- Aged Ridge
Ridge which has undergone considerable weathering. These ridges are best described as undulations.
- Agglomerated Brash
This term is similar to Jammed Brash Barrier but is not consolidated. This is a Canadian description and not part of the WMO nomenclature.
- Anchor Ice
Submerged ice attached or anchored to the bottom, irrespective of the nature of its formation.
- Arrangement of the Ice
- Drift Ice/Pack Ice
- Ice Cover
- Ice Distribution
- Openings in the Ice
- Ice Edge
- Ice Boundary
- Iceberg Limit.
- Bare Ice
Ice without snow cover.
The study of the measurements of the oceans' depths.
- Batture Floes
Large, thick, uneven and discoloured ice floes that form on the upstream side of shoals and islets in rivers when cold weather precedes or accompanies neap tides. Composed of ice of different thicknesses formed under pressure during ebb tide, the whole mass freezing together and gradually increasing in size with each successive tide. As the range increases between the neap and spring tides, large sections of grounded ice break away and drift down river. This is a Canadian description and not part of the WMO nomenclature.
A large feature of pack/drift ice arrangement longer than it is wide; from 1 km to more than 100 km in width.
- Bergy Bit
A piece of glacier ice, generally showing 1 to less than 5 m above sea level, with a length of 5 to less than 15 m. They normally have an area of 100-300 m2.
- Bergy Water
An area of freely navigable water in which ice of land origin is present. Other ice types may be present, although the total concentration of all other ice is less than 1/10.
Situation in which a vessel is surrounded by ice and unable to move.
Extensive crescent-shaped indentation in the ice edge formed by either wind or current.
- Blocky Iceberg
A flat-topped iceberg with steep vertical sides.
- Brash Ice
Accumulation of floating ice made up of fragments not more than 2 m across, the wreckage of other forms of ice.
This term refers to a particular length of time in which ice disappears in a given area (generally 1 to 2 weeks). However, breakup does not necessarily imply a decay or melt of ice, but can also indicate a movement of ice out of a particular area.
A downward projection from the underside of the ice canopy; the submerged counterpart of a hummock.
The breaking away of a mass of ice from an ice wall, ice front or iceberg.
- Close Pack/Drift
Floating ice in which the concentration is 7/10 to 8/10, composed of floes mostly in contact with one another.
- Compact Ice
Floating ice in which the concentration is 10/10 and no water is visible.
- Compacted Ice Edge
Clear-cut ice edge compacted by wind or current, usually on the windward side of an area of ice.
Pieces of floating ice are said to be compacting when subjected to a converging motion, which increases ice concentration and/or produces stresses which may result in ice deformation.
- Concentration Boundary
A line approximating the transition between two areas of floating ice with different concentrations.
The transmission of heat through matter.
- Consolidated Ice
Floating ice in which the concentration is 10/10 and the floes are frozen together.
- Consolidated Ridge
A ridge in which the base has frozen together.
The transfer of heat through a fluid.
Any fracture of fast ice, consolidated ice or a single floe which may have been followed by separation ranging from a few centimetres to 1 m.
- Dark Nilas
Nilas up to 5 cm in thickness and which is very dark in colour.
- Deformed Ice
A general term for ice which has been squeezed together and in places forced upwards and downwards. Subdivisions are rafted ice, ridged ice and hummocked ice.
- Difficult Area
A general qualitative expression to indicate that the relative severity of the ice conditions, prevailing in an area, are such that navigation in it is difficult.
- Diffuse Ice Edge
Poorly defined ice edge limiting an area of dispersed ice, usually on the leeward side of an area of ice.
Ice fields or floes in an area that are subjected to a diverging motion, reducing ice concentration and/or relieving stresses in the ice.
- Domed Iceberg
An iceberg which is smooth and rounded on top.
- Dried Ice
Ice surface from which water has disappeared after the formation of cracks and thaw holes. During the period of drying the surface whitens.
- Drift Ice/Pack Ice
Term used in a wide sense to include any area of ice, other than fast ice, no matter what form it takes or how it is disposed. When concentrations are high, i.e., 7/10 or more, the term pack ice is normally used. When concentrations are 6/10 or less the term drift ice is normally used.
