Mesoscale Oceanographic Processes beneath the Ice of Fram Strait
A major component of the Fram Strait Marginal Ice Zone Experiment was the investigation of air-sea-ice interactions, processes, and circulation patterns found behind the local ice edge and on scales greater than 10 kilometers (mesoscale and large scale). Neutrally buoyant floats, ice-tethered cycles...
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Veröffentlicht in: | Science (American Association for the Advancement of Science) 1987-04, Vol.236 (4800), p.432-434 |
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creator | Manley, T. O. Villanueva, J. Z. Gascard, J. C. Jeannin, P. F. Hunkins, K. L. Van Leer, J. |
description | A major component of the Fram Strait Marginal Ice Zone Experiment was the investigation of air-sea-ice interactions, processes, and circulation patterns found behind the local ice edge and on scales greater than 10 kilometers (mesoscale and large scale). Neutrally buoyant floats, ice-tethered cyclesondes, and helicopter-based measurements were used to obtain uniquely integrated and consistent views of the mesoscale ocean features beneath the ice cover of Fram Strait. Within the vicinity of the Yermak Plateau, three distinct regions of mesoscale motion were observed that coincided with the shallow topography of the plateau, the northward flowing Atlantic water over the western flank of the plateau, and the strong current-shear zone of the East Greenland Polar Front. A subice meander of the front was also observed, which was probably occluded subsequently. |
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O. ; Villanueva, J. Z. ; Gascard, J. C. ; Jeannin, P. F. ; Hunkins, K. L. ; Van Leer, J.</creator><creatorcontrib>Manley, T. O. ; Villanueva, J. Z. ; Gascard, J. C. ; Jeannin, P. F. ; Hunkins, K. L. ; Van Leer, J.</creatorcontrib><description>A major component of the Fram Strait Marginal Ice Zone Experiment was the investigation of air-sea-ice interactions, processes, and circulation patterns found behind the local ice edge and on scales greater than 10 kilometers (mesoscale and large scale). Neutrally buoyant floats, ice-tethered cyclesondes, and helicopter-based measurements were used to obtain uniquely integrated and consistent views of the mesoscale ocean features beneath the ice cover of Fram Strait. Within the vicinity of the Yermak Plateau, three distinct regions of mesoscale motion were observed that coincided with the shallow topography of the plateau, the northward flowing Atlantic water over the western flank of the plateau, and the strong current-shear zone of the East Greenland Polar Front. A subice meander of the front was also observed, which was probably occluded subsequently.</description><identifier>ISSN: 0036-8075</identifier><identifier>EISSN: 1095-9203</identifier><identifier>DOI: 10.1126/science.236.4800.432</identifier><identifier>PMID: 17817128</identifier><identifier>CODEN: SCIEAS</identifier><language>eng</language><publisher>Washington, DC: The American Association for the Advancement of Science</publisher><subject>Analysis ; Arctic ; Buoyancy ; Datasets ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Geology ; Ice ; Marine ; Ocean currents ; Ocean-atmosphere interaction ; Oceanography ; Oceans ; Physics of the oceans ; Saltwater ; Sea ice ; Sea water ; Seas ; Trajectories</subject><ispartof>Science (American Association for the Advancement of Science), 1987-04, Vol.236 (4800), p.432-434</ispartof><rights>Copyright 1987 The American Association for the Advancement of Science</rights><rights>1988 INIST-CNRS</rights><rights>COPYRIGHT 1987 American Association for the Advancement of Science</rights><rights>COPYRIGHT 1987 American Association for the Advancement of Science</rights><rights>Copyright American Association for the Advancement of Science Apr 24, 