The calm that is the ghost of a cycle
Assumes: The map a dripping tap turns out to be · The error that doubles on a schedule
The map a dripping tap turns out to be followed one route into chaos to its end: a strongly damped system, sampled once per cycle, doubles its period again and again until the doublings pile up and the motion becomes irregular. It ended by naming a second route, and the second route looks nothing like the first. There is no cascade. The system is periodic, and then — past a threshold, with nothing gradual about it — it is periodic most of the time, interrupted by bursts of disorder that arrive at no predictable moment and leave as suddenly as they came.
Yves Pomeau and Paul Manneville described this in 1980 and called it intermittency. The same year, measurements in a convection cell showed exactly the pattern they predicted: long stretches of regular oscillation separated by brief, irregular bursts, with the stretches lengthening as a control parameter approached a threshold. The explanation turns out to be one of the most portable arguments in dynamics, because the calm stretches are not a property of chaos at all. They are the ghost of a stable cycle that is about to exist.
Calm, then a burst, then calm
The logistic map, , is chaotic over most of the range of beyond its period-doubling cascade. At exactly a stable three-cycle appears out of that chaos: above that setting, every orbit settles onto three values visited in turn. Just below it, the orbit is doing something neither chaotic nor periodic.
Two hundred-thousandths below the setting where the cycle is born, the orbit spends long stretches cycling through three values, repeating itself to three decimal places every third step. Then it leaves, wanders through every value between nought and one with no discernible pattern — stretched and folded exactly as the fold that has to be there requires, and as chaotic as anywhere in the map’s range — and is captured into another calm, which lasts about as long as the last one and ends as abruptly.
The map contains no randomness. The same starting value produces the same calms and the same bursts every time the sequence is computed. The irregular timing of the bursts is the deterministic chaos of the burst phase, an error that doubles on a schedule during each excursion, deciding where the orbit re-enters the region of calm and so how long the next calm will last.
A cycle that has not been born
The calms are explained by looking at the map three steps at a time. A three-cycle is a point that the third iterate returns to itself, so it lies where the graph of crosses the diagonal. A stable three-cycle is born at in the simplest way a pair of fixed points can be born: the graph of , rising as rises, touches the diagonal at three places and then pushes through, creating at each place a stable crossing and an unstable one. That is a saddle-node bifurcation, sometimes called a tangent bifurcation, and it is the commonest way anything in dynamics comes into existence.
Just below the bifurcation the graph has not quite reached the diagonal. It passes above it at each of the three places, leaving a narrow channel between the curve and the line. An orbit iterated by moves, on each step, by the vertical distance between the curve and the diagonal — and in the channel that distance is tiny. So an orbit arriving at the channel creeps through it in a long series of small steps, each third iterate almost exactly equal to the one before. Seen one iterate at a time, that creep is a nearly perfect three-cycle.
The calm is the ghost of the cycle that will exist at the bifurcation. The fixed point of is not there yet; the place where it will be is there, and an orbit passing through that place behaves as though the fixed point were present, slowly, until it has crept out the other side of the channel and is thrown back into the chaotic part of the map. The figure measures both halves of the geometry directly on the map’s own iterate: the gap is proportional to the distance from the bifurcation, halving when the distance halves, and the curve near its closest approach is a parabola with a definite curvature.
Why the square root
Those two measured facts are the whole of the scaling law.
Near its closest approach the gap between the curve and the diagonal is, to leading order, , where is the distance along the channel from the narrowest point, is the curvature, and is the gap at the narrowest point. An orbit’s step through the channel is that gap, so in a long channel the orbit’s position obeys, to a good approximation, . Counting the steps from one end of the channel to the other is an integral,
the familiar arctangent, which reaches for a channel long compared with its narrowest part. And since the gap grows in proportion to the distance below the bifurcation, the passage time grows as .
A hundred times closer to the cycle’s birth, the calms last ten times longer. The exponent is not a property of the logistic map, of the three-cycle, or of anything chaotic. It comes from a parabola meeting a line and from the gap between them growing linearly, which is what happens at every saddle-node bifurcation in every smooth system. The chaos is needed only to bring the orbit back to the channel after each passage; the length of the calm is decided entirely by the channel.
The calms, measured
The derivation assumes a long channel, a small gap and a clean parabola. The map can be asked directly whether those assumptions hold.