- Drydocked Iceberg
An iceberg which is eroded such that a U-shaped slot is formed near or at water level, with twin columns or pinnacles.
- Easy Area
A general qualitative expression to indicate that ice conditions, prevailing in an area, are such that navigation is not difficult.
- Fast Ice
Ice which forms and remains fast along the coast. It may be attached to the shore, to an ice wall, to an ice front, between shoals or grounded icebergs. Vertical fluctuations may be observed during changes of sea level. It may be formed “in-situ” from water or by freezing of floating ice of any age to shore and can extend a few metres or several hundred kilometres from the coast. It may be more than one year old in which case it may be prefixed with the appropriate age category (old, second-year or multi-year). If higher than 2 m above sea level, it is called an ice shelf.
- Fast Ice Boundary
The ice boundary at any given time between fast ice and the pack/drift ice.
- Fast Ice Edge
The demarcation at any given time between fast ice and open water.
- Finger Rafted Ice
Type of rafted ice in which floes thrust “fingers” alternately over and under the other, common in nilas.
- Finger Rafting
Type of rafting whereby interlocking thrusts are formed like "fingers" alternately over and under the other. This is commonly found in nilas and in grey ice.
Old snow which has recrystallized into a dense material. Unlike ordinary snow, particles are to some extent joined together; but, unlike ice, the air spaces in it still connect with each other.
- First-year Ice
Sea ice of not more than one winter’s growth, developing from young ice; 30 cm or greater. It may be subdivided into thin first-year ice – sometimes referred to as white ice –, medium first-year ice and thick first-year ice.
A narrow separation zone between floating ice and fast ice, where the pieces of ice are in a chaotic state. Flaws form when ice shears under the effect of a strong wind or current along the fast ice boundary.
- Flaw Lead
A passageway between ice and fast ice which is navigable by surface vessels.
- Flaw Polynya
A polynya between ice and fast ice.
- Floating Ice
Any form of ice found floating in water. The principal kinds of floating ice are lake ice, river ice and sea ice which form by the freezing of water at the surface and glacier ice formed on land or in an ice shelf. This term includes ice that is stranded or grounded.
Any relatively flat piece of ice 20 m or more across. Floes are subdivided according to horizontal extent as follows:
- Small: 20-100 m across
- Medium: 100-500 m across
- Big: 500-2,000 m across
- Vast: 2-10 km across
- Giant: Greater than 10 km across
- Flooded Ice
Ice which has been flooded and is heavily loaded by water or water and wet snow.
Any break or rupture through very close pack ice, compact ice, consolidated ice, fast ice or a single floe resulting from deformation processes. Fractures may contain brash ice and/or be covered with nilas and/or young ice. Their lengths may vary from a few metres to many kilometres.
- Fracture Zone
An area which has a great number of fractures. Fractures are subdivided as follows:
- Very Small Fracture: 1 to 50 m wide
- Small Fracture: 50 to 200 m wide
- Medium Fracture: 200 to 500 m wide
- Large Fracture: Greater than 500 m wide
Pressure process whereby ice is permanently deformed and rupture occurs. This term is most commonly used to describe breaking across very close ice, compact ice and consolidated ice.
- Frazil Ice
Fine spicules or plates of ice suspended in water.
This term refers to a particular length of time in which ice appears in a given area (generally 1 to 2 weeks). However, freezeup does not necessarily imply a growth of ice, but can also indicate a movement of ice into a particular area.
The number of times an event, value, or characteristic occurs in a given period of time.
- Friendly Ice
An ice canopy containing many large skylights or other features which permit a submarine to surface. There must be more than ten such features per 30 nautical miles (56 km) along the submarine’s track.
- Frost Smoke
Fog-like clouds formed by the contact of cold air with relatively warm water. These can appear over openings in the ice or leeward of the ice edge and may persist while ice is forming.
