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Ice floe

An ice floe is a segment of floating ice defined as a flat piece at least 20 metres (66 ft) across at its widest point, and up to more than 10 kilometres across. Drift ice is a floating field of sea ice composed of several ice floes. They may cause ice jams on freshwater rivers, and in the open ocean may damage the hulls of ships.

Modelling
The modelling of sea-ice floes has received increasing attention in recent years, as floe size distribution influences heat and momentum fluxes in the marginal ice zone (MIZ). Most observations of sea-ice floe properties are obtained from satellite imagery, which allows the extraction of floe size distributions over large spatial scales. In addition to optical and radar satellite observations, floe characteristics can also be inferred from altimeter measurements. ==Gallery==
Gallery
File:Drift ice in Hudson Strait, 2014.jpg|Several ice floes in the Hudson Strait File:IceNomenclature-2LightPack.jpg|Ice floes in the Weddell Sea File:In the Arctic Sea - An Ice Floe Adrift (NBY 439626).jpg|"In the Arctic Sea – An Ice Floe Adrift". Postcard, Albert Operti, early 20th century ==References==
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