The Great Arctic Cyclone of 2012 from satellite.

It works like a spoon stirring hot coffee, attracting cold air from Siberia. In this respect they serve as confined research regions, like a unique field laboratory experiment.

This post presents an article by John S. Wettlaufer who sees not only the oceans but cosmic patterns in coffee cup vorticies. His essay is The universe in a cup of coffee.  (Bolded text is my emphasis.)

John Wettlaufer is the A. M. Bateman Professor of Geophysics, Physics, and Applied Mathematics at Yale University in New Haven, Connecticut.

As people throughout the world awake, millions of them every minute perform the apparently banal act of pouring cold milk into hot coffee or tea. Those too groggy to reach for a spoon might notice upwelling billows of milk separated by small, sinking, linear dark features such as shown in panel a of the figure. The phenomenon is such a common part of our lives that even scientists—trained to be observant—may overlook its importance and generality. The pattern bears resemblance to satellite images of ocean color, and the physics behind it is responsible for the granulated structure of the Sun and other cosmic objects less amenable to scrutiny.

(a) Everyone knows that if you wait for a while coffee will get cold. The primary agent doing the cooling is evaporatively driven convection. Pour cold milk into hot coffee and wait. The cold milk mixes very little as it sinks to the bottom of the cup, but eventually cold plumes created by evaporation at the surface sink down and displace the milk. In time, a pattern forms of upwelling (lighter) and downwelling (darker) fluid.

Archimedes pondered the powerful agent of motion known as buoyancy more than two millennia ago. Children do, too, when they imagine the origins of cloud animals on a summer’s day. The scientific study of thermal and compositional buoyancy originated in 1798 with a report by Count Rumford intended to disabuse believers of the caloric theory. Nowadays, buoyancy is at the heart of some of the most challenging problems in nonlinear physics—problems that are increasingly compelling. Answers to fundamental questions being investigated today will have implications for understanding Earth’s heat budget, the transport of atmospheric and oceanographic energy, and, as a corollary, the climate and fate of stars and the origins of planets. Few avenues of study combine such basic challenges with such a broad swath of implications. Nonetheless, the richness of fluid flow is rarely found in undergraduate physics courses. 

Wake up and smell the physics

The modern theory of hydrodynamic stability arose from experiments by Henri Bénard, who heated, from below, a thin horizontal layer of spermaceti, a viscous, fluid wax. For small vertical temperature gradients, Bénard observed nothing remarkable; the fluid conducted heat up through its surface but exhibited no wholesale motion as it did so. However, when the gradient reached a critical value, a hexagonal pattern abruptly appeared as organized convective motions emerged from what had been an homogenous fluid. The threshold temperature gradient was described by Lord Rayleigh as reflecting the balance between thermal buoyancy and viscous stresses, embodied in a dimensionless parameter now called the Rayleigh number. 

When the momentary thermal buoyancy of a blob of fluid—provided by the hot lower boundary—overcomes the viscous stresses of the surrounding fluid, wholesale organized motion ensues. The strikingly structured fluid, with its up-and-down flow assuming specific geometries, is an iconic manifestation of how a dissipative system can demonstrate symmetry breaking (the up-and-down flow distinguishes horizontal positions even though the lower boundary is at a uniform temperature), self-organization, and beauty. (See the article by Leo Kadanoff in PHYSICS TODAY, August 2001, page 34.)

Astrophysicists and geophysicists can hardly make traction on many of the problems they face unless they come to grips with convection—and their quests are substantially complicated by their systems’ rotations. Despite the 1835 publication of Gaspard-Gustave Coriolis’s Mémoire sur les équations du mouvement relatif des systèmes de corps (On the Equations of Relative Motion of a System of Bodies), debate on the underlying mechanism behind the deflection of the Foucault pendulum raged in the 1905 volume of Annalen der Physik, the same volume in which Albert Einstein introduced the world to special relativity. Maybe the lack of comprehension is not so surprising: Undergraduates still more easily grasp Einstein’s theory than the Coriolis effect, which is essential for understanding why, viewed from above, atmospheric circulation around a low pressure system over a US city is counterclockwise but circulation over an Australian city is clockwise. 

