Why Water Heats Up and Cools Down So Slowly ✛ ✦

Original: "Structural Origin of Water Heat Capacity Anomaly from Classical and Quantum Simulations"
arXiv:2607.08957 · 2026-07-09 · CC BY 4.0 · 1 min
Scientists have found that the secret lies not in quantum effects, but in the constant rearrangement of molecules between two states.

Water, a liquid we've known since childhood, behaves like a crowded subway car. The hydrogen and oxygen molecules don't just jostle about: as they absorb energy, they constantly switch from a tight packing to a looser one. Each such move requires extra energy, so water soaks up heat with barely a rise in temperature.

When supercooled to –43°C, this mechanism hits a peak: water “guzzles” heat with record-breaking greed.

For a long time, the cause was sought in quantum thermodynamics, but computer simulations powered by machine learning revealed otherwise. Quantum tweaks merely shift the backdrop; the star of the show is entropy (a measure of disorder)—its sharp jump when the packings switch. The ideas of Max Planck and Richard Feynman helped shape the model, but the answer came not from the quantum world, but from the geometry of hydrogen bonds.

Without this quirk, the ocean, which has absorbed 90% of the planet’s excess heat over 50 years, would be boiling by now. Water acts as a giant climate buffer.

Heating one liter of water by one degree takes as much energy as hoisting a 426-kilogram weight one meter up.

C = \frac{Q}{\Delta T}
Heat capacity C shows how much heat Q is needed to change a substance’s temperature by ΔT degrees.
Scientists
Emmy NoetherAlbert EinsteinDaniel BernoulliArchimedesRudolf ClausiusGustav Kirchhoff
Concepts
heat capacity waste heat Upper 300 m temperature Warm water volume joule per kelvin temperature difference carnot limit supercooled water chemical potential thermal bath quantum mpemba effect marine heatwave quantum thermometer thermal jitter information thermodynamics power consumption heating efficiency enthalpy thermoelectric device