Exoplanet Detection
The Rossiter-McLaughlin Effect
As a planet transits a spinning star it hides the approaching limb, then the receding limb, distorting the stellar lines — and betraying whether its orbit is aligned, tilted, or running backward
The Rossiter-McLaughlin effect is the radial-velocity anomaly seen during a planetary transit: as the planet crosses the rotating star it covers first the approaching (blueshifted) then the receding (redshifted) limb, distorting the stellar spectral lines and revealing the sky-projected angle between the planet's orbit and the star's spin axis.
- DiscoveredRossiter & McLaughlin, 1924
- First exoplanet detectionHD 209458 b, 2005
- Measuresprojected obliquity λ
- Typical amplitude10–100 m/s
- ScalingΔV ∝ (R_p/R★)² v sin i★
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A condensed visual walkthrough — narrated, captioned, under a minute.
The intuition: hiding half a spinning star
Point a spectrograph at a star and you do not resolve its disk — you collect the summed light of millions of surface patches into a single spectrum. The star rotates, so one half of its visible disk is sweeping toward you and the other half is sweeping away. By the Doppler effect, the light from the approaching limb is shifted slightly blue and the light from the receding limb slightly red. Each narrow absorption line therefore gets smeared out into a broad, roughly symmetric trough whose width encodes the projected rotation speed, v sin i★. This is ordinary rotational broadening, and it is symmetric: the blue and red contributions balance, so the line centroid sits at the star's true velocity.
Now slide an opaque planet across the disk. When the planet sits on the blueshifted (approaching) limb, it is blocking blue-shifted starlight. That light is missing from the summed profile, so the surviving light is, on average, slightly redder — and the spectrograph reports the star as receding a touch faster than it really is. A few hours later the planet has crossed to the redshifted (receding) limb; now it hides red-shifted light, the surviving profile skews blue, and the apparent velocity flips to a blueshift. The star itself never changed its motion. What you are watching is the spectroscopic shadow of a planet selectively covering a rotating surface. That sign-flipping wobble, superimposed on the transit, is the Rossiter-McLaughlin effect.
The punchline is geometric. The exact timing and shape of the anomaly — which limb is covered first, how symmetric the blue-to-red swing is, where the zero-crossing falls relative to mid-transit — encode the angle between the planet's transit chord and the star's rotation axis. That angle is the system's spin-orbit alignment, and the Rossiter-McLaughlin effect is the single most productive way we have of measuring it.
The mechanism and the governing equation
Treat the stellar disk as a brightness map I(x, y) with a line-of-sight velocity field set by rotation. For solid-body rotation seen with the spin axis projected along the sky's y-direction, the line-of-sight velocity of a surface element at projected position x (in units of the stellar radius R★) is
v_los(x) = x · v sin i★
where v sin i★ is the equatorial rotation velocity projected onto the line of sight. A planet of radius R_p covering a small patch at position (x_p, y_p) removes a flux fraction roughly δ = (R_p/R★)² (modulated by limb darkening) that was carrying velocity v_los(x_p). The flux-weighted velocity centroid of the whole star then shifts by approximately
ΔV_RM(t) ≈ − δ(t) · x_p(t) · v sin i★ · f(limb darkening)
The minus sign is the heart of the effect: removing blue light (x_p < 0) raises the apparent velocity, removing red light (x_p > 0) lowers it. The track x_p(t) of the planet across the disk is a straight chord whose orientation is the projected obliquity λ. For an aligned orbit (λ = 0°) the chord runs perpendicular to the spin axis, x_p sweeps cleanly from −1 to +1, and ΔV_RM traces a clean antisymmetric blue-then-red curve. For a polar orbit (λ = 90°) the chord runs parallel to the spin axis at fixed x_p, so the anomaly has a single sign throughout the transit. The full velocity-anomaly curve is thus a direct readout of the transit geometry.
A subtlety that the simple formula above hides: a partially occulted rotating line profile is not merely shifted, it is deformed — the planet carves a localized bright "bump" out of the dark absorption trough at the velocity of the patch it covers. The classical centroid formula (the Ohta-Taruya-Suto 2005 and Hirano et al. 2011 analytic models) captures the leading behaviour, but precise modern work fits the full line-shape distortion, which is what Doppler tomography and the "reloaded" technique exploit.
The key numbers
The amplitude of the anomaly follows directly from the transit depth and the rotation speed. To order of magnitude,
ΔV_peak ≈ (R_p / R★)² × v sin i★ × C
where C ≈ 0.6–0.8 folds in limb darkening and the geometry of partial coverage. The relevant numbers across real systems:
- Projected rotation speed v sin i★. Sun-like dwarfs rotate at the equator at ~2 km/s (the Sun: 1.6–2.0 km/s); young or hot stars reach 10–150 km/s. The anomaly amplitude is directly proportional to this.
- Transit depth (R_p/R★)². A hot Jupiter (R_p ≈ 1 R_Jup) around a Sun-like star (R★ ≈ 1 R☉, with R_Jup/R☉ ≈ 0.10) gives R_p/R★ ≈ 0.10, depth ≈ 1%. An Earth-size planet gives depth ≈ 0.008% — too small for an RM detection with current instruments.
- Resulting anomaly. 10–100 m/s for typical hot Jupiters; well over 1 km/s for giants around fast-rotating A/F stars. Compare with the orbital reflex (Keplerian) RV signal of a hot Jupiter, ~50–200 m/s, on top of which the RM bump rides during the few-hour transit.
- Instrument precision. HARPS (ESO 3.6 m, La Silla) and ESPRESSO (VLT) reach ~1 m/s and sub-m/s respectively; HIRES (Keck) and SOPHIE (OHP) are at the few-m/s level. This is why even modest anomalies are routinely measurable.
- Timescale. The whole signature plays out over the transit duration — typically 2–4 hours for a hot Jupiter on a ~3-day orbit — which is why a single transit night can deliver an obliquity.
How it is observed and modelled
An RM campaign collects a dense time series of high-resolution spectra spanning a full transit plus baseline before and after. Each spectrum is reduced to a radial velocity (classically) or to a cross-correlation function / line profile (for the modern techniques). The observed RV time series is the sum of three things: the constant systemic velocity, the slowly varying Keplerian orbital reflex motion, and — only during the transit window — the RM anomaly. Subtract a fitted Keplerian and the RM bump stands out.
The data are then fit with a model parameterised by λ and v sin i★ (plus the well-known transit geometry from photometry: R_p/R★, impact parameter b, inclination). Three main methods coexist:
| Method | What it fits | Best for | Key reference |
|---|---|---|---|
| Classical RM (velocity anomaly) | RV centroid vs. time | Slow rotators, legacy data | Ohta+ 2005; Hirano+ 2011 |
| Doppler tomography | Planet "bump" tracking across the line profile | Fast rotators (broad lines) | Collier Cameron+ 2010 |
| Reloaded / Revolutions RM | Local stellar surface spectrum behind the planet | Differential rotation, convection, μ-dependence | Cégla+ 2016; Bourrier+ 2021 |
The output is λ, the sky-projected angle. To turn that into the true three-dimensional obliquity ψ you also need the stellar inclination i★. Combining v sin i★ with an independent rotation period (from photometric spot modulation or asteroseismology) and the stellar radius gives i★, and then cos ψ = cos i★ cos i_orb + sin i★ sin i_orb cos λ.
Worked example: HD 209458 b
Take the first transiting exoplanet found, HD 209458 b, a 0.69 M_Jup hot Jupiter on a 3.52-day orbit around a G0 V star with R★ = 1.16 R☉ and v sin i★ ≈ 4.5 km/s. The transit depth is about 1.5%, so R_p/R★ ≈ 0.12.
Estimate the peak anomaly:
ΔV_peak ≈ (R_p/R★)² × v sin i★ × C
≈ (0.12)² × 4500 m/s × 0.7
≈ 0.0144 × 4500 × 0.7
≈ 45 m/s
The measured semi-amplitude of the anomaly is indeed a few tens of m/s. Winn et al. (2005), using Keck/HIRES, fit the antisymmetric blue-then-red shape and found λ = −4.4° ± 1.4° — the orbit lies essentially in the stellar equatorial plane, prograde and aligned. This was the template case: a textbook well-behaved system that confirmed planets can form and migrate while keeping the disk's original alignment.
