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001        FI15062161_00001
005        20150731110327.0
006        m^^^^^o^^d^^^^^^^^
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245 00 |a The Antarctic Peninsula's retreating ice shelves |h [electronic resource].
260        |a [S.l.] : |b British Antarctic Survey, |c 2012.
506        |a Please contact the owning institution for licensing and permissions. It is the user's responsibility to ensure use does not violate any third party rights.
520 3    |a Ice shelves are the floating extensions of a grounded ice sheet. Although a few small ice shelves exist in the Arctic, most occupy bays around the coast of Antarctica. They were once thought to be permanent features of the Antarctic landscape. The largest ice shelf, the Ronne-Filchner, covers an area slightly smaller than Spain. Over many decades, ice shelves find their natural size when the amount of snow falling on the surface, and the amount ice delivered by glaciers, balances the rate of ice loss through melting and iceberg calving. A change in any of these factors will cause an ice shelf to change its size to find a new equilibrium.
533        |a Electronic reproduction. |c Florida International University, |d 2015. |f (dpSobek) |n Mode of access: World Wide Web. |n System requirements: Internet connectivity; Web browser software.
650    0 |a Climate Change.
650    0 |a Ice Shelves.
651    0 |a Antarctica.
710 2    |a British Antarctic Survey.
830    0 |a dpSobek.
830    0 |a Sea Level Rise.
852        |a dpSobek |c Sea Level Rise
856 40 |u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15062161/00001 |y Click here for full text
992 04 |a http://dpanther.fiu.edu/sobek/content/FI/15/06/21/61/00001/FI15062161_thm.jpg
997        |a Sea Level Rise


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