Tissot's indicatrix of the projection that maps the sphere onto the faces
of the grid's solid (Snyder's equal-area projection, or Fuller's): a small
circle on the sphere maps to an ellipse on the face, with semi-axes
a and b times the circle's radius.
Arguments
- x
A HexGridInfo object from
hex_gridwith an ISEA grid. H3 is built on a gnomonic projection of its own and is not covered.- lon, lat
Longitudes and latitudes in degrees.
Value
A data frame with one row per point: lon, lat,
face (from 0), the scale factors a (largest) and b
(smallest), the maximum angular deformation angular
\(2 \arcsin((a - b) / (a + b))\) in degrees, the areal scale
areal \(a b\), and angle, the direction of the longer
axis on the face plane in degrees anticlockwise from the face's x axis.
Details
The scale factors are the singular values of the projection's derivative,
computed exactly by forward-mode automatic differentiation of the
projection code. Face-plane lengths are measured on the plane triangle
that has the face's area, so the areal scale a * b is 1 everywhere
under Snyder's projection, and its mean over a face is 1 under Fuller's.
Snyder's projection bends along the arcs from each face's centre to its corners, where its derivative jumps; there and on face edges the result is the derivative on one side. Its angular deformation is largest at the face centre, approached along those arcs: 17.27 degrees, with scale factors 1.163 and 0.860 (Snyder 1992, Table 1). At a face centre the projection has a different derivative along each direction, and the result is the limit along the azimuth the point's coordinates give.
References
Snyder, J. P. (1992). An equal-area map projection for polyhedral globes. Cartographica 29(1), 10-21. doi:10.3138/27H7-8K88-4882-1752
van Leeuwen, D. and Strebe, D. (2006). A "slice-and-dice" approach to area equivalence in polyhedral map projections. Cartography and Geographic Information Science 33(4), 269-286. doi:10.1559/152304006779500687
See also
plot with
distortion and tissot to map it