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This article documents a current event. Information may change rapidly as the event progresses.

An ice shelf is a thick, floating platform of ice that forms where a glacier or ice sheet flows down to a coastline and onto the ocean surface. Ice shelves are found in Antarctica, Greenland and Canada only. The boundary between the floating ice shelf and the grounded (resting on bedrock) ice that feeds it is called the grounding line. When the grounding line retreats inland, water is added to the ocean and sea level rises.

In contrast, sea ice is formed on water, is much thinner, and forms throughout the Arctic Ocean. It also is found in the Southern Ocean around the continent of Antarctica.

Ice shelves flow by gravity-driven horizontal spreading on the ocean surface. That flow continually moves ice from the grounding line to the seaward front of the shelf. The primary mechanism of mass loss from ice shelves is iceberg calving, in which a chunk of ice breaks off from the seaward front of the shelf. Typically, a shelf front will extend forward for years or decades between major calving events. Snow accumulation on the upper surface and melting from the lower surface are also important to the mass balance of an ice shelf.

The thickness of modern-day ice shelves ranges from about 100 to 1000 meters. The density contrast between solid ice and liquid water means that only about 1/9 of the floating ice is above the ocean surface. The world's largest ice shelves are the Ross Ice Shelf and the Filchner-Ronne Ice Shelf in Antarctica.

Contents 1 Canadian ice shelves 2 Antarctic ice shelves 3 Ice shelf disruption 4 References 5 See also 6 External links

All Canadian ice shelves are attached to Ellesmere Island and lie north of 82°N:

• Alfred Ernest Ice Shelf
• Ayles Ice Shelf (broke up in 2005)
• M'Clintock Ice Shelf
• Markham Ice Shelf
• Milne Ice Shelf
• Ward Hunt Ice Shelf

44 percent of the Antarctic coastline has ice shelves attached. The individual ice shelf areas are listed below, in a clockwise manner, starting in the west of Eastern Antarctica:

• Abbot Ice Shelf
• Amery Ice Shelf
• Bach Ice Shelf
• Brunt Ice Shelf
• Cook Ice Shelf
• Cosgrove Ice Shelf
• Crosson Ice Shelf
• Dotson Ice Shelf
• Edward VIII Ice Shelf
• Ekstrom Ice Shelf
• Filchner Ice Shelf
• Fimbul Ice Shelf
• George VI Ice Shelf
• Getz Ice Shelf
• Gillett Ice Shelf
• Hannan Ice Shelf
• Jelbart Ice Shelf
• Jones Ice Shelf
• Larsen Ice Shelf
• Lazarev Ice Shelf
• McMurdo Ice Shelf
• Moscow University Ice Shelf
• Müller Ice Shelf
• Nansen Ice Sheet
• Nickerson Ice Shelf
• Prince Gustav Ice Shelf
• Publications Ice Shelf
• Quar Ice Shelf
• Riiser-Larsen Ice Shelf
• Ronne Ice Shelf
• Ross Ice Shelf
• Shackleton Ice Shelf
• Slava Ice Shelf
• Stange Ice Shelf
• Sulzberger Ice Shelf
• Swinburne Ice Shelf
• Venable Ice Shelf
• Voyeykov Ice Shelf
• West Ice Shelf
• Wilkins Ice Shelf
• Wordie Ice Shelf
• Wyers Ice Shelf
• Zubchatyy Ice Shelf

In the last several decades, glaciologists have observed consistent decreases in ice shelf extent through melt, calving, and complete disintegration of some shelves.

The Ellesmere ice shelf reduced by 90 percent in the twentieth century, leaving the separate Alfred Ernest, Ayles, Milne, Ward Hunt, and Markham Ice Shelves. A 1986 survey of Canadian ice shelves found that 48 square km (3.3 cubic kilometers) of ice calved from the Milne and Ayles ice shelves between 1959 and 1974.^[1] The Ayles Ice Shelf calved entirely on August 13, 2005. The Ward Hunt Ice Shelf, the largest remaining section of thick (>10 m) landfast sea ice along the northern coastline of Ellesmere Island, lost 600 square km of ice in a massive calving in 1961-1962.^[2] It further decreased by 27% in thickness (13 m) between 1967 and 1999.^[3] In summer 2002, the Ward Ice Shelf experienced another major breakup. ^[4]

Two sections of Antarctica's Larsen Ice Shelf broke apart into hundreds of unusually small fragments (100's of meters wide or less) in 1995 and 2002.

The breakup events are linked the dramatic polar warming trends that are part of global warming. The leading ideas involve enhanced ice fracturing due to surface meltwater and enhanced bottom melting due to warmer ocean water circulating under the floating ice.

The cold, fresh water produced by melting underneath the Ross and Flichner-Ronne ice shelves is a component of Antarctic Bottom Water.

1. ^ Jeffries, Martin O. Ice Island Calvings and Ice Shelf Changes, Milne Ice Shelf and Ayles Ice Shelf, Ellesmere Island, N.W.T.. Arctic 39 (1) (March 1986)
2. ^ Hattersley-Smith, G. The Ward Hunt Ice Shelf: recent changes of the ice front. Journal of Glaciology 4:415-424. 1963.
3. ^ Vincent, W.F., J.A.E. Gibson, M.O. Jeffries. Ice-shelf collapse, climate change, and habitat loss in the Canadian high Arctic. Polar Record 37 (201): 133-142 (2001)
4. ^ NASA Earth Observatory. Breakup of the Ward Hunt Ice Shelf.

Wikinews

• Wikinews:Ice shelf breaks free in Canadian Arctic

• http://www.antdiv.gov.au/default.asp?casid=1547 - from the Australian Antarctic Division
• http://nsidc.org/iceshelves - from the U.S. National Snow and Ice Data Center
• http://www.cnn.com/2006/TECH/science/12/29/canada.arctic.ap/index.html - CNN story about the Canadian Ayles ice shelf break up in August 2005

• http://ice-glaces.ec.gc.ca/ - from the Canadian Ice Service