Addenda for
J. Geodesy 85(8), 475–485 (Aug. 2011) and
arXiv:1002.1417v3 (Feb. 2011):
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A better starting guess for Newton's method for solving for
the τ in terms of τ', Eqs. (19)–(21), is
τ0 = τ'/(1 - e2)
in Eq. (19). This reduces the number of iterations
required to from two to one for |φ| < 3.35°.
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A good way to visualize the transverse Mercator projection
over the entire global is using
tm-grid.kmz,
which is a Google Earth KML file showing the transverse
Mercator grid (in red) for the WGS84 ellipsoid with grid
spacing 1000 km in the x and y directions. The
scale, k = 0.9998035, has been adjusted so that the
distance from the equator to a pole is 10000 km.
If you
open the "tm-grid" folder in Google Earth and check on the
"spherical-transverse-mercator" subfolder, you will also see
the corresponding spherical transverse Mercator grid (in
yellow) conformally mapped to the WGS84 ellipsoid. (This
doesn't have a constant scale on the central meridian.)
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Color versions of the figures in the papers are available in
vector format in the PDF file tm-figs.pdf or in PNG format
here.
Charles Karney
<charles@karney.com>
(2013-01-07)