[Proj] Re: Graduated equidistant projections for convenient co-ordinate transformations
Michael Ossipoff
mikeo2106 at msn.com
Thu Aug 2 17:25:01 PDT 2007
Daan--
You wrote:
It's very uncommon for a map projection to satisfy two metric criteria
simultaneously.
I reply:
Yes, and thats why the sinusoidal projection is so remarkable. Its
equidistant and its equal-area.
And not just equidistant. Not only are the parallels truly-spaced and
uniformly divided, but theyre all truly divided.
Weve discussed two desiderata for a data map: Ive mentioned the
desirability of feasibly, hopefully easily, finding out if a particular
place is within a certain zone on the map. What good is a data map if you
cant determine that? You mentioned that people expect a data map to be
equal-area. Ok, the sinusoidal has both of those desired properties.
As the price for those properties, the sinusoidal doesnt do well by scale
variation, distances, and directions (unless its a world map, because
interruption is accepted for world maps).
But how fair is it to judge a data map according to how well it works as
navigational map? It isnt a navigational map. Its a special purpose map
for showing _where_ certain spatial distribution zones are.
For example, the gnomonic projection too is a special purpose projection,
for showing great circles as straight lines. No one criticizes the gnomonic
for not being a good source of accurate distances, directions or areas. They
dont, because they know that that is not what its for. Likewise for a
spatial distribution map.
The hiker isnt going to depend on an atlas rainfall-distribution map or a
species range map in a nature guidebook to determine the distances and
directions that s/he needs. How far is the rare salamander habitat from the
trailhead, and what heading should the compass be set for? S/hell find that
out from another map, probably a USGS topographic map.
Does a botanist or wildlife biologist want to know how wide a habitat range
is, or its distance from the nearest river or lake? For one thing, I
question whether s/hell need that more often than s/hell need to know the
position of the habitat ranges boundaries. And, when s/he needs that, and
has gotten some lat/long co-ordinates from an equidistant projection, then
s/he can calculate the distance, or get it from a map better suited for that
than is a little atlas or guidebook range map.
And does a botanist or wildlife biologist really need to get that
information from a little distribution map in a public-consumption atlas or
nature guidebook purchased in a bookstore?
Its difficult to find a scenario in which someone needs accurate distances
from an atlas spatial distribution map or a nature guidebook species range
map. But what makes those maps unique is that they tell where those zones
are, and Im merely asking that they do so _usably_.
You wrote:
You certainly can't get the best distance measurements AND the equidistant
property simultaneously.
I reply:
Well, for the most accurate distances, you can calculate them as accurately
as you want to from a conformal map. Thats more feasible with a conformal
because, at any particular point, the scale is the same in ever direction.
But if youre referring to distances measured directly from the map, without
being corrected for scale in its part of the map, I dont know that
equidistant maps do worse. The sinusoidal, Bonne, and Stabius-Werner have
more scale variation because they concentrate their distortion in the
corners. And the sinusoidal more so, because its an equatorially-centered
map, rather than a locally-centered map.
But, considering for instance the conic projections, the equidistant doesnt
do badly in comparison to the other conics. The equal area conic has more
scale variation than the equidistant or the conformal. If the parallel with
the largest east-west scale has 1.1 times the east-west scale of the
parallel with the smallest east-west scale, then, to make up for that and
maintain equal area, that first parallel must have 1.1 times _less_
north-south scale, in comparison to the second parallel. Resulting in a
maximum scale variation factor of 1.21 instead of just 1.1 Equal area maps
square the maximum scale variation factor. They do _worst_ by the standard
of scale-variation. And equal area maps are the ones that cartographers like
for data maps.
Equidistant conic has pretty much the same scale variation as conformal
conic. But if the equidistant conic spaces its parallels truly, then its
typical, average distances, measured according to its official scale, will
be more accurate than on the conformal, because typically the distances on
the equidistant conic will have some north-south component, and thats the
direction in which scale is true.
So, in that regard, equidistant looks best, and equal area looks worst.
And, as I said, after getting two points lat and long co-ordinates from an
equidistant projection, you can calculate accurate great circle distances
and directions. More accurate than you could measure directly from any map.
On no map are distances always accurate. But they are when you calculate
them from the accurate lat/long co-ordinates that you get from an
equidistant map.
Of course, if distances, including route distances, were the important
thing, then the conformal maps would, because route distances can be
calculate on a conformal as accurately as you want to.
Anyway, it seems to me that the sinusoidal is what satisfies the person who
is interested in the areas of the zones, and also the person who is
interested in _where_ the zone boundaries are.
Sometimes it seems as if cartographers regard data maps as just general
purpose maps on which zones have been drawn, and therefore want them to have
the same properties that they look for in general purpose maps. Atlases
often use, for data maps, the same projection that they use for their
general purpose maps.
It seems to me that the sinusoidal is the projection that would please
everyone, accurately and conveniently giving the two kinds of information
that people actually need, want, and use on a data map.
