Thanks for the info.  I don't mind you plugging your book, that was one of
the questions I asked : What is a good reference on this subject.

See this is where I start getting confused with terminology.  I'm talking
about KED (Kriging with External Drift) and then you start talking about
Universal Kriging.  If I understand correctly they are not the same thing?
With Universal Kriging you remove the trend and Krig the residuals but in
KED you use the trend(drift) in the actual krig matrix?

Mike

-----Original Message-----
From: Isobel Clark [mailto:[EMAIL PROTECTED]]
Sent: Thursday, December 06, 2001 11:18 AM
To: Michael Dennis
Cc: [EMAIL PROTECTED]
Subject: RE: AI-GEOSTATS: Kriging with External Drift


> I'll see if I can get a
> copy of the book you mention to look at to see if it
> helps me out.
>
> You say that KED uses a shape function for the
> "Drift" data.
'shape functions' can be anything you like but most
people stick to simple polynomials. To use Univeral
Kriging the only constraint is that it has to be
expressed as a linear function in the coefficients.
That is: b0 + b1 * some function + b2 * some other
function and so on, where the b's are the
coefficients.

All this is explained in detail in Chapter 12 of
Practical Geostatistics 2000, but we aren't allowed to
say that on the open list ;-)

You can try it out free (completely) with the kriging
game in my briefcase. This shows you the equations and
the terms calculated. A full tutorial on Universal
Kriging is also available in the briefcase and can be
run with the free PG2000 software.

Find them all at:

http://uk.geocities.com/drisobelclark/briefcase.html

Let us know if we can be of further help.

Isobel Clark

________________________________________________________________
Nokia 5510 looks weird sounds great.
Go to http://uk.promotions.yahoo.com/nokia/ discover and win it!
The competition ends 16 th of December 2001.


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