Exoplanets

One eccentric planet, or two circular ones

The velocity curve of a star with one planet on an eccentric orbit is, to first order in the eccentricity, exactly the curve of two planets on circular orbits with periods in the ratio two to one. The difference between the two readings is a term in the eccentricity squared, and for the modest eccentricities most planets have, it is smaller than the noise.

Assumes Reflex velocity, The ellipse and Periodograms.

A star with a planet moves in a small orbit of its own, and its velocity towards and away from the observer rises and falls once per orbit. For a circular orbit the curve is a sine wave, and its amplitude and period give the planet’s minimum mass and its distance. For an eccentric orbit the curve is skewed: the star moves fast near periastron and slowly near apastron, as the second law requires, so one half of the cycle is compressed and the other stretched. The skew is how an observer measures the shape of an orbit nobody can see.

It is also exactly what a second planet would do. A skewed periodic curve is a sine wave plus harmonics — components at twice the frequency, three times, and so on — and the largest of them, at twice the frequency, is indistinguishable from the signal of another planet orbiting at half the period on a circular orbit. For the eccentricities most planets have, one reading of the data is a single planet on a moderately eccentric orbit, and the other is two planets on circular orbits with periods in the ratio two to one. The two are the same measurement.

One eccentric planet, drawn as two circular ones. Top: the velocity of a star with one companion on an orbit of eccentricity 0.25 (argument of periastron 0.9 radians), in units of its semi-amplitude K, over two orbits — and on top of it the sum of two circular orbits, one at the same period and one at half of it, fitted by taking the first two terms of the exact curve's Fourier series. The second orbit's amplitude comes out at 0.246 of the first, which is the eccentricity to first order. Bottom: the difference between the two, on a scale 12 times magnified; its largest excursion is 0.0889 K and its rms 0.0473 K, second order in the eccentricity. For a planet with K = 30 m/s that is 1.42 m/s rms — below the noise of most instruments — so an eccentric single planet and a pair of planets in a 2:1 period ratio are the same measurement unless the data are good enough to see a term of order e².
Fig. 1 A single planet on an orbit of eccentricity 0.25, in thick red, and the sum of two circular orbits at the same period and at half of it, in dashed blue, whose amplitudes and phases are taken from the first two terms of the red curve’s Fourier series. The second orbit’s amplitude comes out at 0.246 of the first — the eccentricity, to first order. The lower panel is their difference, magnified twelvefold: its largest excursion is nine per cent of the semi-amplitude and its rms under five per cent.

The expansion that makes them the same

The reason is a line of algebra. The star’s velocity along the line of sight is

v=K[cos(ν+ω)+ecosω],v = K\left[\cos(\nu + \omega) + e\cos\omega\right],

where ν is the true anomaly — the angle of the planet from periastron — ω is the orientation of the orbit, and K the semi-amplitude. The true anomaly does not advance uniformly in time; it runs ahead near periastron. Expanded in the mean anomaly M, which does advance uniformly, it is

ν=M+2esinM+O(e2).\nu = M + 2e\sin M + O(e^2).

Put that into the velocity, expand the cosine, and keep terms to first order in e. The constant term cancels against the ecosωe\cos\omega, and what is left is

vK[cos(M+ω)+ecos(2M+ω)].v \approx K\left[\cos(M+\omega) + e\cos(2M+\omega)\right].

That is a sinusoid at the orbital frequency with amplitude K plus a sinusoid at twice the frequency with amplitude eK. And a circular orbit at half the period has a velocity curve that is exactly a sinusoid at twice the frequency, with any amplitude and any phase. So an eccentric orbit of eccentricity e, to first order, is a circular orbit plus a second circular orbit at half the period with an amplitude e times as large.

There is no phase constraint that saves the distinction. The second harmonic’s phase is locked to the fundamental’s through ω, but ω is a free parameter of the orbit. Any relative phase the two-planet model wants can be supplied by choosing ω; any ω the eccentric model has can be imitated by choosing the phase of the inner planet. The mapping between the two models is exact at first order, and it runs in both directions.

