Deep ocean circulation: physical and chemical aspects
Saved in:
| Format: | Electronic eBook |
|---|---|
| Language: | English |
| Published: |
Amsterdam
Elsevier
1993
|
| Series: | Elsevier oceanography series
59 |
| Subjects: | |
| Online Access: | Volltext |
| Item Description: | This volume comprises the final report of the research project entitled the Dynamics of the Deep Ocean Circulation. The layered structure of the subsurface circulation, which had been predicted in the hypothetical model proposed prior to the research, is verified through Eulerian and Lagrangian measurements of current. By the use of the numerical model, the deep circulation of the Philippine Sea, which has been long supposed to be isolated from the North Pacific, is revealed to be derived in close association with that of the latter ocean. Behavior of the deep current around the equator is also clarified by numerical modeling. By the extensive use of sediment trapping technology, it becomes clear that sinking sediments play an important role in the distribution of chemical substances in the deep ocean. Graduate students in the field of oceanography will find this a good textbook Includes bibliographical references |
| Physical Description: | 1 Online-Ressource (ix, 382 p.) |
| ISBN: | 9780444889614 0444889612 9780080870977 008087097X |
Staff View
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Record in the Search Index
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| dewey-full | 551.47 |
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| dewey-ones | 551 - Geology, hydrology, meteorology |
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| discipline | Geologie / Paläontologie |
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| spelling | Deep ocean circulation physical and chemical aspects edited by T. Teramoto Amsterdam Elsevier 1993 1 Online-Ressource (ix, 382 p.) txt rdacontent c rdamedia cr rdacarrier Elsevier oceanography series 59 This volume comprises the final report of the research project entitled the Dynamics of the Deep Ocean Circulation. The layered structure of the subsurface circulation, which had been predicted in the hypothetical model proposed prior to the research, is verified through Eulerian and Lagrangian measurements of current. By the use of the numerical model, the deep circulation of the Philippine Sea, which has been long supposed to be isolated from the North Pacific, is revealed to be derived in close association with that of the latter ocean. Behavior of the deep current around the equator is also clarified by numerical modeling. By the extensive use of sediment trapping technology, it becomes clear that sinking sediments play an important role in the distribution of chemical substances in the deep ocean. Graduate students in the field of oceanography will find this a good textbook Includes bibliographical references Oceans / Currents Chemical oceanography fast Ocean circulation fast SCIENCE / Earth Sciences / Oceanography bisacsh NATURE / Ecosystems & Habitats / Oceans & Seas bisacsh Geowissenschaften Ocean circulation Chemical oceanography Hydrochemie (DE-588)4072678-2 gnd rswk-swf Meeresströmung (DE-588)4130725-2 gnd rswk-swf Meeresphysik (DE-588)4038324-6 gnd rswk-swf Tiefsee (DE-588)4185436-6 gnd rswk-swf 1\p (DE-588)4143413-4 Aufsatzsammlung gnd-content Tiefsee (DE-588)4185436-6 s Meeresströmung (DE-588)4130725-2 s Hydrochemie (DE-588)4072678-2 s 2\p DE-604 Meeresphysik (DE-588)4038324-6 s 3\p DE-604 Teramoto, Toshihiko Sonstige oth http://www.sciencedirect.com/science/book/9780444889614 Verlag Volltext 1\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk 2\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk 3\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk |
| spellingShingle | Deep ocean circulation physical and chemical aspects Oceans / Currents Chemical oceanography fast Ocean circulation fast SCIENCE / Earth Sciences / Oceanography bisacsh NATURE / Ecosystems & Habitats / Oceans & Seas bisacsh Geowissenschaften Ocean circulation Chemical oceanography Hydrochemie (DE-588)4072678-2 gnd Meeresströmung (DE-588)4130725-2 gnd Meeresphysik (DE-588)4038324-6 gnd Tiefsee (DE-588)4185436-6 gnd |
| subject_GND | (DE-588)4072678-2 (DE-588)4130725-2 (DE-588)4038324-6 (DE-588)4185436-6 (DE-588)4143413-4 |
| title | Deep ocean circulation physical and chemical aspects |
| title_auth | Deep ocean circulation physical and chemical aspects |
| title_exact_search | Deep ocean circulation physical and chemical aspects |
| title_full | Deep ocean circulation physical and chemical aspects edited by T. Teramoto |
| title_fullStr | Deep ocean circulation physical and chemical aspects edited by T. Teramoto |
| title_full_unstemmed | Deep ocean circulation physical and chemical aspects edited by T. Teramoto |
| title_short | Deep ocean circulation |
| title_sort | deep ocean circulation physical and chemical aspects |
| title_sub | physical and chemical aspects |
| topic | Oceans / Currents Chemical oceanography fast Ocean circulation fast SCIENCE / Earth Sciences / Oceanography bisacsh NATURE / Ecosystems & Habitats / Oceans & Seas bisacsh Geowissenschaften Ocean circulation Chemical oceanography Hydrochemie (DE-588)4072678-2 gnd Meeresströmung (DE-588)4130725-2 gnd Meeresphysik (DE-588)4038324-6 gnd Tiefsee (DE-588)4185436-6 gnd |
| topic_facet | Oceans / Currents Chemical oceanography Ocean circulation SCIENCE / Earth Sciences / Oceanography NATURE / Ecosystems & Habitats / Oceans & Seas Geowissenschaften Hydrochemie Meeresströmung Meeresphysik Tiefsee Aufsatzsammlung |
| url | http://www.sciencedirect.com/science/book/9780444889614 |
| work_keys_str_mv | AT teramototoshihiko deepoceancirculationphysicalandchemicalaspects |