Ice shove
Appearance
An ice shove, ice surge, ice heave, ivu,[1] or shoreline ice pileup is a surge of ice from an ocean or large lake onto the shore.[2] Ice shoves are caused by ocean currents, strong winds, or temperature differences pushing ice onto the shore,[3] creating piles up to 12 metres (40 feet) high. Some have described them as 'ice tsunamis',[4] but the phenomenon works like an iceberg.[5] Witnesses have described the shove's sound as being like that of a train or thunder.[2][6][7][4] Ice shoves can damage buildings and plants that are near to the body of water.[2][4][6][7][8] Arctic communities can be affected by ice shoves.[9]
See also
External links
References
- ^ Mason, Owen; Neal, William J.; Pilkey, Orrin H.; Bullock, Jane; Fathauer, Ted; Pilkey, Deborah F.; Swanston, Douglas (1997). "Wind, Ice, and Sea" (cloth). Living with the coast of Alaska. Living with the Shore. Durham, NC: Duke University Press. p. 93. ISBN 978-0-8223-2009-8. Retrieved 12 December 2013. – also paperback (ISBN 978-0-8223-2019-7)
- ^ a b c Doran, Chad. "Ice shoves cause damage on Lake Winnebago shoreline". WLUK-TV. Archived from the original on January 26, 2013. Retrieved January 21, 2013.
- ^ "Glossary for the letter i". National Oceanic and Atmospheric Administration. Retrieved January 21, 2013.
- ^ a b c All Things Considered (2013-04-24). "'Ice Shove' Damages Some Manitoba Homes Beyond Repair". NPR. Retrieved 2013-05-15.
- ^ "'Ice tsunamis' sweep into homes". CNN.com. Retrieved 2013-05-15.
- ^ a b "Winds whip up worry in Manitoba community hit by ice wall". CBC News. May 13, 2013. Retrieved 2013-05-15.
- ^ a b "Wall of ice destroys Manitoba homes, cottages". CBC News. May 11, 2013. Retrieved 2013-05-15.
- ^ "Ice Tsunami..Glacier like ice moving across Mille Lacs lake, damaging houses, Minnesota". Retrieved 2014-09-08.
- ^ Mahoney, Andrew; Eicken, Hajo; Shapiro, Lewis; Grenfell, Tom C. (2004-03-01). "Ice motion and driving forces during a spring ice shove on the Alaskan Chukchi coast". Journal of Glaciology. 50 (169): 195–207. doi:10.3189/172756504781830141.