A difference that is second order

The two models part company at the next order in e. The true velocity curve contains a third harmonic of amplitude about e2Ke^2 K, a fourth of amplitude about e3Ke^3 K, and so on; the two-planet model has none of these. The difference between the two curves is therefore of order e2Ke^2 K, and how visible it is depends on how that compares with the noise.

The residual that separates one planet from two. The rms difference between an eccentric Keplerian velocity curve and the best imitation by two circular orbits at periods P and P/2, in units of the semi-amplitude K, against eccentricity (argument of periastron 0.9 radians). It grows as the square of the eccentricity — slope 2.00 measured off the drawn points — because the imitation is exact to first order. The horizontal lines are measurement noise as a fraction of K: 0.1 (for example 3.0 m/s on a 30 m/s planet), crossed at e ≈ 0.40; 0.03 (for example 0.9 m/s on a 30 m/s planet), crossed at e ≈ 0.20; 0.01 (for example 0.3 m/s on a 30 m/s planet), crossed at e ≈ 0.13. Below the crossing, a single set of velocities cannot distinguish the two; many sets can, because noise averages down as the square root of the number of points and the residual does not, but the eccentricities of published planets pile up exactly in the range where the distinction needs that averaging.
Fig. 2 The rms difference between an eccentric orbit and its best two-planet imitation, in units of the semi-amplitude, against eccentricity. It grows as the square of the eccentricity, measured from the drawn points at a slope of 2.00. The horizontal lines are noise levels as fractions of K. A single season’s velocities with noise a tenth of the semi-amplitude cannot tell the two models apart below an eccentricity of about 0.4; at a thirtieth, below 0.2; at a hundredth, below about 0.13.

For a planet with a semi-amplitude of 30 metres a second observed with an instrument delivering one metre a second, the noise is about three per cent of K, and eccentricities below about 0.2 are ambiguous from any single set of data of modest size. That covers most of the eccentricities in the known population. The distinction can still be made with enough data — noise averages down as the square root of the number of observations and the residual does not — but the amount of data required rises steeply as the eccentricity falls, and a published orbit fitted from a few dozen velocities has usually not reached it.

This is not the same effect as the preference every detection method has for circular orbits, though it is related to it. That effect is about which planets are found: a periodogram built from sine waves loses the power in an eccentric orbit’s harmonics, so an eccentric planet is slightly harder to detect than a circular one of the same mass. The degeneracy here is about what is concluded once a planet has been found: the power that went into the harmonics is still in the data, and it can be attributed to the planet’s orbit or to another planet.

The planet an eccentricity can hide

Read in one direction, the degeneracy says an eccentric orbit might really be two planets. Read in the other, it says a real second planet might be absorbed into the first planet’s orbit and never reported.

The planet an eccentricity can hide. The minimum mass of the inner planet that a two-planet fit assigns, as a fraction of the outer one's, when the data are really one eccentric orbit — against that orbit's eccentricity. A velocity semi-amplitude scales as mass times period to the minus one third, so a companion at half the period with a second-harmonic amplitude eK has a mass of e/2^⅓ ≈ 0.79e of the first. At e = 0.1: 0.079; At e = 0.2: 0.157; At e = 0.3: 0.233. Read the other way, a genuine inner planet of a fifth of the outer one's mass, on a 2:1 orbit, can be absorbed into a single orbit with an eccentricity of about a quarter — and it disappears from the catalogue while making its companion look more eccentric than it is. The dashed line is the first-order relation; the curve is the exact Fourier ratio.
Fig. 3 The minimum mass of the inner planet a two-planet fit assigns, as a fraction of the outer planet’s, when the data are really a single eccentric orbit. A velocity amplitude scales as the mass times the period to the minus one third, so a companion at half the period with an amplitude eK has a mass of 0.79e of the first: 0.08 at an eccentricity of 0.1, 0.16 at 0.2, 0.23 at 0.3. The dashed line is the first-order relation.

