In article <[email hidden]>, Peter Clinch
<[email hidden]> writes
Quoted message said:Bernard Hill said:But they can't be. So don't assume they must and define them in a
more logical way.
Well what is your "more logical way"?
It's a mathematical fact that the axis of rotation of any body contains
the centroid (centre of gravity). Furthermore the axis is easy to
define. So the logical way is that each position is defined in what
mathematicians call spherical polar coordinates: distance from the
centre+latitude+longitude.
These are defined and unique only on the assumption that an arbitrary
zero of latitude is chosen. And that's some particular spot in Greenwich
observatory, at some particular point in the past.
Quoted message said:
Quoted message said:Quoted message said:so given angular distances along it are constant,
??
x degrees along a parallel, angular distance should always be a
constant c km lomg. But if the surface is irregular (as it is), that
won't be the case. This is Not Good in a deterministic measurement
system...
Why? We don't expect that a distance on a map is the distance we walk -
we have to go up and down too. It seems good to me to have agreement
across the world...
Quoted message said:
Quoted message said:Of course. But that doesn't mean to say that there isn't a set of
coordinates which describe points on the surface. In mathematical
terms it's called Spherical Polar Coordinates: radius, latitude,
longitude. Conventionally called R, theta, phi. All you need to
define are where the zeroes of theta and phi are.
This isn't new stuff: it's centuries old.
It isn't new, but what it isn't is much use in practice on the Earth.
WGS84 gives a much better account of the real shape of the place than
an ellipsoid, which is what you need for sperical polars to work
consistently, accurately and usefully across the surface. Since maps
are of the surface, and not some reference ellipsoid, it makes a lot of
sense to use a reference model that more accurately reflects the
surface you're mapping.
Quoted message said:As I said, there can be defined one unique set of lat/long.
The issue isn't whether you can do it, it's is it actually useful in
practice. Lat/Long breaks down as a fully consistent system because
its assumed geometry is not the same as the earth's.
That doesn't make it break down at all! It gives a unique, true value
which we could use on maps. I can see that each country may want its own
grid reference - like Britain - but not that they each want their own
definition of what can be uniquely defined. That's why we agree on the
definition of metre (etc).
--
Bernard Hill
Selkirk, Scotland