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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Australian Ocean Data Network
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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 |