So a real inner planet of a fifth of the outer planet’s mass, on a 2:1 orbit, produces the same velocities as a single planet with an eccentricity of about a quarter. Fitted as a single planet, the inner one disappears from the catalogue, and the outer one is recorded as more eccentric than it is. Both errors propagate. The catalogue’s count of planets in 2:1 resonance is too low, and its distribution of eccentricities is too high, by amounts that depend on how many such pairs there are — which is the quantity that cannot be measured without resolving the degeneracy.

That matters because the two readings imply different histories. A pair of planets in a 2:1 resonance is the characteristic product of convergent migration in a gas disc: two planets drifting inward at different rates meet at a resonance and are captured into it, and chains of such captures are the strongest evidence that planets migrate. A single eccentric planet is the characteristic product of the opposite kind of history: a violent one, in which planets scattered each other or a distant companion pumped the eccentricity. The same velocity curve supports a quiet history or a violent one, and the demographics of planetary systems depend on which is chosen.

There is one constraint the two-planet reading has to satisfy that the single-planet reading does not, and occasionally it decides the matter. Two planets at a period ratio of two sit at orbital radii in the ratio 22/31.592^{2/3} \approx 1.59, and a pair that close is stable only if the planets are not too massive and their orbits not too eccentric. For a pair of small planets around a Sun-like star this is no restriction at all. For the fits that come out with an inner planet of a Jupiter mass or more, and with eccentricities of their own, it can be: a numerical integration of the fitted system over a few million orbits sometimes shows it tearing itself apart in a few thousand, and a solution that could not have survived to be observed is excluded whatever its likelihood. The opposite does not follow — stability says a pair could exist, not that it does — and a resonance can protect a pair that would otherwise be unstable, which is exactly the configuration convergent migration produces.

How the second planet gets manufactured

The degeneracy would be only a curiosity if the analysis always fitted both models and compared them. In practice the analysis is often sequential, and the sequence decides the answer.

A second planet at half the period, found in one planet's residuals. The Lomb–Scargle periodogram of 60 velocities of a star with one companion on a 40-day orbit of eccentricity 0.3, observed at random times over 600 days with noise of 0.15 K, after the strongest signal — found at 39.9 days — has been removed as a circular orbit. What is left has its highest peak at 19.9 days, half the period, standing well clear of everything else. It is not an alias of the sampling; it is the orbit's own second harmonic, which a search built from sinusoids can only represent as a separate signal. The power is drawn on the scale of the original periodogram, where the first peak reached 26. An analysis that subtracts a circular orbit and searches the residuals finds a second planet here; one that fits an eccentric orbit first finds nothing. The peak does not say which is true.
Fig. 4 Sixty velocities of a star with one planet on a 40-day orbit of eccentricity 0.3, with noise of fifteen per cent of the semi-amplitude. The strongest periodic signal is found at 40 days and removed as a circular orbit; the periodogram of what is left is drawn here, and its highest peak is at 20 days, standing well clear of the rest. A search that proceeds by removing the strongest sinusoid and looking again finds a second planet at half the period. A search that fits an eccentric orbit first finds nothing there.

The standard procedure for finding multiple planets in velocity data is exactly the one in the figure: compute a periodogram, fit the strongest signal, subtract it, and compute the periodogram of the residuals. If the first fit is a circular orbit, the residuals contain the second harmonic, and the second harmonic looks like a planet. If the first fit is a Keplerian with free eccentricity, the second harmonic is absorbed and the residuals are clean.

Neither choice is neutral. A circular first fit manufactures an inner planet whenever the real orbit is eccentric; an eccentric first fit absorbs an inner planet whenever the real system is a 2:1 pair. The residual periodogram does not say which happened. A peak in a periodogram is a statement about the model subtracted before it was computed, and a peak at exactly half the period of a known planet is the least informative peak there is.

That is not a hypothetical concern. Re-analyses of published single-planet systems have found that a substantial fraction of the moderately eccentric ones are fitted as well, or better, by a pair of planets near a 2:1 period ratio, and several systems first reported as a single eccentric planet have later been reported as two. The reverse has also happened: signals at half a known planet’s period have been withdrawn when the first planet’s orbit was refitted with a small eccentricity.

