Birefringent Ice
toptics
A
Highlights
Ice crystals on a car windscreen illuminated by a street lamp. Pictured in Northern Russia by Boris Borisovich (journal).

Image ©Boris Borisovich, shown with permission




Ice structure                              Birefringence & airplane windows
   
      Ice colours               Weaker ice colours from thin film interference

  Internal strain

                    Double vision



Ice has a rather open hexagonal structure. We can thank that for our existence for otherwise ice would not float on water and Earth's climate would be quite different.

An ice crystal's properties depend on direction. It is anisotropic. As a result light refracts differently depending its direction through the crystal. Unpolarised light splits into two polarised components travelling in slightly different directions.

Waves of the differently refracted polarised components overlap and interfere. The effect is wavelength dependent and so we see birefringent colours.