A mass of snow and ice continuously moving from higher to lower ground or, if afloat, continuously spreading. The principal forms of glaciers are: inland ice sheets, ice shelves, ice streams, ice caps, ice piedmonts, cirque glaciers and various types of mountain (valley) glaciers.
- Glacier Ice
Ice in or originating from a glacier, whether on land or floating on the sea as icebergs, bergy bits, growlers or ice islands.
- Glacier Tongue
Projecting seaward extension of a glacier, usually afloat. In the Antarctic, glacier tongues may extend over many tens of kilometres.
- Grease Ice
A later stage of freezing than frazil ice where the crystals have coagulated to form a soupy layer on the surface. Grease ice reflects little light, giving the water a matte appearance.
- Grey Ice
Young ice 10-15 cm thick, less elastic than nilas and breaks on swell. It usually rafts under pressure.
- Grey-White Ice
Young ice 15-30 cm thick. Under pressure it is more likely to ridge than to raft.
- Grounded Hummock
A hummocked, grounded ice formation. There are single grounded hummocks and lines (or chains) of grounded hummocks.
- Grounded Ice
Floating ice which is aground in shoal water.
Piece of ice smaller than a bergy bit and floating less than 1 m above the sea surface, a growler generally appears white but sometimes transparent or blue-green in colour. Extending less than 1 m above the sea surface and normally occupying an area of about 20 m2., growlers are difficult to distinguish when surrounded by sea ice or in high sea state.
- Hostile Ice
An ice canopy containing no large skylights or other features which permit a submarine to surface.
A hillock of broken ice which has been forced upwards by pressure. May be fresh or weathered. The submerged volume of broken ice under the hummock, forced downwards by pressure, is termed a bummock.
- Hummocked Ice
Ice piled haphazardly one piece over another to form an uneven surface. When weathered it has the appearance of smooth hillocks.
Pressure process by which ice is forced into hummocks. When the floes rotate in the process it is termed screwing.
- Ice Blink
A whitish glare on low clouds above an accumulation of distant ice.
- Ice Boom
A temporary structure constructed to encourage the formation of an ice cover outside the main shipping channel.
- Ice Boundary
The demarcation at any given time between fast ice and floating ice or between areas of ice of different concentrations, types and/or floe sizes.
- Ice Breccia
Ice pieces of different stages of development frozen together.
- Ice Cake
Any relatively flat piece of ice less than 20 m across.
- Ice Canopy
Ice from the point of view of the submariner.
- Ice Climatology
Long-term view of ice conditions observations and measurements over a given geographic water region.
- Ice Concentration
The ratio expressed in tenths describing the area of the water surface covered by ice as a fraction of the whole area.
- Ice Cover
The ratio of an area of ice to the total area of water surface within some large geographic locality. This locality may be global, hemispheric or prescribed by a specific oceanographic entity such as Baffin Bay or the Barents Sea.
- Ice Edge
The demarcation at any given time between open water and sea, lake or river ice whether fast or drifting.
- Ice Field
Area of floating ice, consisting of any size of floes and greater than 10 km across.
- Ice Free
No ice present. If ice of any kind is present, this term shall not be used.
- Ice Front
The vertical cliff forming the seaward face of an ice shelf or other floating glacier, varying in height from 2 to 50 m or more above sea level.
- Ice Island
A large piece of floating ice protruding about 5 m above sea level, which has broken away from an Arctic ice shelf. They have a thickness of 30-50 m and an area of from a few thousand square metres to 500 km2 or more. They are usually characterized by a regularly undulating surface giving a ribbed appearance from the air.
- Ice Island Fragment
Piece of an ice island that has broken away from the main mass.
- Ice Jam
An accumulation of broken river ice or sea ice not moving due to some physical restriction and resisting to pressure.
- Ice Keel
A downward-projecting ridge on the underside of the ice canopy; the submerged counterpart of a ridge. Ice keels may extend as much as 50 m below the surface.
- Ice Limit
Climatological term referring to the extreme minimum or extreme maximum extent of the ice edge in any given month or period based on observations over a number of years. This term should be preceded by minimum or maximum.
- Ice Massif
A variable accumulation of pack or very close pack, covering hundreds of square kilometres and found in the same region every summer.
