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Buried under the snow of following years, the coarse-grained hoar frost compresses into lighter layers than the winter snow.

As a result, alternating bands of lighter and darker ice can be seen in an ice core.

It can be up to about 20 m thick, and though it has scientific value (for example, it may contain subglacial microbial populations), Cores are often drilled in areas such as Antarctica and central Greenland where the temperature is almost never warm enough to cause melting, but the summer sun can still alter the snow.

In polar areas, the sun is visible day and night during the local summer and invisible all winter.

These data can be combined to find the climate model that best fits all the available data. Coastal areas are more likely to include material of marine origin, such as sea salt ions.