Publication Date:
1998-05-22
Description:
The migration and evolution of a deep ocean hydrothermal event plume were tracked with a neutrally buoyant RAFOS float. The float remained entrained in the plume for 60 days, and the plume vorticity was calculated directly from the anticyclonic motion of the float. Concentrations of suspended particles, particulate iron, and dissolved manganese in the plume did not decay significantly during the 60 days, which indicates that event plumes would be easily detectable a year after formation.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Lupton -- Baker -- Garfield -- Massoth -- Feely -- Cowen -- Greene -- Rago -- New York, N.Y. -- Science. 1998 May 15;280(5366):1052-5.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉J. E. Lupton and R. R. Greene, Pacific Marine Environmental Laboratory, National Oceanic and Atmospheric Administration (NOAA), Newport, OR 97365, USA. E. T. Baker, G. J. Massoth, R. A. Feely, Pacific Marine Environmental Laboratory, NOAA〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/9582113" target="_blank"〉PubMed〈/a〉
Print ISSN:
0036-8075
Electronic ISSN:
1095-9203
Topics:
Biology
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Chemistry and Pharmacology
,
Computer Science
,
Medicine
,
Natural Sciences in General
,
Physics
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