Seasonal variations in the upper Arctic Ocean as observed at T-3
Hydrographic data from T‐3 are analyzed to illustrate the behavior of the Arctic mixed layer. The mixed layer depth fluctuates 11 m annually and mixed layer salinity fluctuates 0.32‰. The fluctuations in total salt content are consistent with theoretical work by Maykut and are in phase with mixed la...
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| Veröffentlicht in: | Geophysical research letters 1981-07, Vol.8 (7), p.753-756 |
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| container_title | Geophysical research letters |
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| creator | Morison, James Smith, J. Dungan |
| description | Hydrographic data from T‐3 are analyzed to illustrate the behavior of the Arctic mixed layer. The mixed layer depth fluctuates 11 m annually and mixed layer salinity fluctuates 0.32‰. The fluctuations in total salt content are consistent with theoretical work by Maykut and are in phase with mixed layer depth, indicating changes in the mixed layer are controlled by salt flux. Deepening of the mixed layer brings 0.3 kcal cm−2 yr−1 of heat to the surface from the ocean below. |
| doi_str_mv | 10.1029/GL008i007p00753 |
| format | Article |
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Dungan</creator><creatorcontrib>Morison, James ; Smith, J. Dungan</creatorcontrib><description>Hydrographic data from T‐3 are analyzed to illustrate the behavior of the Arctic mixed layer. The mixed layer depth fluctuates 11 m annually and mixed layer salinity fluctuates 0.32‰. The fluctuations in total salt content are consistent with theoretical work by Maykut and are in phase with mixed layer depth, indicating changes in the mixed layer are controlled by salt flux. Deepening of the mixed layer brings 0.3 kcal cm−2 yr−1 of heat to the surface from the ocean below.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/GL008i007p00753</identifier><language>eng</language><publisher>Blackwell Publishing Ltd</publisher><subject>Arctic Ocean ; Fluctuation ; Flux ; Geophysics ; Marine ; Oceans ; Phase transformations ; Salinity ; Seasonal variations</subject><ispartof>Geophysical research letters, 1981-07, Vol.8 (7), p.753-756</ispartof><rights>Copyright 1981 by the American Geophysical Union.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4179-dc558bfdc1dfdfdf4bac2fb4ef78fac5c0120c0f494bb8bd953c2b21a9cafc623</citedby><cites>FETCH-LOGICAL-c4179-dc558bfdc1dfdfdf4bac2fb4ef78fac5c0120c0f494bb8bd953c2b21a9cafc623</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2FGL008i007p00753$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2FGL008i007p00753$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,27901,27902,45550,45551</link.rule.ids></links><search><creatorcontrib>Morison, James</creatorcontrib><creatorcontrib>Smith, J. 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Deepening of the mixed layer brings 0.3 kcal cm−2 yr−1 of heat to the surface from the ocean below.</description><subject>Arctic Ocean</subject><subject>Fluctuation</subject><subject>Flux</subject><subject>Geophysics</subject><subject>Marine</subject><subject>Oceans</subject><subject>Phase transformations</subject><subject>Salinity</subject><subject>Seasonal variations</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1981</creationdate><recordtype>article</recordtype><recordid>eNqFkMtLxDAQxoMouD7OXnMSL9XJq01uimgVFwUfLHgJaZpgtLY16a7639tlxYMHZRhmBn7fN8MgtEfgkABVR-UUQAaAoh9TsDU0IYrzTI7TOpoAqLGnRb6JtlJ6BgAGjEzQ8Z0zqWtNgxcmBjOErk04tHh4cnje9y7ik2iHYPGNdabFJuGuSi4uXI3NgO8ztoM2vGmS2_2u2-jh_Oz-9CKb3pSXpyfTzHJSqKy2QsjK15bUfhm8Mpb6ijtfSG-ssEAoWPBc8aqSVa0Es7SixChrvM0p20b7K98-dm9zlwb9GpJ1TWNa182TJpLJQuVqBA_-BgUnnEolyf-egioh6XL50Qq0sUspOq_7GF5N_NQE9PL7-tf3RwVfKd5D4z7_w3V5OyV5sTw-W8lCGtzHj8zEF50XrBB6dl3qmYLyiqiZfmRfcyWWTw</recordid><startdate>198107</startdate><enddate>198107</enddate><creator>Morison, James</creator><creator>Smith, J. 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Deepening of the mixed layer brings 0.3 kcal cm−2 yr−1 of heat to the surface from the ocean below.</abstract><pub>Blackwell Publishing Ltd</pub><doi>10.1029/GL008i007p00753</doi><tpages>4</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0094-8276 |
| ispartof | Geophysical research letters, 1981-07, Vol.8 (7), p.753-756 |
| issn | 0094-8276 1944-8007 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_18387969 |
| source | Wiley Online Library Journals Frontfile Complete |
| subjects | Arctic Ocean Fluctuation Flux Geophysics Marine Oceans Phase transformations Salinity Seasonal variations |
| title | Seasonal variations in the upper Arctic Ocean as observed at T-3 |
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