Classifications
pseudocylindric
Graticule
Meridians: Elliptic curves.
Parallels: Equally spaced straight parallel lines, with spacing greater than earth’s reality. Perpendicular to the central meridian.
Poles: Points.
Symmetry: About the central meridian and the equator.
Distortion
Undistorted at 40°N (or other, depending on the standard parallel) on the central meridian. Angular deformation dominates away from the equator, poles, and central meridian. Distortion is more evenly mixed elsewhere.
Parameters
One parameter, a “standard parallel”, along which scale is correct, but only in the direction of the parallel.
Similar projections
Cabot has similar parallel spacing and similar meridional curves, but its pole lines are shorter.
Origin
Oswald Winkel, 1918.