Comparison of theoretical and laboratory models of ocean wave transmission by a group of ice floes

Although the floating sea ice surrounding the Antarctic damps ocean waves, they may still be detected hundreds of kilometres from the ice edge. Over this distance the waves leave an imprint of broken ice, which is susceptible to winds, currents, and lateral melting. The important omission of wave-ic...

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Bibliographic Details
Other Authors: AADC (originator), AU/AADC > Australian Antarctic Data Centre, Australia (resourceProvider)
Format: Dataset
Language:unknown
Published: Australian Ocean Data Network
Subjects:
oceans
OCEAN WAVES
EARTH SCIENCE
ICE FLOES
CRYOSPHERE
SEA ICE
LABORATORY
AMD
AMD/AU
CEOS
OCEAN &gt
SOUTHERN OCEAN
GEOGRAPHIC REGION &gt
POLAR
CONTINENT &gt
ANTARCTICA
Antarctic
Southern Ocean
The Antarctic
Antarc*
Antarctica
Sea ice
Online Access:https://researchdata.ands.org.au/comparison-theoretical-laboratory-ice-floes/685584
https://data.aad.gov.au/metadata/records/AAS_4123_model_comparisons
http://data.aad.gov.au/aadc/portal/download_file.cfm?file_id=4297
https://secure3.aad.gov.au/proms/public/projects/report_project_public.cfm?project_no=4123
http://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=AAS_4123_model_comparisons

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