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Azimuthal equidistant projection and rgdal

Dear Johan (and list),

you are right in the first case: I think the result is expected. Using global 
data with this sort of projection will look kind of awful - the equatorial 
azimuthal equidistant illustrations in Snyder do not try to map data for the 
whole planet - they employ a hemisphere.

When I clip the results to a hemisphere:
dta <- map("world",  xlim=c(-180, 0), ylim=c(-90,90), plot=FALSE)
...
dta2 <- spTransform(dta1, CRS("+proj=aeqd +lat_0=0 +lon_0=-0"))
plot(dta2, axes=TRUE)

the result looks pretty similar to what I see in Snyder's work.

That said... it is strange to me that using your global data the projection 
does NOT wrap around when doing a polar azimuthal projection, but then it does 
when you do not. This may not be on-topic for this stats list - I wonder if 
you could reach out to the GDAL community if you still have questions?

Yours,

Ashton
On 11/13/12, Johan Mazel, wrote:
-----
Ashton Shortridge
Associate Professor			ashton at msu.edu
Dept of Geography			http://www.msu.edu/~ashton
235 Geography Building		ph (517) 432-3561
Michigan State University		fx (517) 432-1671