- Ice of Land Origin
Ice formed on land or in an ice shelf, found floating in water.
- Ice Patch
An area of ice less than 10 km across.
- Ice Rind
A brittle, shiny crust of ice formed on a quiet surface by direct freezing or from grease ice, usually in water of low salinity. It has a thickness of about 5 cm. Easily broken by wind or swell, commonly breaking into rectangular pieces.
- Ice Shelf
A floating ice sheet of considerable thickness showing 2 m or more above sea level, attached to the coast. They usually have great horizontal extent and a level or gently undulating surface. Ice shelf growth occurs by annual snow accumulation and also by the seaward extension of land glaciers. Limited areas may be aground. The seaward edge is termed an ice front.
- Ice Stream
Part of an inland ice sheet in which the ice flows more rapidly and not necessarily in the same direction as the surrounding ice. Margins are sometimes clearly marked by a change in direction of the surface slope but may be indistinct.
- Ice Under Pressure
Ice in which deformation processes are actively occurring. It is a potential impediment or danger to shipping.
- Ice Wall
An ice cliff forming the seaward margin of a glacier which is aground. The rock basement being at or below sea level (see “ice front”, below). The term also includes the seaward face of non-active glaciers.
A massive piece of ice of greatly varying shape, protruding 5 m or more above sea level, which has broken away from a glacier and which may be afloat or aground. They may be described as tabular, domed, pinnacled, wedged, drydocked or blocky. Sizes of icebergs are classed as small, medium, large and very large.
- Iceberg Limit
The limit at any given time between ice of land origin and the open sea or sea ice.
- Iceberg Tongue
A major accumulation of icebergs projecting from the coast, held in place by grounding and joined together by fast ice.
A harbour, inlet, etc., is said to be ice-bound when navigation by ships is prevented, on account of ice, except possibly with the assistance of an icebreaker.
A narrow fringe of ice attached to the coast, unmoved by tides and remaining after the fast ice has moved away.
An embayment in ice, often of a temporary nature, where ships can moor alongside and unload directly onto the ice itself.
- Jammed Brash Barrier
A strip or narrow belt of new, young or brash ice usually 100-5000 m across formed at the edge of either floating or fast ice or at the shore. Heavily compacted, mostly due to wind action, may extend 2 to 20 m below the surface, but does not normally have appreciable topography. Jammed brash barriers may disperse with changing winds, but can also consolidate to form a strip of unusually thick ice in comparison to the surrounding ice.
- Lake Ice
Ice formed on a lake, regardless of observed locations.
- Large Ice Field
An ice field over 20 km across.
- Large Iceberg
A piece of glacier ice extending 46 to 75 m above sea level and with a length of 121 to 200 m.
Any fracture or passageway through ice which is navigable by surface vessels.
- Level Ice
Ice unaffected by deformation.
- Light Nilas
Nilas which is more than 5 cm in thickness and lighter in colour than dark nilas.
- Limit of all known Ice
The limit at any given time between icebergs and/or sea-ice infested waters and ice-free waters.
- Maximum Iceberg Limit
Maximum limit of icebergs based on observations over a period of years.
- Mean Ice Edge
Average position of the ice edge in any given month or period based on observations over a number of years. Other terms which may be used are mean maximum ice edge and mean minimum ice edge.
- Mean Iceberg Limit
Average position of the limit of icebergs at any given time based on observations over a number of years.
Designating the middle number in a series containing an odd number of items.
Designating the number midway between the two middle numbers (the average) in a series containing an even number of items.
- Median Ice Edge
The position of the ice edge where its frequency of occurrence is fifty percent.
- Median Iceberg Limit
The position where the historical or statistical frequency of occurrence of the iceberg limit is fifty percent.
- Medium First-year Ice
70-120 cm thick.
- Medium Ice Field
An ice field 15-20 km across.
- Medium Iceberg
A piece of glacier ice extending 16 to 45 m above sea level and with a length of 61 to 120 m.
- Medium Lake Ice
15-30 cm thick.
