Sökning: WFRF:(Eriksson Johanna) > Flow of Canadian Ba...
Fältnamn | Indikatorer | Metadata |
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000 | 04601naa a2200577 4500 | |
001 | oai:gup.ub.gu.se/118479 | |
003 | SwePub | |
008 | 240528s2010 | |||||||||||000 ||eng| | |
009 | oai:DiVA.org:su-47295 | |
024 | 7 | a https://gup.ub.gu.se/publication/1184792 URI |
024 | 7 | a https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-472952 URI |
024 | 7 | a https://doi.org/10.1016/j.dsr.2010.01.0062 DOI |
040 | a (SwePub)gud (SwePub)su | |
041 | a eng | |
042 | 9 SwePub | |
072 | 7 | a ref2 swepub-contenttype |
072 | 7 | a art2 swepub-publicationtype |
100 | 1 | a Björk, Göran,d 1956u Gothenburg University,Göteborgs universitet,Institutionen för geovetenskaper,Department of Earth Sciences4 aut0 (Swepub:gu)xbjogo |
245 | 1 0 | a Flow of Canadian Basin Deep Water in the Western Eurasian Basin of the Arctic Ocean |
264 | 1 | b Elsevier BV,c 2010 |
500 | a authorCount :17 | |
520 | a The LOMROG 2007 expedition targeted the previously unexplored southern part of the Lomonosov Ridge north of Greenland together with a section from the Morris Jesup Rise to Gakkel Ridge. The oceanographic data shows that Canadian Basin Deep Water (CBDW) passes the Lomonosov Ridge in the area of the Intra Basin close to the North Pole and then continues along the ridge towards Greenland and further along its northernmost continental slope. The CBDW is clearly evident as a salinity maximum and oxygen minimum at a depth of about 2000 m. The cross slope sections at the Amundsen Basin side of the Lomonosov Ridge and further south at the Morris Jesup Rise show a sharp frontal structure higher up in the water column between Makarov Basin water and Amundsen Basin water. The frontal structure continues upward into the Atlantic Water up to a depth of about 300 m. The observed water mass division at levels well above the ridge crest indicates a strong topographic steering of the flow and that different water masses tend to pass the ridge guided by ridge-crossing isobaths at local topographic heights and depressions. A rough scaling analysis shows that the extremely steep and sharply turning bathymetry of the Morris Jesup Rise may force the boundary current to separate and generate deep eddies. | |
650 | 7 | a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe |
650 | 7 | a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng |
653 | a Deep water circulation | |
653 | a Intermediate water circulation | |
653 | a Arctic Ocean | |
653 | a Eurasian Basin | |
653 | a Deep water circulation; Intermediate water circulation; Arctic Ocean; Eurasian Basin | |
653 | a Earth sciences | |
700 | 1 | a Anderson, Leif G,d 1951u Gothenburg University,Göteborgs universitet,Institutionen för kemi,Department of Chemistry4 aut0 (Swepub:gu)xanlei |
700 | 1 | a Jakobsson, Martinu Stockholms universitet,Institutionen för geologiska vetenskaper,Marin geologi4 aut0 (Swepub:su)mjako |
700 | 1 | a Antony, D4 aut |
700 | 1 | a Eriksson, Björnu Stockholms universitet,Institutionen för geologiska vetenskaper4 aut0 (Swepub:su)bjeri |
700 | 1 | a Eriksson, PB4 aut |
700 | 1 | a Hell, Benjaminu Stockholms universitet,Institutionen för geologiska vetenskaper4 aut0 (Swepub:su)bhell |
700 | 1 | a Hjalmarsson, Sofia,d 1980u Gothenburg University,Göteborgs universitet,Institutionen för kemi,Department of Chemistry4 aut0 (Swepub:gu)xhjaso |
700 | 1 | a Janzen, T4 aut |
700 | 1 | a Jutterström, Sara,d 1975u Gothenburg University,Göteborgs universitet,Institutionen för kemi,Department of Chemistry4 aut0 (Swepub:gu)xjutsa |
700 | 1 | a Linders, Johannau Gothenburg University,Göteborgs universitet,Institutionen för geovetenskaper,Department of Earth Sciences4 aut |
700 | 1 | a Löwemark, Ludvigu Stockholms universitet,Institutionen för geologiska vetenskaper4 aut0 (Swepub:su)lul4918 |
700 | 1 | a marcussen, C4 aut |
700 | 1 | a Olsson, Anders,d 1970u Gothenburg University,Göteborgs universitet,Institutionen för kemi,Department of Chemistry4 aut0 (Swepub:gu)xoandq |
700 | 1 | a Rudels, B.4 aut |
700 | 1 | a Sellen, Eu Stockholms universitet,Institutionen för geologiska vetenskaper4 aut |
700 | 1 | a Sölvsten, M4 aut |
710 | 2 | a Göteborgs universitetb Institutionen för geovetenskaper4 org |
773 | 0 | t Deep Sea Researchd : Elsevier BVg 57:4, s. 577-586q 57:4<577-586x 0967-0637x 1879-0119 |
856 | 4 8 | u https://gup.ub.gu.se/publication/118479 |
856 | 4 8 | u https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-47295 |
856 | 4 8 | u https://doi.org/10.1016/j.dsr.2010.01.006 |
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