Sea ice driven iceberg drift in Baffin Bay.
Simulations carried out with NEMO at 1/4 degree resolution over the Arctic and Northern Hemisphere Atlantic (ANHA) domain. SIL differs from CTL only in the parameterization of the sea ice force over icebergs; for CTL it is simply a drag force, in SIL sea ice above 90% concentration is capable of locking icebergs.
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Zipped SIL and CTL folders.
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Field label
Study/Dataset Example
Format
inconnu
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Datastore contains all records of source file
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Has views
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Id
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Package id
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State
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