Practitioners of rotating-fluid mechanics generally credit mathematical physicist Vagn Walfrid Ekman for putting things in the modern framework, in another key paper from 1905. Several years earlier, during his famous Fram expedition, explorer Fridtjof Nansen had observed that ice floes moved to the right of the wind that imparted momentum to them. Nansen then suggested to Ekman that he investigate the matter theoretically. That the deflection was due to the ocean’s rotating with Earth was obvious, but Ekman described the corrections that must be implemented in a noninertial reference frame. Since so much in the extraterrestrial realm is spinning, scientists taken by cosmological objects eventually embraced Ekman’s formulation and sought evidence for large-scale vortex structures in the accretion disks around stars. Vortices don’t require convection and when convection is part of a vortex-producing system, additional and unexpected patterns ensue. 

Cream, sugar, and spinning

The Arctic Ocean freezes, cooling and driving salt into the surface layers. Earth’s inner core solidifies, leaving a buoyant, iron-depleted metal. Rapidly rising air from heated land surfaces creates thunderstorms. Planetary accretion disks receive radiation from their central stars. In all these systems, rotation has a hand in the fate of rising or sinking fluid. What about your steaming cup of coffee: What happens when you spin that?

(b) Several views of a volume of water 11.4 cm deep with a cross section of 22.9 × 22.9 cm. Panel b shows the liquid about 7.5 minutes after the fluid is set in motion at a few tenths of a radian per second. The principal image indicates particle density (light is denser) at a depth of 0.6 cm below the surface. The inset is a thermal image of the surface

Place the cup in the center of a spinning record player— some readers may even remember listening to music on one of those. The friction from the wall of the cup transmits stresses into the fluid interior. If the coffee is maintained at a fixed temperature for about a minute, every parcel of fluid will move at the same angular velocity; the coffee is said to be spun up.

On the time scales of contemporary atmospheric and oceanographic phenomena, Earth’s rotation is indeed a constant, whereas the time variation of the rotation could be important for phenomena in planetary interiors, the evolution of an accretion disk, or tidal perturbations of a distant moon. Thus convective vortices are contemplated relative to a rotating background flow. Perturbations in the rotation rate revive the role of boundary friction and substantially influence the interior circulation. Moreover, evaporation and freezing represent additional perturbations, which alter how the fluid behaves as stresses attempt to enforce uniform rotation. Returning to the coffee mug as laboratory, the model system shown in panel b of the figure reveals how the added complexity of rotation momentarily organizes the pattern seen in panel a into concentric rings of cold and warm fluid.

(c) Panel c shows the breakup of the rings, 11 minutes after the initiation of rotation, due to a shearing instability.

Fundamental competitions play out when you rotate your evaporating coffee. As we have seen, evaporative cooling drives narrow regions of downward convection; significant viscous and Coriolis effects balance each other in those downwelling regions. Rotation then dramatically organizes the sinking cold sheets and rising warm billows into concentric rings that first form at the center of the cup. By about 7.5 minutes after rotation has been initiated, the rings shown in panel b have grown to cover most of the horizontal plane. Their uniform azimuthal motion exists for about 3.5 minutes, at which time so-called Kelvin–Helmholtz billows associated with the shearing between the rings appear at their boundaries, grow, and roll up into vortices; see panel c. Three minutes later, as shown in panel d, those vortices lose their azimuthal symmetry and assemble into a regular vortex grid whose centers contain sinking fluid.

(d) As panel d shows, at 14 minutes the breakup leads to a grid of vortices. (Adapted from J.-Q. Zhong, M. D. Patterson, J. S. Wettlaufer, Phys. Rev. Lett. 105, 044504, 2010.)

Panel d shows one type of coherent structure that forms in rotating fluids and other mathematically analogous systems if the persistence time of the structure—vortices here— is much longer than the rotational period. Other well-known examples are Jupiter’s Great Red Spot, which is an enduring feature of the chaotic Jovian atmosphere, and the meandering jet streams on Earth.

Moreover, persistent vortices in superconductors and superfluids organize themselves. Indeed, it appears that vortices in superconductors are as mobile as their counterparts in inviscid fluids. And although scientists have long studied rotating convective superfluids, the classical systems considered in this Quick Study suggest that we may yet find surprising analogies in superconductors. Will we one day see superconducting jet streams?

If you are reading this article with a cup of coffee, put it down and take a closer look at what is going on in your cup.

Summary

Wettlaufer has been an advocate for getting the physics right in climate models.  His analogy of a cuppa coffee is actually a demonstration of mesoscale fluid and rotational dynamics and perturbations that still defy human attempts to simulate climate operations.