Ice
crystals nucleate and grow when a water solution is cooled
below its freezing point. The growth velocities and morphologies of
the ice crystals depend on many parameters, such as the temperature
of ice growth, the melting temperature, and the interactions of solutes
with the growing crystals. Three types of morphologies may appear:
dendritic, cellular (or fingerlike), or the faceted equilibrium form.
Understanding and controlling which type of morphology is formed is
essential in several domains, from biology to geophysics and materials
science. Obtaining, in situ, three dimensional observations without
introducing artifacts due to the experimental technique is nevertheless
challenging. Here we show how we can use laser scanning confocal microscopy
to follow in real-time the growth of smoothed and faceted ice crystals
in zirconium acetate solutions. Both qualitative and quantitative
observations can be made. In particular, we can precisely measure
the lateral growth velocity of the crystals, a measure otherwise difficult
to obtain. Such observations should help us understand the influence
of the parameters that control the growth of ice crystals in various
systems.