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| Fältnamn | Indikatorer | Metadata |
|---|---|---|
| 000 | 02679naa a2200373 4500 | |
| 001 | oai:DiVA.org:su-149820 | |
| 003 | SwePub | |
| 008 | 171214s2017 | |||||||||||000 ||eng| | |
| 024 | 7 | a https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-1498202 URI |
| 024 | 7 | a https://doi.org/10.1038/nature244722 DOI |
| 040 | a (SwePub)su | |
| 041 | a engb eng | |
| 042 | 9 SwePub | |
| 072 | 7 | a ref2 swepub-contenttype |
| 072 | 7 | a art2 swepub-publicationtype |
| 100 | 1 | a de lavergne, C.4 aut |
| 245 | 1 0 | a Abyssal ocean overturning shaped by seafloor distribution |
| 264 | c 2017-11-09 | |
| 264 | 1 | b Springer Science and Business Media LLC,c 2017 |
| 338 | a print2 rdacarrier | |
| 520 | a The abyssal ocean is broadly characterized by northward flow of the densest waters and southward flow of less-dense waters above them. Understanding what controls the strength and structure of these interhemispheric flows-referred to as the abyssal overturning circulation-is key to quantifying the ocean's ability to store carbon and heat on timescales exceeding a century. Here we show that, north of 32 degrees S, the depth distribution of the seafloor compels dense southernorigin waters to flow northward below a depth of about 4 kilometres and to return southward predominantly at depths greater than 2.5 kilometres. Unless ventilated from the north, the overlying mid-depths (1 to 2.5 kilometres deep) host comparatively weak mean meridional flow. Backed by analysis of historical radiocarbon measurements, the findings imply that the geometry of the Pacific, Indian and Atlantic basins places a major external constraint on the overturning structure. | |
| 650 | 7 | a NATURVETENSKAPx Geovetenskap och miljövetenskapx Oceanografi, hydrologi och vattenresurser0 (SwePub)105092 hsv//swe |
| 650 | 7 | a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Oceanography, Hydrology and Water Resources0 (SwePub)105092 hsv//eng |
| 653 | a Palaeoceanography | |
| 653 | a Physical oceanography | |
| 700 | 1 | a Madec, G.4 aut |
| 700 | 1 | a Roquet, Fabienu Stockholms universitet,Meteorologiska institutionen (MISU)4 aut0 (Swepub:su)froqu |
| 700 | 1 | a Holmes, R. M.4 aut |
| 700 | 1 | a McDougall, T. J.4 aut |
| 710 | 2 | a Stockholms universitetb Meteorologiska institutionen (MISU)4 org |
| 773 | 0 | t Natured : Springer Science and Business Media LLCg 551:7679, s. 181-186q 551:7679<181-186x 0028-0836x 1476-4687 |
| 856 | 4 | u https://hal.archives-ouvertes.fr/hal-03334723/file/abyssal%20ocean%20overturning%20shaped%20by%20seafloor%20distribution.pdf |
| 856 | 4 8 | u https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-149820 |
| 856 | 4 8 | u https://doi.org/10.1038/nature24472 |
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