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Ice Forms: What You Should Know

Sea ice is also called sea ice, ocean ice, polar ice, and atmospheric ice. Sea ice is formed when water from the Arctic Ocean has no access to the Pacific Ocean or tropics due to a strong wind or currents causing the water to move north. As it warms, it creates a layer of ocean ice or crosshair along the north-east coast of Greenland and north-west coast of Canada. At this point, the water is still below freezing and the ice that forms is called sea ice. Sea ice extends in great distances and can remain present during the winter months up to three months. When the sea ice starts to melt, it is often called sea ice retreat. Sea ice retreat can be caused by rising sea levels, changing winds, or ocean currents.  Icebergs — Wikipedia Icebergs are large bodies of water formed from seawater that have been broken by rising waters. The breaking of marine ice in the open sea creates open water on the sea floor and the resulting calving of icebergs may occur at any time in the year.   Icebergs are formed when high waves pushed against the floating ice shelves.  Most ice in the Arctic Ocean is composed of the sea ice and glacial ice and is referred to as the North Atlantic Ice Sheet ; but Greenland's ice can also be referred to as ice landmass because it is situated in this area.  The Antarctic Ice Sheet is ice landmass. Icebergs are the main cause of icebergs in the sea because of their massive volume, size, and stability. They do not break easily and form a dangerous threat to shipping. Icebergs also present a threat when ice sheets in Greenland or Antarctica are melting due to rising air temperatures and water temperatures.  When icebergs are larger than 4,000 sq km (2,000 sq mi), marine traffic is particularly affected and shipping from all ports in the world could affect. Icebergs can break into pieces (called icebergs) or break in two (delta, or multiple). Multiple icebergs may be a warning of an imminent danger.  Icebergs are visible from space and can be seen from the coast, but they can take a long time to become visible. Icebergs in the ocean can become frozen by freezing water around them when they are pushed by currents. They can become ice dams which protect coastal areas and slow down the flow of water.

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