I understand that, for instance, course-instructors might want spatial
distribution maps that show their students how the total area of the Earths
boreal forest compares to that of the tropical rainforest, etc.
You wrote:
You don't see more maps on the projections you describe because not many
people share your priorities.
I reply:
I certainly cant argue with that.
I guess sinusoidal isnt going to become widely used for data maps, because
cartographers apply general-purpose requirements to those special purpose
maps.
Im the first to admit that Im the only person Im aware of who has
expressed the preferences that Ive been expressing here.
So then what would be a more realistic request for me to make to the
publishers of atlases and nature guidebooks? Id ask them to at least avoid
the azimuthal equal-area projection. Or, if they must use it, then at least
state, somewhere, the X,Y map co-ordinates, and the lat/long co-ordinates,
of the projections center. If they dont want to write it on the map page,
the could have it on part of one page of an appendix. So that someone could
find the position of zone boundaries without having to first solve a system
of five simultaneous nonlinear equations to find the projections center and
orientation.
Id ask them to avoid the polyconic too. It isnt that the polyconic is more
difficult than other projections. Its that it has no properties, has
nothing to justify its use for a data map.
The polyconic is often used to map the U.S. But its the wrong projection
for a country of east-west extent.
Better yet, to make the request more complete, Id recommend that publishers
only use the following kinds of projections for data maps:
Cylindrical, conic, polar azimuthal (and maybe oblique azimuthal if they
tell the maps center position [in map co-ordinates and lat/long
co-ordinates] and the maps orientation about that center), and
pseudocylindrical.
Well, usually the only major offender is the azimuthal equal area map,
without the information that should go with it. If it werent for that one,
I might not have posted these messages.
But this list is proof that Im not the only person who is interested in
co-ordinate transformations and considers them important, and wants ways of
making them more feasible. In fact just the other day, on this list, there
was discussion about software for transforming from the azimuthal equal
areas map co-ordinates to lat/long co-ordinates. Exactly the transformation
that motivated me to post here, on the very projection that creates the most
difficulty for the person who wants positions of zone boundaries on a data
map. But how would you like it if you had to solve a system of five
simultaneous nonlinear equations, to find the position of the projections
center (in both co-ordinate systems) and its orientation about that center,
before you could begin the actual co-ordinate transformation task?
Michael Ossipoff
I have a better idea of where you're coming from now. I see your need, more
or less, though you seem more interested in precise coordinate inversion
than I really see the need for. You don't see more maps on the projections
you describe because not many people share your priorities. Be careful not
to get too cavalier about the other traits. It's very uncommon for a map
projection to satisfy two metric criteria simultaneously. You may mean that
you can get good "enough" distance measurements even wit your "graduated"
equidistant, but good "enough" for you might not be good enough for someone
else. You certainly can't get the best distance measurements AND the
equidistant property simultaneously
Daan--
You wrote:
It's very uncommon for a map projection to satisfy two metric criteria
simultaneously.
I reply:
Yes, and thats why the sinusoidal projection is so remarkable. Its
equidistant and its equal-area.
And not just equidistant. Not only are the parallels truly-spaced and
uniformly divided, but theyre all truly divided.
Weve discussed two desiderata for a data map: Ive mentioned the
desirability of feasibly, hopefully easily, finding out if a particular
place is within a certain zone on the map. What good is a data map if you
cant determine that? You mentioned that people expect a data map to be
equal-area. Ok, the sinusoidal has both of those desired properties.
As the price for those properties, the sinusoidal doesnt do well by scale
variation, distances, and directions (unless its a world map, because
interruption is accepted for world maps).
But how fair is it to judge a data map according to how well it works as
navigational map? It isnt a navigational map. Its a special purpose map
for showing _where_ certain spatial distribution zones are.
For example, the gnomonic projection too is a special purpose projection,
for showing great circles as straight lines. No one criticizes the gnomonic
for not being a good source of accurate distances, directions or areas. They
dont, because they know that that is not what its for. Likewise for a
spatial distribution map.
The hiker isnt going to depend on an atlas rainfall-distribution map or a
species range map in a nature guidebook to determine the distances and
directions that s/he needs. How far is the rare salamander habitat from the
trailhead, and what heading should the compass be set for? S/hell find that
out from another map, probably a USGS topographic map.
Does a botanist or wildlife biologist want to know how wide a habitat range
is, or its distance from the nearest river or lake? For one thing, I
question whether s/hell need that more often than s/hell need to know the
position of the habitat ranges boundaries. And, when s/he needs that, and
has gotten some lat/long co-ordinates from an equidistant projection, then
s/he can calculate the distance, or get it from a map better suited for that
than is a little atlas or guidebook range map.
And does a botanist or wildlife biologist really need to get that
information from a little distribution map in a public-consumption atlas or
nature guidebook purchased in a bookstore?
Its difficult to find a scenario in which someone needs accurate distances
from an atlas spatial distribution map or a nature guidebook species range
map. But what makes those maps unique is that they tell where those zones
are, and Im merely asking that they do so _usably_.
