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Anchor ice is defined by theWorld Meteorological Organization as "submerged ice attached or anchored to the bottom, irrespective of the nature of its formation".[1] It may also be calledbottom-fast ice.[2] Anchor ice is most commonly observed in fast-flowing rivers during periods of extreme cold, at the mouths of rivers flowing into very cold seawater, in the shallowsub orintertidal during or after storms when the air temperature is below thefreezing point of the water, and thesubtidal in theAntarctic alongice shelves or near floatingglacier tongues, and in shallow lakes.[3]
Anchor ice will generally form in fast-flowing rivers during periods of extreme cold. Due to the motion of the water, ice cover may not form consistently, and the water will quickly reach itsfreezing point due to mixing and contact with the atmosphere.Ice platelets generally form very quickly in the water column and on submerged objects once conditions are optimal for anchor ice formation. Anchor ice in rivers tends to be composed of numerous small crystals adhering to each other in small flocculent masses. Anchor ice in rivers can seriously disrupthydro-electric power plants by significantly reducing flow or stopping turbines completely.
Another form of anchor ice may be observed at the mouths ofArctic rivers where fresh water seeps out of the river bed into the ocean up through the sediment. Anchor ice forms if the seawater is below thefreezing point of the river water.
Shallowtundra lakes may feature anchor ice with a specific behavior.[2] Lakes in the southwestern part ofNunavut, Canada typically freeze down to the bottom when the water level is low. On some cases spring meltwater flows into the lake under the ice cover, which becomes domed leaving a depressed "racetrack" ring around the shore where meltwater accumulates as well. The ice cover remains bottom-fast until the buoyancy force exceeds the freezing bond. At the latter moment the ice cover abruptly breaks off the bottom to form a flat sheet.[2] In other cases the anchor ice becomes completely submerged into the meltwater and holes may be melted throughout the ice sheet. When the sheet finally lifts off the bottom, the meltwater accumulated at the surface is jetted through these holes with enough force to create small craters in the lake bottom where it is soft (sand or silt). This downward jet phenomenon was previously described for deltas into theBeaufort Sea, where they were caused by periodic tidal buoyancy of holed ice.[4]
Anchor ice may be formed in the shallowintertidal orsubtidal during storms in cold weather, when the uppermost layers of the water column are churned up by strong winds or waves. This type of anchor ice can be found primarily in theArctic, where submerged ice may be observed to completely cover the substrate to depths of up to 2m, with some anchor ice cover observed at more than 4.5m depth.
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Antarctic anchor ice is perhaps one of the most interesting phenomena of ice formation in the marine environment. The general mechanism of its formation is commonly assumed as the following:
Anchor ice crystals in the Antarctic are generally in the form of thin, circular platelets of 2–10 cm in diameter. Large masses of irregularly-oriented crystals form anchor ice formations, which may be as large as 4m in diameter when attached to large immovable objects on the sea floor.
Anchor ice that forms on the underside of sea ice is often referred to asplatelet orcongelation ice, and can be hard to distinguish from that formed due to the cooling of the sea ice cover by cold atmospheric conditions.
Anchor ice is thought to be relatively common in the Antarctic, due to largeice shelves that occupy many areas of the continental coast. Studies and observations of anchor ice formation inMcMurdo Sound,Antarctica have shown that the phenomenon regularly causes the formation of ice on the seafloor to depths of approximately 15m, and rarely to depths of approximately 30m.
Especially in theAntarctic, anchor ice has been implicated in drastic zonation of thesubtidalfauna. Many animals are directly affected by the growth of anchor ice, and certainsponges have been shown to readily grow anchor ice and to be damaged by it. Anchor ice may also grow on animate or inanimate objects and lift them from the sea floor. In theAntarctic this will most likely result in the death of an organism, since during much of the year the ocean is covered by annual sea ice, and the organism is likely to become incorporated into this.
Many organisms have actually been found on the surface ofice shelves in certain places in theAntarctic, likely due to the anchor icing phenomenon:[5]
