The collection

Every essay — page 32

One idea per essay, ordered so that the earlier ones set up the later ones — but nothing here depends on being read in sequence. Essays 621–640 of 909.

Galaxies

Where the unknown stops being a number and becomes a profile — and most of it is not light.

Gravitation

Two bodies pulling on each other, and everything that goes wrong at three.

Orbits

Kepler's three laws, and the family of curves a single force allows.

The observed sky

Coordinates, seasons, phases and shadows — geometry seen from inside it.

Spaceflight

Celestial mechanics used forwards — where to burn, and what it costs.

Starlight

Distance, brightness and colour: what can be measured when nothing can be visited.

Stars

The diagram that sorted them, and the one quantity that decides a star's whole life.

Cosmology

One object, seen once, from inside — and every number in it the output of a model.

Orbits

Kepler's three laws, and the family of curves a single force allows.

One history of mass loss, three orbits, three outcomes. The eccentricity of three planets' orbits against the fraction of the star's mass lost so far, as the star sheds 45 per cent of its mass in 6 equal pulses at irregular intervals. Each planet starts with e = 0.05. The pulses are the same events in the star's own time, and the planets differ only in their periods, so each pulse lasts 3, 0.3, 0.03 orbital periods respectively. For the innermost planet, to which every pulse is slow, the eccentricity ends at 0.050: the orbit swells and keeps its shape. For the outermost, to which every pulse is sudden, each pulse kicks the eccentricity by an amount set by where the planet happened to be, and it ends at 0.298. The middle planet ends at 0.090. The same total loss leaves three different shapes, and only one of them is predicted by either limit alone.

The size forgets how the mass was lost, and the shape does not

A dying star loses half its mass, and a planet round it keeps its orbit's shape if the loss is slow and has it scrambled if the loss is sudden. Real stars lose mass in pulses — each one sudden or slow depending on the planet — and what survives a train of pulses is neither answer: the orbit's size settles to the slow value quickly, while its eccentricity random-walks and keeps a record of the history.

5 figures · Effective potential
How much of a population is driven how close. The fraction of an isotropic population of inner orbits whose Kozai–Lidov cycling brings 1 − e below a given value within 150 secular timescales, against that value, both logarithmic, for octupole strengths ε = 0, 0.01, 0.03; each curve is 128 integrated orbits with random pericentres and nodes. The thin line is the quadrupole closed form, √((3/5)(1 − (1 − q)²)), which the ε = 0 population follows. At 1 − e = 0.01 the fractions are 9.4, 20.3, 40.6 per cent; at 0.001, 3.1, 18.0, 38.3. The octupole matters most where the quadrupole is weakest — at the extreme closeness a planet needs to be captured by tides, or a pair of compact objects needs to merge — because it adds orbits whose quadrupole cycle stopped far short of it.

Eleven in a hundred by geometry, and the rest by waiting

A distant companion drives an inner orbit through cycles of eccentricity, and whether a given system reaches a dangerously close approach depends on its inclination. Counted over a population with random orientations, the answer at quadrupole order is pure geometry — about eleven per cent reach one per cent of their semi-major axis, all at the same inclination. An eccentric outer orbit multiplies that share, spreads the inclinations, and makes the count depend on how long the systems have been waiting.

5 figures · Kozai–Lidov
The same tilt, and ice ages of two different lengths. Top: the obliquity anomaly in degrees from the five largest terms of the standard series, over 2 million years of model time; it is dominated by the 41,000-year cycle and has no power at all near 100,000 years. Bottom: ice volume in a threshold model driven by it — the ice grows steadily, and it collapses whenever volume plus a multiple of the obliquity anomaly crosses a threshold, marked by dots. For the first 1 million years the threshold is low and the ice collapses at nearly every obliquity maximum, on average every 43 thousand years. At the vertical line the threshold is raised, and nothing else changes: the ice now survives one or two obliquity maxima and collapses at the second or third, every 108 thousand years on average. The forcing is identical on both sides; the ice sheet counts it differently.

An ice sheet that skips a beat of the tilt

The last eight hundred thousand years of ice ages come roughly every hundred thousand years, and the Earth's orbit has no forcing of any strength at that period. A model in which an ice sheet collapses only when it is both large and warmed by a high-obliquity summer reproduces the rhythm with nothing but the forty-one-thousand-year tilt — the ice sheet grows through one or two maxima and falls on the next — and a slow rise in how large the ice must grow turns the older forty-one-thousand-year world into the newer one without any change in the orbit.

5 figures · Orbital averages

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