The relative dielectric constant shows a temperature maximum
Instead of falling monotonically, the dielectric constant shows a maximum at a certain temperature.
Scientific Explanation
For liquid water, the dielectric constant rises with decreasing temperature — a behavior also observed in other polar liquids, because lower temperatures favor the alignment of dipoles in an electric field. For ice, this trend initially continues: the dielectric constant of ice at 0 degrees Celsius is even higher than that of liquid water.
However, upon further cooling, the dielectric constant of ice reaches a maximum and then declines. This temperature maximum is anomalous, since one would naively expect that increasing order at lower temperatures would further enhance the dielectric response.
The explanation lies in the slowing of molecular reorientation. At very low temperatures, the rotational movements of water molecules within the ice lattice freeze out — the molecules can no longer follow the applied field. The relaxation time becomes so long that a measurement at a given frequency no longer fully captures the static dielectric constant. The apparent maximum thus represents a transition from a regime where the dipoles can follow the field to one where they are effectively frozen.
Everyday Relevance
This behavior is relevant for radar technology and remote sensing. Satellites use microwave signals to survey ice sheets and snow cover. The temperature dependence of the dielectric constant determines how strongly signals are reflected or absorbed. The temperature maximum means that the signal response is not monotonically related to temperature — a fact that must be accounted for when interpreting satellite data.