When the data cannot decide, the prior does

Faced with two models that fit equally well, a careful analysis compares them formally, and the comparison is less objective than it sounds.

A single eccentric orbit has five parameters: period, semi-amplitude, eccentricity, orientation and a reference time. Two circular orbits have six: a period, amplitude and phase each. The eccentric model is therefore the simpler of the two, and any criterion that penalises extra parameters prefers it when the fits are equally good. But the fits are not equally good in general; the two-planet model can always absorb some noise the eccentric one cannot, and the penalty for one extra parameter is small. The outcome of the comparison depends on how the penalty is set.

In a Bayesian comparison the penalty is replaced by priors, and the priors are where the answer hides. A prior on eccentricity that favours small values — as the observed distribution does, with most planets below 0.3 — pushes the eccentric model towards zero and makes the two-planet reading more attractive. A prior on multiplicity that says 2:1 pairs are rare pushes the other way. Both priors are taken from the catalogue, and the catalogue is built from fits that faced this very choice. The circle closes: the eccentricity distribution is inferred from orbits whose eccentricities were partly decided by an assumed eccentricity distribution.

None of that makes the analysis wrong. It makes the eccentricity of an individual planet, below about 0.2 and without a transit or a long baseline, a quantity whose value depends on what else is believed about planetary systems. That is a different kind of uncertainty from a measurement error, and it does not shrink with better calibration.

Why noise alone makes orbits look eccentric

There is an older version of the same problem, and it pushes in the same direction. An eccentricity is a positive quantity: it is the length of a vector whose two components are ecosωe\cos\omega and esinωe\sin\omega. If the true orbit is circular, both components are zero, but a fit to noisy data returns small non-zero values for each, and the length of the resulting vector is always positive. Noise therefore never makes a circular orbit look circular. It makes it look slightly eccentric, with an eccentricity of order the noise divided by the semi-amplitude.

For spectroscopic binary stars the effect was recognised in 1971, and the standard response is a significance test: an eccentricity is quoted only if it is significantly larger than the value noise alone would produce for a circular orbit, and set to zero otherwise. The same bias afflicts planets, and it compounds with the degeneracy rather than cancelling it. A circular planet with a real inner companion at half its period is fitted, as a single planet, with an eccentricity inflated both by the companion’s harmonic and by the noise — two effects of the same sign, neither of which can be seen in the fit.

The combined result is that the lower end of the eccentricity distribution is the least secure part of it, and it is precisely the part that distinguishes a system that migrated quietly from one that did not.

The harmonic that only an ellipse makes

The way out is the third harmonic, and it is worth being precise about what it can decide.

The third harmonic that two circular planets cannot make. The amplitudes of the first 5 harmonics of an eccentric orbit's velocity curve, relative to the semi-amplitude, for eccentricities 0.1 and 0.3, on a logarithmic scale. At e = 0.1: 0.9903, 0.0988, 0.0111, 0.0013, 0.0002. At e = 0.3: 0.9135, 0.2676, 0.0882, 0.0307, 0.0110. Each harmonic is roughly the eccentricity times the one before it. Two circular planets at P and P/2 produce the first two bars and nothing else; the third harmonic and beyond are the eccentric orbit's own signature, and they are what a fit has to detect to decide between the two. At e = 0.1 the third harmonic is 1.11% of K — for a 30 m/s planet, 0.33 m/s. Two real planets in a 2:1 resonance also perturb each other and produce extra harmonics of their own, so even a detected third harmonic has to be modelled rather than simply counted.
Fig. 5 The amplitudes of the first five harmonics of an eccentric orbit’s velocity curve, relative to the semi-amplitude, at eccentricities of 0.1 and 0.3. Each is roughly the eccentricity times the one before. Two circular planets at P and P/2 produce the first two bars and nothing beyond; the third harmonic and higher belong to the eccentric orbit alone. At an eccentricity of 0.1 the third harmonic is 1.1 per cent of the semi-amplitude — a third of a metre a second on a 30-metre-a-second planet.

