Ice calving

A mass of ice calves from the Perito Moreno glacier in Lago Argentino

Ice calving, also known as glacier calving or iceberg calving, is the breaking of ice chunks from the edge of a glacier.[1] It is a form of ice ablation or ice disruption. It is the sudden release and breaking away of a mass of ice from a glacier, iceberg, ice front, ice shelf, or crevasse. The ice that breaks away can be classified as an iceberg, but may also be a growler, bergy bit, or a crevasse wall breakaway.[2]

Calving of glaciers is often accompanied by a loud cracking or booming sound[3] before blocks of ice up to 60 metres (200 ft) high break loose and crash into the water. The entry of the ice into the water causes large, and often hazardous waves.[4] The waves formed in locations like Johns Hopkins Glacier can be so large that boats cannot approach closer than three kilometres (1+1⁄2 nautical miles). These events have become major tourist attractions in locations such as Alaska.

Many glaciers terminate at oceans or freshwater lakes which results naturally[5] with the calving of large numbers of icebergs. Calving of Greenland's glaciers produce 12,000 to 15,000 icebergs each year alone.[6]

Calving of ice shelves is often preceded by a rift.[7] An ice shelf in steady state calves at roughly the same rate as the influx of new ice,[8][9] and calving events may occur on sub-annual to decadal timescales to maintain an overall average mean position of the ice shelf front. When calving rates exceed the influx of new ice, ice front retreat occurs, and ice shelves may grow smaller and weaker.[10]

  1. ^ Essentials of Geology, 3rd edition, Stephen Marshak
  2. ^ Glossary of Glacier Terms, Ellin Beltz, 2006. Retrieved July 2009.
  3. ^ Glacier Bay, National Park Service. Retrieved July 2009.
  4. ^ Glacier Calving photos Archived 2010-01-25 at the Wayback Machine. Retrieved July 2009.
  5. ^ ARCTIC, Vol. 39, No. 1 (March 1986) P. 15-19, Ice Island Calvings and Ice Shelf Changes, Milne Ice Shelf and Ayles Ice Shelf, Ellesmere Island, N.W.T. Archived 2019-09-28 at the Wayback Machine, Martin O. Jeffries, 1985, University of Calgary. Retrieved 18 July 2009.
  6. ^ Oceans, Oxfam. Retrieved June 2009.
  7. ^ Promotions/Public Relations (2006-12-08). "The loose tooth: rifting and calving of the Amery Ice Shelf - Australian Antarctic Division". Aad.gov.au. Archived from the original on October 2, 2009. Retrieved 2010-07-30.
  8. ^ Rignot, E.; Jacobs, S.; Mouginot, J.; Scheuchl, B. (19 July 2013). "Ice-Shelf Melting Around Antarctica". Science. 341 (6143): 266–270. doi:10.1126/science.1235798. PMID 23765278. S2CID 206548095.
  9. ^ Depoorter, M. A.; Bamber, J. L.; Griggs, J. A.; Lenaerts, J. T. M.; Ligtenberg, S. R. M.; van den Broeke, M. R.; Moholdt, G. (3 October 2013). "Calving fluxes and basal melt rates of Antarctic ice shelves". Nature. 502 (7469): 89–92. doi:10.1038/nature12567. PMID 24037377. S2CID 4462940.
  10. ^ Greene, Chad A.; Gardner, Alex S.; Schlegel, Nicole-Jeanne; Fraser, Alexander D. (10 August 2022). "Antarctic calving loss rivals ice-shelf thinning". Nature. 609 (7929): 948–953. Bibcode:2022Natur.609..948G. doi:10.1038/s41586-022-05037-w. PMID 35948639. S2CID 251495070.