The circulation of deep water in the Tasman and Coral Seas

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dc.contributor.authorHarries, JRen_AU
dc.date.accessioned2007-11-22T04:26:08Zen_AU
dc.date.accessioned2010-04-30T04:37:20Zen_AU
dc.date.available2007-11-22T04:26:08Zen_AU
dc.date.available2010-04-30T04:37:20Zen_AU
dc.date.issued1976-07en_AU
dc.description.abstractThe physical oceanography of the Tasman and Coral Seas is reviewed with an emphasis on the deep currents. There are many uncertainties in the deep circulation pattern. The available data are used to develop an idealised circulation to estimate the likely path taken by water flowing from a depth of 5000 m in the Tasman Sea. The model suggests that the water would finally reach the surface layers south of the Antarctic Convergence with a median delay of 600 years.en_AU
dc.identifier.citationMarine disposalen_AU
dc.identifier.citationHarries, J. R. (1976). The circulation of deep water in the Tasman and Coral Seas (AAEC/E390). Lucas Heights, NSW: Australian Atomic Energy Commission.en_AU
dc.identifier.govdoc609en_AU
dc.identifier.isbn0642997527en_AU
dc.identifier.otherAAEC-E-390en_AU
dc.identifier.placeofpublicationLucas Heights, New South Walesen_AU
dc.identifier.urihttp://apo.ansto.gov.au/dspace/handle/10238/599en_AU
dc.language.isoen_auen_AU
dc.publisherAustralian Atomic Energy Commissionen_AU
dc.subjectLiquid flowen_AU
dc.subjectPacific Oceanen_AU
dc.subjectRadionuclide migrationen_AU
dc.subjectContaminationen_AU
dc.subjectSeawateren_AU
dc.titleThe circulation of deep water in the Tasman and Coral Seasen_AU
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