CMB Polarization and E/B Modes
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CMB linear polarization requires two ingredients at the same event: Thomson scattering and a quadrupole in the radiation incident on the electron. The result is a spin-2 field on the sky, whose parity-even and parity-odd parts are called E and B. Scalar perturbations generate primordial E but no primordial B at linear order; tensors, vector modes, lensing, rotation, foregrounds, and instrumental leakage change that conclusion in physically distinct ways.
Required background. Probability and Inference for Gravity supplies Probability and Statistical Inference for random fields and cross-spectra.
Helpful background. The Einstein Equation supplies Einstein Equations and scalar/tensor metric sources; Relativistic Matter and Compact Objects supplies Relativistic Matter and Compact Objects radiation moments; Relativistic Cosmology supplies recombination and perturbation transfer; and The Wave Equation and Characteristics supplies Waves, Green Functions, and Geometric Optics for polarization transport.
Thomson scattering selects a quadrupole
Section titled “Thomson scattering selects a quadrupole”Choose a right-handed orthonormal basis , with the first two axes on the screen perpendicular to the outgoing direction . For incident direction and linear-polarization vectors , the Thomson kernel is
Let describe about , with azimuth measured from toward . Define and from the electric-field coherency matrix , so that means polarization along . For an optically thin electron screen with Thomson optical depth , initially unpolarized incident intensity produces the scattered contributions
The dimensionless makes have the same intensity units. The signs follow by projecting the incident unpolarized matrix onto the screen: its contribution is proportional to . For a beam incident along , the scattered electric field lies along , giving , as the formula predicts. Rotating the screen rotates both the Stokes components and their angular basis; a sign change of alone is not a harmless change to a temperature– polarization cross-spectrum.
The angular kernels are harmonics. An isotropic monopole cancels between orthogonal polarization states; a dipole also integrates to zero. Only an incident quadrupole survives. Frequent scattering suppresses precisely that quadrupole, so polarization is generated most efficiently while the plasma becomes optically thin and again when reionization exposes a large-scale quadrupole.
The scattering geometry and Stokes interpretation are explained by Hu and White 1997, §2.1, pp. 2–3, eqs. (1)–(3) (Open PDF). In a cosmological calculation the infinitesimal source is integrated through the visibility function, rather than treating the entire last-scattering region as one thin screen.
In the brightness normalization used in the previous chapter, Thomson scattering couples the intensity quadrupole to
The complete collision terms and their numerical factors are given in Ma and Bertschinger 1995, §5.5, printed pp. 21–22, eqs. (59)–(64) (Open PDF). In tight coupling the quadrupole is of order , making the small polarization fraction a controlled mean-free-path effect rather than a separate primordial amplitude.
A spin-2 field on the sphere
Section titled “A spin-2 field on the sphere”The Stokes pair depends on the screen basis. Under a right-handed basis rotation by ,
Expand these spin-weighted fields as
The basis-independent gradient-like and curl-like coefficients are defined by
They are nonlocal combinations of and : a single pixel does not possess an E or B label. Under parity,
For , statistical isotropy defines
A parity-invariant ensemble has ; that is a physical assumption, not part of the definition of B. Hu and Dodelson introduce the polarization spectra and parity distinction in Hu and Dodelson 2002, §2.3, preprint printed pp. 5–8, especially eq. (5) (Open PDF).
Why a scalar mode has no linear primordial B
Section titled “Why a scalar mode has no linear primordial B”Orient one scalar Fourier mode along . Its perturbations are axisymmetric about and contain no second transverse direction or handedness. Thomson scattering therefore creates an axisymmetric spin-2 pattern aligned with or orthogonal to the projected wavevector. That pattern is pure E. Rotating the mode and linearly superposing scalar modes does not create B, because the E/B decomposition itself is linear.
This is the precise boundary of the familiar statement:
- scalar perturbations produce no primordial linear B modes;
- tensor and vector perturbations have transverse structure and can produce both E and B at last scattering;
- gravitational lensing remaps an existing E field and converts part of it to B even when the primordial perturbations were scalar;
- polarization rotation, including a calibration-angle error or physical birefringence, mixes E and B;
- Galactic foregrounds and temperature-to-polarization leakage can imitate B unless they are included in the measurement model.
The local quadrupole argument and scalar E-only result are developed in Hu and Dodelson 2002, §3.7, preprint printed pp. 21–22 (Open PDF). The Particle Data Group gives a current observational orientation in Scott and Smoot 2026, §29.7 and §§29.7.1–29.7.3, printed pp. 10–14 (official PDF). Those dated measurements do not alter the geometric definitions above.
Physical interpretation and limits
Section titled “Physical interpretation and limits”Temperature density extrema and fluid velocity are approximately a quarter period out of phase in the acoustic limit. Because the polarization quadrupole is fed by velocity gradients, EE peaks are correspondingly out of phase with the dominant TT acoustic extrema, while TE changes sign across correlated phases. Reionization generates an additional large-angle E feature and suppresses already-formed small-scale primary power by rescattering.
Circular polarization is absent from this Thomson, linear, parity-even discussion. Partial-sky E/B separation has ambiguous modes and leakage that do not occur in the full-sky definitions. Nonlinear scattering, patchy reionization, lensing, frequency-dependent foregrounds, and instrumental systematics must not be labeled primordial merely because they contribute to .
Exercises
Section titled “Exercises”Use parity to show that and vanish for a parity-invariant ensemble, while need not vanish.
Solution
Statistical isotropy makes each two-point function diagonal in . Under parity, a or E coefficient contributes , whereas a B coefficient contributes . Hence a or correlator changes by the factor . Parity invariance requires it to equal its transformed value, so it must be zero. A correlator instead acquires and is allowed. Parity violation, cosmic or instrumental polarization rotation, or an inadequately modeled systematic can invalidate the vanishing-cross-spectrum check.
References
Section titled “References”- Hu, W., and M. White, “A CMB Polarization Primer,” New Astronomy 2, 323–344 (1997), DOI, Open PDF.
- Hu, W., and S. Dodelson, “Cosmic Microwave Background Anisotropies,” Annual Review of Astronomy and Astrophysics 40, 171–216 (2002), DOI, Open PDF.
- Ma, C.-P., and E. Bertschinger, “Cosmological Perturbation Theory in the Synchronous and Conformal Newtonian Gauges,” The Astrophysical Journal 455, 7–25 (1995), DOI, Open PDF.
- Scott, D., and G. F. Smoot, “Cosmic Microwave Background,” in F. Takahashi et al. (Particle Data Group), Review of Particle Physics, International Journal of Modern Physics A 41, 2630011 (2026), Official PDF.