Sea ice types

Pancake Ice
Pancake Ice seen from the Aurora Australis, a week from Hobart (Photo: Peter Schuller)
Sea ice breaking outThe Aurora Australis in sea iceSea ice near Casey stationSea ice forming near the Davis beachSun reflecting off water and slushy ice known as frazil iceFrazil ice built up at the shore amongst rocksA close up of frazil ice on top of water at Casey stationAerial shot of fast ice at Commonwealth Bay

Sea ice is any form of ice found at sea which has originated from the freezing of sea water. It can be broadly described as new ice, young ice, first-year ice and old ice. These categories broadly reflect the age of the ice and include different forms and thicknesses of ice at various stages of development.

Even in winter only a small fraction of sea ice close to the Antarctic continent occurs as a continuous and uniform sheet. This ‘land fast’ ice is pinned to the coast and does not move. The majority of the ice occurs in a wide band around the continent and is referred to as ‘pack ice’. This is a region of highly variable ice conditions, including broken pieces (floes) with a range of sizes, ages and thicknesses, present in varying concentrations. The pack is highly mobile, moving with the wind and currents, with its characteristics constantly changing. There is frequently some open water (leads) between the floes and it is common to see ice at various stages of development present in the same area. This is the result of the dynamic nature of the pack, with the thickness of floes increasing through ‘rafting’ and ‘ridging’ (see definitions below) as they interact, and new open water areas constantly being created, allowing new ice to form.

Some of the different forms of Antarctic sea ice are described below. These definitions come from the Antarctic Sea Ice Process and Climate website, which has a comprehensive description of sea ice – its formation, characteristics, importance in climate and marine ecosystems, and images. The italicised descriptions are the standard definitions published by the World Meteorological Organisation (World Meteorological Organisation. 1970. WMO sea-ice nomenclature, terminology, codes and illustrated glossary. WMO/OMM/BMO 259, TP 145. Geneva, World Meteorological Organisation).

The Woods Hole Oceanographic Institution website has useful information about Arctic sea ice.

Brash ice

Accumulations of floating ice made up of fragments not more than 2 m across; the wreckage of other forms of ice.

Brash is common between colliding floes or in regions where pressure ridges have collapsed.

First year ice

Sea ice of not more than one winter's growth, developing from young ice; thickness (typically) 30 cm - 2 m. May be subdivided into thin first-year ice/white ice, medium first-year ice and thick first-year ice.

Frazil ice

Fine spicules or plates of ice, suspended in water.

Frazil ice formation represents the first stage of sea ice growth. The frazil crystals are usually suspended in the top few centimetres of the surface layer of the ocean and give the water an oily appearance. In the open ocean the crystals may form, or be stirred to a depth of several metres by wave-induced turbulence.

Grease ice

A later stage of freezing than frazil ice when the crystals have coagulated to form a soupy layer on the surface. Grease ice reflects little light, giving the surface a matt appearance.

Grease ice behaves in a viscous fluid-like manner, and does not form distinct ice floes.

Grey ice

Young ice 10-15 cm thick. Less elastic than nilas and breaks on swell. Usually rafts under pressure.

Grey-white ice

Young ice 15-30 cm thick. Under pressure more likely to ridge than to raft

Multi-year ice

Old ice up to 3 m or more thick which has survived at least two summers' melt. Hummocks (hillocks of broken ice that have been forced up by pressure) even smoother than in second-year ice, and the ice is almost salt-free. Colour, where bare, is usually blue. Melt pattern consists of large interconnecting irregular puddles and a well-developed drainage system.

New ice

A general term for recently formed ice which includes frazil ice, grease ice, slush and shuga.

Nilas ice

A thin elastic crust of ice, easily bending on waves and swell and under pressure, thrusting in a pattern of interlocking ‘fingers’ (finger rafting). Has a matt surface and is up to 10 cm in thickness. May be subdivided into dark nilas and light nilas.

Dark nilas is < 5 cm thick and very dark in colour. Light nilas is 5-10 cm thick and reflects proportionately more light than dark nilas, depending on its thickness.

Pancake ice

Predominantly circular pieces of ice from 30 cm - 3 m in diameter, and up to 10 cm in thickness (unrafted), with raised rims due to the pieces striking against one another. It may be formed on a slight swell from grease ice, shuga or slush or as the result of the breaking of ice rind, nilas or, under severe conditions of swell or waves, of grey ice.

Rafting

Pressure process whereby one piece of ice overrides another. Most common in new and young ice

Ridging

The pressure process by which sea ice is forced into ridges.

A ridge is a line or wall of broken ice forced up by pressure. May be fresh or weathered. The submerged volume of broken ice under a ridge, forced downwards by pressure, is termed an ice keel.

Second-year ice

Old ice which has survived only one summer's melt. Because it is thicker and less dense than first-year ice, it stands higher out of the water. In contrast to multi-year ice, summer melting produces a regular pattern of puddles. Bare patches and puddles are usually greenish-blue.

Shuga ice

An accumulation of spongy white lumps, a few centimetres across; they are formed from grease ice or slush and sometimes from anchor ice rising to the surface.

Slush

Snow which is saturated and mixed with water on land or ice surfaces, or as a viscous floating mass in water after heavy snowfall.

Young ice

Ice in the transition stage between nilas and first-year ice, 10-30 cm in thickness. May be subdivided into grey ice and grey-white ice.

 

This page was last modified on 3 November 2010.