Over three decades of distance the mean calm grows from 245 iterates to 8,125, and the fitted slope on logarithmic axes is −0.506. The longest possible passage through the channel, computed from the gap and curvature measured at each setting, has slope −0.500 exactly, and lies a little above the mean at every setting — because a calm begins wherever the burst happens to drop the orbit, which is usually somewhere inside the channel rather than at its entrance.
The law is a limit, and it is worth being plain about where. Measured further from the bifurcation, at a distance of or , the channel is no longer long compared with its narrowest part, the calms are only a few dozen iterates, and the local slope drifts away from −½. The figure’s settings were chosen where the measured slope has settled, which is below about — and a sweep of real data that happened to sit in the drifting region would find an exponent that was not −½ without contradicting anything.
A waiting time with a ceiling
A sequence of bursts at irregular moments looks, from outside, like a random process, and the most familiar random waiting time is a nucleus with no clock: exponential, memoryless, with no longest wait. The calms are not that.
The distribution of calm lengths is nearly the opposite of an exponential. It rises towards a maximum rather than falling from one, piles up just below the longest passage the channel allows, and stops — the opposite of an exponential that holds only in the middle and fails at its ends, this one has no middle to be exponential in. In six million iterates at a distance of there are nearly twenty thousand calms, and not one of them is longer than 342 iterates against a longest passage of 358.
The shape comes from the reinjection. A burst drops the orbit back somewhere near the channel, and the calm that follows lasts as long as the remaining passage from that point. An orbit re-entering near the entrance creeps through the whole channel and gives a long calm; one re-entering near the middle gives a shorter one; the channel’s own shape — slow in the middle, fast at the ends — concentrates the lengths near the maximum. The waiting time between bursts carries a memory of the geometry that produced it, and a histogram of waiting times that stops sharply at a ceiling is a signature a record of bursts can be tested for.
Chaos that fades rather than stops
At the bifurcation the three-cycle becomes stable and the chaos ends. Approaching from below, it does not end abruptly; it thins out.
The Lyapunov exponent measures the average rate at which neighbouring orbits separate, and in an intermittent orbit the separation happens almost entirely during the bursts: through the channel, neighbouring orbits creep along together. As the calms lengthen, bursts become rarer — in proportion to the square root of the distance, since that is how often a calm ends — and the average separation rate falls with them. So the exponent should vanish as the square root of the distance, and measured at settings from to below the bifurcation it falls from 0.0914 to 0.0033 with a fitted slope of 0.48.
Further from the edge the same measurement grows only as the 0.32 power, for the reason the calm lengths drift: the calms are too short for the channel to dominate them. The chaos does not switch off at the bifurcation as a light does. It fades, and the fading has an exponent that belongs to the channel rather than to the chaos.
The same bottleneck, elsewhere
The argument used nothing about maps except a parabola near a line, and the same parabola appears wherever something is pushed just past the point at which a stable state disappears.
A pendulum with strong friction — the overdamped case of the three ways of coming to rest — pushed by a steady torque, settles at an angle where the torque balances gravity. Increase the torque past the largest gravity can balance and the pendulum goes over the top — but just past that threshold it lingers, for a long time, near the angle where the balance used to be, before swinging round and returning to linger again. The time per revolution grows as the inverse square root of the excess torque, by the same integral, because the stable and unstable resting angles have merged and left a narrow gap in the pendulum’s equation of motion.
That equation is exactly the equation of a Josephson junction. The phase difference across a superconducting junction obeys the driven, overdamped pendulum equation, with the bias current playing the torque and the critical current playing the largest torque gravity can resist. Above the critical current the phase slips, and the voltage that is a frequency is the rate of those slips. Just above the critical current, the slips are separated by long pauses in which the phase lingers near its vanished resting value, and the average voltage rises as the square root of the excess current, . A superconducting junction just above its critical current and the logistic map just below its three-cycle window are the same bottleneck, with a voltage measuring in one what the calm lengths measure in the other.
Neurons of one common type begin to fire repetitively the same way. Below a threshold current the cell rests; just above it, the resting state has vanished in a saddle-node, the membrane voltage lingers in the ghost of that state between spikes, and the firing rate starts from zero and rises as the square root of the excess current. The long quiet intervals of a slowly firing cell are ghosts of a resting state, as the calms are ghosts of a cycle.
The lingering near a vanished fixed point is related to the slowing down near a critical point that the point at which the two become one describes, and both are the dynamical signature that a system is close to a change in what it is able to do — which is why ecologists and climate scientists look for lengthening recovery times as a warning that a threshold is near.