- Minimum Iceberg Limit
Minimum limit of icebergs based on observations over a period of years.
- Multi-year Ice
Old ice which has survived at least two summer’s melt. Hummocks are smoother than on second-year ice and the ice is almost salt-free. Where bare, this ice is usually blue in colour. The melt pattern consists of large interconnecting, irregular puddles and a welldeveloped drainage system.
- New Ice
A general term for recently formed ice which includes frazil ice, grease ice, slush and shuga. These types of ice are composed of ice crystals which are only weakly frozen together (if at all) and have a definite form only while they are afloat.
- New Lake Ice
Recently formed ice less than 5 cm thick.
- New Ridge
Ridge with sharp peaks and slope of sides usually 40 degrees or more. Fragments are visible from the air at low altitude.
A thin elastic crust of ice, easily bending on waves and swell and under pressure growing in a pattern of interlocking “fingers” (finger rafting). Nilas has a matte surface and is up to 10 cm in thickness and may be subdivided into dark nilas and light nilas.
Ice is said to nip when it forcibly presses against a ship. A vessel so caught, though undamaged, is said to have been nipped.
A normal is the long-term average value of a climate element, a particular ice attribute (e.g. ice concentration or predominant ice type) for a certain area averaged over a 30 year period.
- Old Ice
Sea ice which has survived at least one summer’s melt. Topographic features generally are smoother than first-year ice. It maybe subdivided into second-year ice and multiyear ice.
- Open Drift
Floating ice in which the concentration is 4/10 to 6/10, with many leads and polynyas. Floes generally not in contact with one another.
- Open Water
A large area of freely navigable water in which ice is present in concentrations less than 1/10. No ice of land origin is present.
- Pancake Ice
Predominantly circular pieces of ice 30 cm to 3 m in diameter, up to 10 cm in thickness, with raised rims due to the pieces striking against one another. It may form on a slight swell from grease ice, shuga or slush or as a result of the breaking of ice rind, nilas or, under severe conditions of swell or waves, of grey ice. It also sometimes forms at some depth at an interface between water bodies of different physical characteristics where it floats to the surface. It may rapidly form over wide areas of water.
- Partial Ice Concentration
Partial ice concentration refers to the amount of a particular stage or of a particular form of ice and represents only a part of the total.
- Pinnacled Iceberg
An iceberg with a central spire or pyramid, with one or more spires.
Any non-linear shaped opening enclosed by ice. May contain brash ice and/or be covered with new ice, nilas or young ice; submariners refer to these as skylights.
- Predominant ice type
Ice type in the greatest concentration within a given area.
An accumulation of water on ice, mainly due to melting snow, but in the more advanced stages also to the melting of ice.
- Rafted Ice
Type of deformed ice formed by one piece of ice overriding another.
Pressure process whereby one piece of ice overrides another. Most common in new and young ice.
An underwater ice projection from an ice wall, ice front, iceberg or floe. Its formation is usually due to a more intensive melting and erosion of the unsubmerged part.
- Recurring Polynya
A polynya which recurs in the same position every year.
Resonance causes an object to move back and forth or up and down.
- Ridge (Ice)
A line or wall of broken ice forced up by pressure. It may be fresh or weathered. The submerged volume of broken ice under a ridge, forced downwards by pressure, is termed an ice keel.
- Ridged Ice
Ice piled haphazardly one piece over another in the form of ridges or walls. Usually found in first-year ice.
- Ridged Ice Zone
An area of many ridges with similar characteristics (rubble field).
The pressure process by which ice is forced into ridges.
- River Ice
Ice formed on a river, regardless of observed location.
- Rotten Ice
Ice which has become honeycombed and is in an advanced state of disintegration.
Sharp, irregular ridges formed on a snow surface by wind erosion and deposition. On mobile floating ice the ridges are parallel to the direction of the prevailing wind at the time they were formed.
- Sea Ice
Any form of ice found at sea which has originated from the freezing of water.
- Second-year Ice
Old ice which has survived only one summer’s melt. Thicker than first-year ice, it stands higher out of the water. In contrast to multi-year ice, summer melting produces a regular pattern of numerous small puddles. Bare patches and puddles are usually greenish-blue.