An eccentric orbit predicts a third harmonic with a definite amplitude — about 98e2K\tfrac{9}{8}e^2K — and a definite phase relative to the first two. The two-circular-planet model predicts none. Detecting a third harmonic of the right size and phase is therefore evidence for eccentricity, and failing to detect one where the eccentric model says it should be large enough is evidence against it. The required precision is set by e2Ke^2 K, which at an eccentricity of 0.1 is a hundredth of the semi-amplitude.

Two complications prevent this from being a clean test. First, two real planets in or near a 2:1 resonance perturb each other, and the perturbation produces signals of its own at combinations of the two frequencies, including the third harmonic of the outer one. A resonant pair does not look like the sum of two independent circular orbits once the data span long enough for the interaction to matter. Second, the two planets need not be on circular orbits either: a pair can have small eccentricities of its own, with harmonics of its own. The comparison is therefore not between one eccentric orbit and two circular ones, but between one eccentric orbit and two interacting, slightly eccentric ones — a model with more parameters, which can always fit a little better.

What the long baseline buys is exactly the interaction. A single eccentric orbit is strictly periodic. A resonant pair is not: its orbits precess and exchange energy on a timescale of years to decades, and its velocity curve changes shape slowly. A data set spanning several of those cycles can tell the two apart by the drift, whatever the third harmonic does — which is why the ambiguous systems are resolved by time rather than by precision.

Transits break it, when they exist

For a planet that also transits, the degeneracy has an independent resolution, because a transit time is a direct statement about where the planet is.

A planet on an eccentric orbit transits at a phase that depends on ω, and its transit duration differs from that of a circular orbit by a factor depending on e and ω together. An inner planet at half the period would transit too, if its orbit were aligned closely enough with the outer one’s, and it would be seen. And a resonant pair of transiting planets shifts each other’s transit times by minutes to hours, in a pattern that has no counterpart for a single planet. Any one of those three is enough to decide.

Most planets found by velocities do not transit, and for those the degeneracy is resolved only by more velocities. That is why the eccentricity distribution of velocity-detected planets — the distribution every theory of planetary dynamics is ultimately tested against — carries an uncertainty that is not in any individual orbit’s error bar.

What the picture assumes

The figures draw the velocities as coming only from the planet. A real star adds its own signals: rotation, spots and convection, many of them periodic, and the rotation signal of a spotted star is itself strongly non-sinusoidal, with harmonics of its own. A star rotating in forty days with a spot pattern that persists for several rotations produces power at forty days and at twenty, just like the eccentric planet in the figures. A signal at half a known period may be the orbit’s harmonic, a second planet, or the star’s rotation harmonic, and the three have to be separated by other means — activity indicators, line shapes and the persistence of the phase.

The figures also assume full phase coverage when they compute the imitation. With gaps, the best two-planet fit is not simply the first two Fourier terms, and the sampling’s own periodicities can make the degeneracy worse — a gap pattern with power at the orbital period mixes the harmonics with each other.

Still open: how many 2:1 pairs are catalogued as eccentric planets

The fraction is not known, and it is a fraction that matters. If a substantial part of the moderately eccentric planets found by velocities are really unresolved 2:1 pairs, then resonant pairs are more common than the catalogues say and the eccentricity distribution is less extreme than it looks — which would move the balance between the quiet, migration-driven histories and the violent, scattering-driven ones. The test is data: long, dense velocity series on the ambiguous systems, analysed with both models fitted from the start rather than in sequence. Those series also run into the floor that the star’s own surface sets on every velocity measurement, which at the precision a third harmonic needs is no longer the instrument’s to set.

About the same objects

Not linked from either essay — found by the objects both name.

What links here

Essays that link to this one from their own argument.

The objects this essay names

Each one links to every other essay that touches it.

DegeneracyEccentricityFourier seriesHarmonicMinimum massPeriodogramRadial velocityReflex motionResonanceSemi-amplitude