Meridional circulation — where it appears
Named by 3 essays across 2 fields — each of them below, with the objects they name alongside it.
A shear layer that should have spread
The Sun's convection zone turns differentially — its equator laps its poles about once every three months — and the radiative interior below turns as one rigid piece. Between them is a transition four per cent of the radius thick. Nothing in hydrodynamics keeps a velocity discontinuity that thin for four and a half billion years.
One step of memory kept at the poles
The amplitude of a solar maximum tells almost nothing about the next one. The polar field measured at the minimum in between tells a great deal — so the cycle is not a pendulum with momentum but a process with exactly one state variable, and the variable is a field of a few gauss at latitudes nobody can see well.
The circulation that should have stirred every fast rotator
A rotating star in radiative equilibrium cannot be balanced in pressure and in heat at the same time, and the mismatch drives a slow circulation from pole to equator. The classical estimate of its speed says that any star turning at more than a tenth of its break-up rate should be stirred from core to surface within its life, bringing the nitrogen of hydrogen burning up with it. Some fast rotators show that nitrogen and some do not, and some slow rotators show it when they should not — including more than the angle of their axes can explain.
Named alongside it
The objects these essays reach for when they reach for this one.
TachoclineAngular momentum transportBabcock leighton dynamoCNO cycleConvective envelopeCritical rotationDifferential rotationDynamoFlux transportGravity darkeningHelioseismologyInternal magnetic field