Astronomy & Celestial Mechanics
the sky, computed
Concept

Comet — where it appears

A small icy body from the outer solar system that develops a coma of gas and dust when sunlight warms it. Its ices and isotopes preserve conditions from where it formed, which makes comets samples of the cold outer disc that built the giant planets.

Named by 2 essays across 2 fields — each of them below, with the objects they name alongside it.

An invariant that moves by 8.0e-3 once the planet's orbit is real. The Tisserand parameter of a comet on an orbit of semi-major axis 5 and eccentricity 0.8, followed through a close passage of Jupiter, integrated twice. The lower trace has Jupiter on a perfect circle, which is the problem the parameter is an exact constant of: it survives the encounter having moved by 1.0e-4, which is the integrator's own error and not a physical change, and the spike at the moment of closest approach is the osculating elements being briefly meaningless while the comet is inside Jupiter's sphere of influence rather than the constant failing. The upper trace is the same encounter with Jupiter on its real orbit, eccentricity 0.0489. The parameter comes out changed by 8.0e-3, 79 times as much, because the Jacobi constant exists only when the rotating frame is uniformly rotating and a planet on an ellipse does not provide one. That number is small and it is not negligible: comet families are separated by boundaries in this parameter placed to two decimal places, and a comet that drifts across one over several encounters has changed class without anything having happened to it that a single encounter could account for.

An invariant that is only almost one

The Tisserand parameter survives a close encounter with Jupiter exactly, and comet families are separated by boundaries in it drawn to two decimal places. The exactness holds for a Jupiter on a circle. Jupiter's eccentricity is 0.0489, and integrating the same encounter twice shows what that costs.

orbits · Tisserand parameter The deuterium in the solar system's water, body by body. The ratio of deuterium to ordinary hydrogen in water, on a logarithmic axis, for the Earth's oceans and for the bodies it has been measured in, with the protosolar hydrogen and the water around young protostars as the two ends of the range. The oceans, 1.6·10⁻⁴, are 7.8 times the protosolar value; the carbonaceous and enstatite chondrites sit within ten per cent of them, as do two comets from the Jupiter family. The comets from the Oort cloud, and 67P from the Jupiter family, are two to three and a half times richer. Water made in a cold molecular cloud is richer still, near 0.001. The ratio is fixed when the water forms or last exchanges with hydrogen gas, and is not changed by anything that happens afterwards except escape, so it is a label that each body's water carries from wherever it was made.

Water that remembers how cold it was

Every water molecule in the solar system carries a label: the share of its hydrogen that is deuterium, fixed when the water last exchanged with hydrogen gas. Water made in the cold cloud the Sun formed from is rich in it; water that passed through the hot inner disc is poor. The Earth's oceans sit within ten per cent of the carbonaceous meteorites and twice below most comets — a record of where the water was assembled, and of how much of it had ever been hot.

exoplanets · The snow line

Named alongside it

The objects these essays reach for when they reach for this one.

Carbonaceous chondriteCircular restricted problemClose encounterDeuteriumGravity assistIsotopic ratioJacobi constantMolecular cloudOrbital elementsOsculating elementsProtoplanetary discResonance

All concepts