Arctic Sea Ice and Its Role in Global Change

• Main Authors: Liu, Jiping, Horton, Radley M.
• Format: Other/Unknown Material
• Language: unknown
• Published: 2018
• Subjects: Oceanography; Arctic; Arctic Ocean; Baffin Bay; Bering Sea; Greenland; Hudson; Okhotsk; Antarc*; Antarctica; Baffin; Greenland Sea; okhotsk sea; Sea ice
• Online Access: http://hdl.handle.net/2060/20190025691

Sea ice is an important component of the global climate system. Sea ice forms, grows, and melts in the ocean. Sea ice grows during the fall and winter and melts during the spring and summer. Sea ice can melt completely in summer or survive multiple years. Sea ice can be classified by stages of development (thickness and age), that is, first-year sea ice (ice thickness typically <1.8 m) and multiyear sea ice (ice thickness typically >1.8 m). Sea ice occurs in both hemispheres. In the Northern Hemisphere, sea ice develops in the Arctic Ocean and surrounding bodies including Hudson and Baffin Bay, Gulf of St. Lawrence, the Greenland Sea, the Bering Sea, and the Sea of Okhotsk (sea ice can be observed as far south as Bohai Bay, China, ~38N). In the Southern Hemisphere, sea ice only develops around Antarctica, reaching a maximum equatorward extension at around ~55S).