1987</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c741t-b4cc67015426f8db5571b51e67c21429a60edb8e4ee7bab73274216ebabaf43b3</citedby><cites>FETCH-LOGICAL-c741t-b4cc67015426f8db5571b51e67c21429a60edb8e4ee7bab73274216ebabaf43b3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/1699003$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/1699003$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,776,780,799,2871,2872,27901,27902,57992,58225</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=7395446$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/17817128$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Manley, T. O.</creatorcontrib><creatorcontrib>Villanueva, J. Z.</creatorcontrib><creatorcontrib>Gascard, J. C.</creatorcontrib><creatorcontrib>Jeannin, P. F.</creatorcontrib><creatorcontrib>Hunkins, K. L.</creatorcontrib><creatorcontrib>Van Leer, J.</creatorcontrib><title>Mesoscale Oceanographic Processes beneath the Ice of Fram Strait</title><title>Science (American Association for the Advancement of Science)</title><addtitle>Science</addtitle><description>A major component of the Fram Strait Marginal Ice Zone Experiment was the investigation of air-sea-ice interactions, processes, and circulation patterns found behind the local ice edge and on scales greater than 10 kilometers (mesoscale and large scale). Neutrally buoyant floats, ice-tethered cyclesondes, and helicopter-based measurements were used to obtain uniquely integrated and consistent views of the mesoscale ocean features beneath the ice cover of Fram Strait. Within the vicinity of the Yermak Plateau, three distinct regions of mesoscale motion were observed that coincided with the shallow topography of the plateau, the northward flowing Atlantic water over the western flank of the plateau, and the strong current-shear zone of the East Greenland Polar Front. A subice meander of the front was also observed, which was probably occluded subsequently.</description><subject>Analysis</subject><subject>Arctic</subject><subject>Buoyancy</subject><subject>Datasets</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Geology</subject><subject>Ice</subject><subject>Marine</subject><subject>Ocean currents</subject><subject>Ocean-atmosphere interaction</subject><subject>Oceanography</subject><subject>Oceans</subject><subject>Physics of the oceans</subject><subject>Saltwater</subject><subject>Sea ice</subject><subject>Sea water</subject><subject>Seas</subject><subject>Trajectories</subject><issn>0036-8075</issn><issn>1095-9203</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1987</creationdate><recordtype>article</recordtype><recordid>eNqN011v0zAUBuAIgVg3-AcTihBiFyPFX7GTO0bFSqVCkQbcWo570qZK4mIn0vj3nNKIDVSxxheJ4sdH1rHfKDqnZEwpk2-DraC1MGZcjkVGyFhw9igaUZKnSc4IfxyNCOEyyYhKT6LTEDaE4FzOn0YnVGVUUZaNonefILhgTQ3xwoJp3cqb7bqy8RfvLIQAIS6gBdOt424N8cxC7Mr42psmvum8qbpn0ZPS1AGeD--z6Nv1h6-Tj8l8MZ1NruaJVYJ2SSGslYrQVDBZZssiTRUtUgpSWUYFy40ksCwyEACqMIXiTAlGJeC3KQUv-Fl0sa-79e5HD6HTTRUs1LVpwfVBK84Z5ZJIlK__K7kUGc1J_iBklGK7hHoQUpFLxoRA-PIfuHG9b7EvWIynnGVit7_LPVph13XVlg4baVfYZW9q10JZ4e8r3CM-BPWbAxrHEprKHuAXf3EUHdx2K9OHoGc3n4-Vi-_HyvfTI2U2nd-Xl4ekdXUNK9B4dSaL-1rstfUuBA-l3vqqMf6npkTv0qCHNGhMg96lQWMacNmL4Tj6ooHl3aLh-iN4NQCzy0DpTWur8Mcpnqfi94md79kmdM7flZF5jhHjvwAMwRZT</recordid><startdate>19870424</startdate><enddate>19870424</enddate><creator>Manley, T. 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language | eng |
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source | JSTOR Archive Collection A-Z Listing; Science Magazine |
subjects | Analysis Arctic Buoyancy Datasets Earth, ocean, space Exact sciences and technology External geophysics Geology Ice Marine Ocean currents Ocean-atmosphere interaction Oceanography Oceans Physics of the oceans Saltwater Sea ice Sea water Seas Trajectories |
title | Mesoscale Oceanographic Processes beneath the Ice of Fram Strait |
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