Contrast that with HAT-P-7 b. Here the anomaly does not flip from blue to red — it stays one-signed and then reverses the expected order, the spectroscopic fingerprint of a planet that crosses the receding limb first. Narita et al. and Winn et al. (2009) independently derived λ ≈ 180° (within errors): the planet orbits retrograde, against the star's spin. No quiet disk migration can produce that; it demands a violent dynamical history.
Discovery and the rise of obliquity science
The effect was seen first not in planets but in eclipsing binary stars. In 1924 Richard A. Rossiter, in his University of Michigan doctoral thesis, reported the anomalous velocity excursions during the eclipses of Beta Lyrae; in the same year and at the same institution Dean B. McLaughlin reported them for Algol (β Persei). The physical interpretation — selective occultation of a rotating disk — was understood almost immediately, and the signature became a tool for studying stellar rotation in eclipsing binaries for decades.
Its exoplanet career began in 2000, when Queloz and collaborators reported a first tentative measurement for HD 209458 b and noted the technique could probe spin-orbit alignment; Gaudi and Winn (2007) later spelled out clearly how the anomaly's shape constrains λ. It began in earnest in 2005 with the precise HD 209458 b measurement. The field then exploded. The discovery of clearly misaligned (XO-3 b, 2008) and retrograde (HAT-P-7 b and WASP-17 b, 2009) hot Jupiters overturned the comfortable assumption of universal alignment. By around 2010–2012 Amaury Triaud, Simon Albrecht, and collaborators had assembled enough measurements to reveal a startling pattern: misalignment correlates with host-star temperature. Planets around hot stars (T_eff > ~6250 K, the Kraft break) are frequently misaligned; planets around cool stars are usually aligned. Today the catalog runs to hundreds of measured obliquities, gathered by HARPS, ESPRESSO, HIRES, SOPHIE, and SUBARU/HDS, and the technique is being pushed down toward smaller planets and even to mapping the stellar surface itself.
Variants and related phenomena
- Doppler tomography. Rather than collapsing each spectrum to one velocity, this tracks the dark planetary "bump" as it migrates across the broad, rotationally smeared line profile. Because broad lines (fast rotators) carry more spatial information, tomography is the method of choice for hot, rapidly rotating A/F stars — exactly the regime where the classical centroid method struggles.
- The "reloaded" Rossiter-McLaughlin (RMreloaded) and RM Revolutions. Developed by Cégla, Bourrier, and colleagues, these isolate the spectrum of the precise surface element behind the planet at each moment, directly recovering the local rotation velocity. They can detect differential rotation (equator faster than poles), center-to-limb convective shifts, and resolve degeneracies between λ and v sin i★.
- Gravity darkening. A rapidly rotating star is oblate and has hotter, brighter poles (von Zeipel effect). The asymmetric brightness map distorts the transit light curve itself, providing an independent — and out-of-the-plane — handle on obliquity, as exploited for KOI-13 b by Barnes and others.
- Spot crossings and starspot tracking. Repeated transits over a spotted star can show the planet occulting the same spots, mapping the latitude band the chord crosses and constraining alignment photometrically (used extensively for Kepler systems).
- Stellar obliquities of binaries. The original 1924 application — measuring the mutual alignment of stellar spins and orbits in eclipsing binaries — remains active and informs theories of binary formation.
Common misconceptions and subtleties
- "It measures the true obliquity." No — it measures only the sky-projected angle λ. A system with λ ≈ 0° could still be substantially misaligned in 3-D if the star's pole points toward or away from us. The true obliquity ψ needs the stellar inclination as well.
- "The star's velocity actually changes during transit." It does not. The bulk radial velocity of the star is unchanged; the apparent shift is an artifact of removing part of a rotating, spatially unresolved surface from the line profile.
- "The line is just Doppler-shifted, so a centroid fit is exact." A partly occulted line is deformed, not cleanly shifted, so the classical centroid model is biased. The bias is small for slow rotators but grows for fast ones, which is why line-profile (tomographic) modelling is preferred there.
- "Retrograde means the planet physically reversed its motion." Retrograde here is relative to the star's spin: the orbit runs counter to the stellar rotation. The planet's own orbital motion is perfectly ordinary; it is the spin-orbit relationship that is backward, pointing to scattering or Kozai-Lidov migration rather than smooth disk migration.
