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The Newton-Raphson iteration converges more slowly near
the poles, and triggers a divide-by-zero at the poles.
Although the previous transform was handling this correctly
in the sense that it was still giving the right answer,
the divide-by-zero warning was non-optimal.
The present version switches to a Taylor-series approximation
for latitudes within 5 degrees of the poles. This avoids
the divide-by-zero, and also runs faster on arrays with a
full range of latitudes.