECTED]
> > > http://ns3.123.co.nz/mailman/listinfo/delphi
> > >
> >
> > _______________________________________________
> > Delphi mailing list
> > [EMAIL PROTECTED]
> > http://ns3.123.co.nz/mailman/listinfo/delphi
>
>
> ----------------------------------------------------------
> Phil Scadden, Institute of Geological and Nuclear Sciences
> 764 Cumberland St, Private Bag 1930, Dunedin, New Zealand
> Ph +64 3 4799663, fax +64 3 477 5232
>
> _______________________________________________
> Delphi mailing list
> [EMAIL PROTECTED]
> http://ns3.123.co.nz/mailman/listinfo/delphi
>

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