Sea ice is frozen seawater. Because ice is less dense than its melt, sea ice floats. Sea ice covers about 7% of the Earth’s surface, or about 12% of the world’s oceans. In the North, it is found in the Arctic Ocean, in areas just below it and in other cold oceans, seas and gulfs; in the Antarctic, it occurs in various areas around Antarctica (the continent). Due to the combined action of winds, currents and air temperature fluctuations, sea ice expanses are very dynamic. In the fall and winter, the ice grows progressively thicker, defining floes of various sizes that collide against each other. This activity also goes on in the spring and summer, but during that time part of the ice melts. This ice may be contrasted with icebergs, which are chunks of ice shelves or glaciers that calve into the ocean. Unlike sea ice, which is saline, icebergs are made from fresh water. They may be enclosed within sea ice expanses and drift along with it.
Read more about Sea Ice: Types of Sea Ice, Formation of Sea Ice, Yearly Freeze and Melt Cycle, Monitoring and Observations, Modelling, Ecology, Relationship To Global Warming and Climate Change
Famous quotes containing the words sea and/or ice:
“Another success is the post-office, with its educating energy augmented by cheapness and guarded by a certain religious sentiment in mankind; so that the power of a wafer or a drop of wax or gluten to guard a letter, as it flies over sea over land and comes to its address as if a battalion of artillery brought it, I look upon as a fine meter of civilization.”
—Ralph Waldo Emerson (1803–1882)
“Suddenly I saw the cold and rook-delighting heaven
That seemed as though ice burned and was but the more ice,”
—William Butler Yeats (1865–1939)