- "Any transiting planet can be measured." The anomaly scales as (R_p/R★)² v sin i★. Small planets, or planets around very slow rotators, can push the signal below the m/s noise floor — so RM obliquities are still dominated by giant planets, though ESPRESSO is steadily reaching smaller worlds.
- "Limb darkening can be ignored." Limb darkening reshapes both the brightness map and the effective velocity weighting; ignoring it skews the inferred λ and v sin i★. It is a standard nuisance parameter in every modern fit.
Frequently asked questions
What exactly does the Rossiter-McLaughlin effect measure?
It measures the sky-projected spin-orbit angle, λ — the angle on the plane of the sky between the star's rotation axis and the normal to the planet's orbit. A symmetric, sign-flipping anomaly (redshift then blueshift) means the orbit is aligned with the stellar equator (λ ≈ 0°). An anomaly that stays a single sign throughout, or that is strongly lopsided, means the orbit is misaligned. An entirely reversed signature (blueshift first) means the planet crosses the receding limb first — a retrograde or polar orbit. Note λ is only the projected angle; the true 3-D obliquity ψ also requires the stellar inclination i_star, usually obtained from v sin i_star together with the rotation period and stellar radius.
Why does blocking part of the star look like a velocity shift?
A star is spatially unresolved, so its spectrum is the sum of light from every surface element. Rotation Doppler-shifts the approaching limb's light to the blue and the receding limb's to the red, broadening each absorption line into a roughly bell-shaped, rotationally broadened profile. When the planet covers a patch on the blueshifted limb, it subtracts blue-shifted starlight, so the line's flux-weighted centroid moves to the red — the spectrograph reports a positive (receding) radial-velocity anomaly even though the star has not changed its bulk motion. The effect is purely a consequence of selectively hiding part of a rotating surface.
How large is the velocity anomaly in practice?
The peak amplitude scales roughly as the transit depth times the projected rotation speed: ΔV ≈ (R_p/R_star)² × v sin i_star × (factor of order 0.6–0.8 from limb darkening and partial coverage). For a hot Jupiter with R_p/R_star ≈ 0.12 transiting a slow rotator with v sin i_star = 4 km/s, that is about 0.12² × 4000 m/s ≈ 58 m/s peak-to-peak — easily resolved by HARPS-class spectrographs that reach ~1 m/s precision. Around a fast-rotating A or F star with v sin i_star up to 100 km/s, the anomaly can exceed 1 km/s.
Why are so many hot Jupiters misaligned or retrograde?
Planets form in a disk that should share the star's spin, so a primordial alignment is expected. The fact that a large fraction of hot Jupiters — and almost all of those around hot (>6250 K) stars — are misaligned points to violent migration: planet-planet scattering or Kozai-Lidov cycles driven by a distant companion can pump up the orbital inclination, after which tidal friction shrinks the orbit into a hot Jupiter on a tilted or even backward path. Cooler stars with thick convective envelopes can tidally re-align the orbit, which is why misalignment correlates with stellar effective temperature — a pattern first highlighted by Amaury Triaud and by Simon Albrecht and colleagues around 2010–2012.
Who discovered the effect and when was it first seen for an exoplanet?
The spectroscopic distortion during an eclipse was reported independently in 1924 by Richard A. Rossiter (in his PhD thesis on the eclipsing binary Beta Lyrae) and by Dean B. McLaughlin (in the prototype eclipsing binary Algol). It lay largely dormant for exoplanets until Joshua Winn and collaborators measured it for the first transiting exoplanet, HD 209458 b, in 2005, finding a well-aligned orbit (λ ≈ −4.4°). The first clearly retrograde planet, HAT-P-7 b, was announced in 2009 by both Norio Narita's team and Joshua Winn's team.
Can the effect be measured without spectroscopy of the whole line?
Yes. The classical method fits the velocity anomaly extracted from the cross-correlation function, but it is biased because a partly occulted line is not simply shifted — it is deformed. Modern analyses instead model the full distortion: 'Doppler tomography' tracks the dark 'bump' the planet carves across the rotationally broadened line profile (powerful for fast rotators), while the 'reloaded RM' technique of Vincent Bourrier and colleagues isolates the spectrum of the exact stellar surface region behind the planet, recovering the local rotation velocity directly and even mapping differential rotation and convective effects.