Other kinds of intermittency
The saddle-node route is the intermittency Pomeau and Manneville classified as type I, to distinguish it from two others. All three belong to damped systems; a frictionless one reaches chaos by the destruction of invariant curves instead, and has no calms of this kind. In type II, a stable fixed point loses stability to a spiral, and the orbit spends its calms spiralling slowly away from the ghost of a steady state; in type III, the instability is of the period-doubling kind, and the calms are nearly periodic with a slowly growing alternation. Both have calms whose mean length grows as the inverse of the distance to threshold rather than its inverse square root, because the orbit’s escape is governed by a linear instability rather than by a parabolic channel.
The distinction matters practically. An experiment that measures how calm lengths scale as a control parameter approaches threshold can identify which kind of bifurcation it is near, without knowing the system’s equations — the same move the map a dripping tap turns out to be made with the Feigenbaum ratio. The exponent is a fingerprint of the local geometry of the bifurcation, and it is visible in a record of when bursts happened.
Where the map stops describing an experiment
Noise closes the channel. The passage time grows without limit only in a noiseless system. Any real noise kicks the orbit across the narrow part of the channel, and once the distance to the bifurcation is small enough that the gap is comparable with the noise, the calms stop lengthening. A measured mean calm length that grows as the inverse square root and then levels off is reading the noise level, not a failure of the theory.
The reinjection is global. The scaling exponent belongs to the channel; the distribution of calm lengths, and so the mean’s prefactor, depends on where the bursts drop the orbit, which depends on the whole map. Two systems near the same kind of bifurcation share an exponent and not a histogram.
A calm has to be defined. Detecting calms requires a threshold — here, repeating to within 0.004 every third step — and the measured mean depends on it: with a threshold of 0.001 the mean at is about ten per cent longer. The exponent does not depend on the threshold once the calms are long; the numbers do.
Real systems are not one-dimensional maps. The logistic map stands for any system whose sampled dynamics is effectively one-dimensional, which is the condition the dripping tap essay set out. A system with several unstable directions can pass near a saddle-node in more complicated ways, and a convection cell’s intermittency is a map only after the same contraction of phase space that made its period doubling one.
And the law is a limit. The measured slopes settle at −½ and ½ only close to the bifurcation, and drift measurably away from it. That is a statement about the approach to the asymptote, not a failure of it, and it means an exponent measured over a range that includes the drift will be wrong in a definite direction.
What a time series cannot show
The series figure shows calms and bursts and cannot show why the calms are calm. The channel lives in the graph of the third iterate, which the series does not contain: seen one value at a time, the creep through the channel is a near-repetition, and nothing about it announces that the repetition is running out. The geometry that decides the calm’s length is invisible from inside the calm.
Nor can any finite record show the ghost’s defining property, which is that it becomes a real cycle at a setting just beyond the record’s range. A system that has lingered near a three-cycle for a hundred thousand iterates is not distinguishable, by that record alone, from one that will linger there forever. The bifurcation is inferred from how the calms change as the setting changes, never from one setting.
Still open: telling a ghost from noise
Bursts separated by quiet intervals are found in records of many systems whose equations nobody has written down — lasers, turbulent boundary layers, the firing of neurons, climate proxies with abrupt transitions — and the question each time is whether the quiet intervals are ghosts of a nearby bifurcation or simply a noisy system switching between two states. The two produce superficially similar records and imply different things: a ghost means the system is close to acquiring a new stable state, and its calms will lengthen predictably as a parameter changes; a noise-driven switch means no such change is coming.
The calm-length distribution is the obvious discriminator — a ghost’s calms pile up below a ceiling, a noise-driven switch gives an exponential tail — and in clean simulations it works. In real records it is weakened by exactly the noise that closes the channel, by short records with few calms, and by the threshold that defines a calm in the first place. How reliably intermittency can be identified, and its kind determined, from a single noisy record of finite length is an open problem in the analysis of data from systems near tipping points.
The habit worth carrying away is to read long quiet intervals as a clue about what is nearby. A system that lingers has usually lost a stable state recently, or is about to gain one, and the rate at which the lingering grows as a parameter changes is a measurement of the geometry of that loss.
Part 5 of 5
This essay is one argument about Chaos. The others:
The objects named here
The third axis, after the field and the reading path: the things themselves, and every essay that touches each one.
AttractorBifurcationChaosIntermittencyJosephson effectLogistic mapLyapunov exponentSaddle node bifurcation