You wrote:
You certainly can't get the best distance measurements AND the equidistant
property simultaneously.
I reply:
Well, for the most accurate distances, you can calculate them as accurately
as you want to from a conformal map. Thats more feasible with a conformal
because, at any particular point, the scale is the same in ever direction.
But if youre referring to distances measured directly from the map, without
being corrected for scale in its part of the map, I dont know that
equidistant maps do worse. The sinusoidal, Bonne, and Stabius-Werner have
more scale variation because they concentrate their distortion in the
corners. And the sinusoidal more so, because its an equatorially-centered
map, rather than a locally-centered map.
But, considering for instance the conic projections, the equidistant doesnt
do badly in comparison to the other conics. The equal area conic has more
scale variation than the equidistant or the conformal. If the parallel with
the largest east-west scale has 1.1 times the east-west scale of the
parallel with the smallest east-west scale, then, to make up for that and
maintain equal area, that first parallel must have 1.1 times _less_
north-south scale, in comparison to the second parallel. Resulting in a
maximum scale variation factor of 1.21 instead of just 1.1 Equal area maps
square the maximum scale variation factor. They do _worst_ by the standard
of scale-variation. And equal area maps are the ones that cartographers like
for data maps.
Equidistant conic has pretty much the same scale variation as conformal
conic. But if the equidistant conic spaces its parallels truly, then its
typical, average distances, measured according to its official scale, will
be more accurate than on the conformal, because typically the distances on
the equidistant conic will have some north-south component, and thats the
direction in which scale is true.
So, in that regard, equidistant looks best, and equal area looks worst.
And, as I said, after getting two points lat and long co-ordinates from an
equidistant projection, you can calculate accurate great circle distances
and directions. More accurate than you could measure directly from any map.
On no map are distances always accurate. But they are when you calculate
them from the accurate lat/long co-ordinates that you get from an
equidistant map.
Of course, if distances, including route distances, were the important
thing, then the conformal maps would, because route distances can be
calculate on a conformal as accurately as you want to.
Anyway, it seems to me that the sinusoidal is what satisfies the person who
is interested in the areas of the zones, and also the person who is
interested in _where_ the zone boundaries are.
Sometimes it seems as if cartographers regard data maps as just general
purpose maps on which zones have been drawn, and therefore want them to have
the same properties that they look for in general purpose maps. Atlases
often use, for data maps, the same projection that they use for their
general purpose maps.
It seems to me that the sinusoidal is the projection that would please
everyone, accurately and conveniently giving the two kinds of information
that people actually need, want, and use on a data map.
I understand that, for instance, course-instructors might want spatial
distribution maps that show their students how the total area of the Earths
boreal forest compares to that of the tropical rainforest, etc.
You wrote:
You don't see more maps on the projections you describe because not many
people share your priorities.
I reply:
I certainly cant argue with that.
I guess sinusoidal isnt going to become widely used for data maps, because
cartographers apply general-purpose requirements to those special purpose
maps.
Im the first to admit that Im the only person Im aware of who has
expressed the preferences that Ive been expressing here.
So then what would be a more realistic request for me to make to the
publishers of atlases and nature guidebooks? Id ask them to at least avoid
the azimuthal equal-area projection. Or, if they must use it, then at least
state, somewhere, the X,Y map co-ordinates, and the lat/long co-ordinates,
of the projections center. If they dont want to write it on the map page,
the could have it on part of one page of an appendix. So that someone could
find the position of zone boundaries without having to first solve a system
of five simultaneous nonlinear equations to find the projections center and
orientation.
Id ask them to avoid the polyconic too. It isnt that the polyconic is more
difficult than other projections. Its that it has no properties, has
nothing to justify its use for a data map.
The polyconic is often used to map the U.S. But its the wrong projection
for a country of east-west extent.
Better yet, to make the request more complete, Id recommend that publishers
only use the following kinds of projections for data maps:
Cylindrical, conic, polar azimuthal (and maybe oblique azimuthal if they
tell the maps center position [in map co-ordinates and lat/long
co-ordinates] and the maps orientation about that center), and
pseudocylindrical.
Well, usually the only major offender is the azimuthal equal area map,
without the information that should go with it. If it werent for that one,
I might not have posted these messages.
But this list is proof that Im not the only person who is interested in
co-ordinate transformations and considers them important, and wants ways of
making them more feasible. In fact just the other day, on this list, there
was discussion about software for transforming from the azimuthal equal
areas map co-ordinates to lat/long co-ordinates. Exactly the transformation
that motivated me to post here, on the very projection that creates the most
difficulty for the person who wants positions of zone boundaries on a data
map. But how would you like it if you had to solve a system of five
simultaneous nonlinear equations, to find the position of the projections
center (in both co-ordinate systems) and its orientation about that center,
before you could begin the actual co-ordinate transformation task?
Michael Ossipoff
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