hdl:10013/epic.11203
The occurrence of ice platelets at 250 m depth near the Filchner Ice Shelf and its significance for sea ice biology
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gdieckmann [ at ] awi-bremerhaven.de
Abstract
Large single-crystal ice platelets were collected at 250 m depth in the vicinity of the Filchner Ice Shelf. They were probably formed in supercooled water streaming out from under the ice shelf as supported by hydrographic observations. The significance of large platelets rising from greater depths for the biological processes in sea ice along the Antarctic ice shelves is discussed. © 1986.
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Article
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Divisions
AWI Organizations > Biosciences > Polar Biological Oceanography
AWI Organizations > Climate Sciences > Physical Oceanography of the Polar Seas
AWI Organizations > Climate Sciences > Climate Dynamics
AWI Organizations > Climate Sciences > Sea Ice Physics
AWI Organizations > Climate Sciences > Physical Oceanography of the Polar Seas
AWI Organizations > Climate Sciences > Climate Dynamics
AWI Organizations > Climate Sciences > Sea Ice Physics
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Publication Status
Published
Eprint ID
616
DOI
https://www.doi.org/10.1016/0198-0149(86)90114-7
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Cite as
Dieckmann, G.
,
Rohardt, G.
,
Hellmer, H.
and
Kipfstuhl, J.
(1986):
The occurrence of ice platelets at 250 m depth near the Filchner Ice Shelf and its significance for sea ice biology
,
Deep Sea Research Part A. Oceanographic Research Papers,
33
(2),
pp. 141-148
.
doi: https://www.doi.org/10.1016/0198-0149(86)90114-7
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