Const
Natural Earth 1 — pseudocylindrical, pleasing aesthetics. D3-geo parity: x = λ·k(φ²), y = φ·j(φ²) where k and j are polynomial functions of latitude. Meridians converge toward the poles correctly. Source: https://github.com/d3/d3-geo/blob/main/src/projection/naturalEarth1.js
Natural Earth 1 — pseudocylindrical, pleasing aesthetics. D3-geo parity: x = λ·k(φ²), y = φ·j(φ²) where k and j are polynomial functions of latitude. Meridians converge toward the poles correctly. Source: https://github.com/d3/d3-geo/blob/main/src/projection/naturalEarth1.js