An area of floating ice is subject to shear when the ice motion varies significantly in the direction normal to the motion, subjecting the ice to rotational forces. These forces may result in phenomena similar to a flaw.
- Shore Lead
A lead between ice and the shore or between ice and an ice front.
- Shore Polynya
A polynya between ice and the coast or between ice and an ice front.
An accumulation of spongy white ice lumps having a diameter of a few centimeters across; they are formed from grease ice or slush and sometimes from anchor ice rising to the surface.
Thin places in the ice canopy, usually less than 1 m thick and appearing from below as relatively light, translucent patches in dark surroundings. The undersurface is normally flat. Skylights are termed large if big enough for a submarine to attempt to surface through them (120 m) or small if not.
Snow which is saturated and mixed with water on land or ice surfaces or as a viscous floating mass in water after a heavy snowfall.
- Small Ice Cake
An ice cake less than 2 m across.
- Small Ice Field
An ice field 10-15 km across.
- Small Iceberg
A piece of glacier ice extending 5 to 15 m above sea level and with a length of 15 to 60 m.
- Snow-Covered Ice
Ice covered with snow.
An accumulation of wind-blown snow deposited in the lee of obstructions or heaped by wind eddies. A crescent-shaped snowdrift, with ends pointing down-wind, is called a snow barchan.
- Stages of Development of Lake Ice
- New Lake Ice
- Thin Lake Ice
- Medium Lake Ice
- Thick Lake Ice
- Very Thick Lake Ice
- Stages of Development of Sea Ice
- New Ice
- Young Ice
- First-year Ice
- Old Ice
- Stages of Melting
- Thaw Holes
- Dried Ice
- Rotten Ice
- Flooded Ice
- Standing Floe
A separate floe standing vertically or inclined and enclosed by rather smooth ice.
- Stranded Ice
Ice which had been floating and has been deposited on the shore by retreating high water.
Long narrow area of pack/drift ice, about 1 km or less in width, usually composed of small fragments detached from the main mass of ice, which run together under the influence of wind, swell or current.
- Tabular Iceberg
A flat-topped iceberg. Most show horizontal banding.
- Thaw Holes
Vertical holes in ice formed when surface puddles melt through to the underlying water.
- Thick First-year Ice
Greater than 120 cm thick.
- Thick Lake Ice
30-70 cm thick.
- Thin First-year Ice/White Ice - First Stage
30-50 cm thick.
- Thin First-year Ice/White Ice - Second Stage
50-70 cm thick.
- Thin Lake Ice
5-15 cm thick.
- Tide Crack
Crack at the line of junction between an immovable ice foot or ice wall and fast ice, the latter subject to rise and fall of the tide.
A projection of the ice edge up to several kilometres in length, caused by wind or current.
- Total Ice Concentration
Total ice concentration includes all stages of development that are present.
- Very Close Pack/Drift
Floating ice in which the concentration is 9/10 to less than 10/10.
- Very Large Iceberg
A piece of glacier ice extending more than 75 m above sea level and with a length of more than 200 m.
- Very Open Drift
Ice in which the concentration is 1/10 to 3/10 and water dominates over ice.
- Very Thick Lake Ice
Greater than 70 cm thick.
- Very Weathered Ridge
Ridge with tops very rounded. Slope of sides usually 20 to 30 degrees.
- Water Sky
Dark streaks on the underside of low clouds, indicating the presence of water features in the vicinity of ice.
- Weathered Ridge
Ridge with peaks slightly rounded and slope of sides usually 30 to 40 degrees. Individual fragments are not discernible.
Processes of ablation and accumulation which gradually eliminate irregularities in an ice surface.
- Wedged Iceberg
An iceberg which is rather flat on top and with steep vertical sides on one end, sloping to lesser sides on the other end.
- Young Coastal Ice
The initial stage of fast ice formation consisting of nilas or young ice; its width varying from a few metres up to 100-200 m from the shoreline.
- 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.
- Date modified: