For an elliptically polarized wave, the tip of its transverse vector traces an ellipse at a fixed point during each wave period. For polarization of an electromagnetic wave, this is the electric field vector. With the real components in polarization of waves, assume and . Eliminating time givesA short derivation uses and the cosine addition formula to obtain ; squaring and using the sine and cosine identity gives the displayed equation. Outside phase quadrature, the mixed term gives a tilted ellipse; are component wave amplitudes and need not be its semi-major and semi-minor axes.
In phase quadrature, , the mixed term vanishes. For , the ellipse is , its semi-major and semi-minor axes have lengths and , and its electric field magnitude varies between and . At with , the electric field is and has magnitude . Equal wave amplitudes instead give circular polarization, a special case of elliptical polarization with constant magnitude. As approaches or , the ellipse collapses to a line segment and gives linear polarization; this limit is degenerate rather than a nondegenerate ellipse.
Changing from to reverses traversal of the same ellipse. In the displayed plot, moves from toward negative as time increases. A label such as right- or left-handed circular polarization additionally requires a stated viewing direction and naming convention: viewing along propagation and viewing against propagation reverse the apparent rotation. [ref]
https://www.feynmanlectures.caltech.edu/I_33.html#Ch33-S1. Feynman Lectures, I §33–1: polarization conventions
.The ellipse records both the relative wave amplitudes and the phase difference of two transverse oscillations. This separates a change of polarization of waves from a change of overall wave amplitude: multiplying both components by the same positive factor enlarges the ellipse while preserving its shape and orientation.
A rotating ideal linear polarizer can probe this geometry. For the ellipse in phase quadrature, orthogonal projection onto a pass axis at angle gives , in . Averaging its square over a wave period gives , while the incoming squared electric field magnitude averages to . Thus the transmitted fraction of light intensity is : it is at , at and at . There is no single incident line of linear polarization to insert into Malus's law; projecting the electric field and averaging its square is the appropriate generalization. This measurement cannot distinguish from , because reversing the traversal leaves all these squared averages unchanged.
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