Longest sediment flows yet measured show how major rivers connect efficiently to deep sea
Here we show how major rivers can efficiently connect to the deep-sea, by analysing the longest runout sediment flows (of any type) yet measured in action on Earth. These seafloor turbidity currents originated from the Congo River-mouth, with one flow travelling >1,130 km whilst accelerating from...
| Main Authors: | , , , , , , , , , , , , , , , , , , , , , , , , , , , , , |
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| Format: | Journal article |
| Language: | English |
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Springer Nature
2022
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| Subjects: |
| _version_ | 1797110032211378176 |
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| author | Talling, PJ Baker, ML Pope, EL Ruffell, SC Jacinto, RS Heijnen, MS Hage, S Simmons, SM Hasenhündl, M Heerema, CJ McGhee, C Apprioual, R Ferrant, A Cartigny, MJB Parsons, DR Clare, MA Tshimanga, RM Trigg, MA Cula, CA Faria, R Gaillot, A Bola, G Wallance, D Griffiths, A Nunny, R Urlaub, M Peirce, C Burnett, R Neasham, J Hilton, R |
| author_facet | Talling, PJ Baker, ML Pope, EL Ruffell, SC Jacinto, RS Heijnen, MS Hage, S Simmons, SM Hasenhündl, M Heerema, CJ McGhee, C Apprioual, R Ferrant, A Cartigny, MJB Parsons, DR Clare, MA Tshimanga, RM Trigg, MA Cula, CA Faria, R Gaillot, A Bola, G Wallance, D Griffiths, A Nunny, R Urlaub, M Peirce, C Burnett, R Neasham, J Hilton, R |
| author_sort | Talling, PJ |
| collection | OXFORD |
| description | Here we show how major rivers can efficiently connect to the deep-sea, by analysing the longest runout sediment flows (of any type) yet measured in action on Earth. These seafloor turbidity currents originated from the Congo River-mouth, with one flow travelling >1,130 km whilst accelerating from 5.2 to 8.0 m/s. In one year, these turbidity currents eroded 1,338-2,675 [>535-1,070] Mt of sediment from one submarine canyon, equivalent to 19–37 [>7–15] % of annual suspended sediment flux from present-day rivers. It was known earthquakes trigger canyon-flushing flows. We show river-floods also generate canyon-flushing flows, primed by rapid sediment-accumulation at the river-mouth, and sometimes triggered by spring tides weeks to months post-flood. It is demonstrated that strongly erosional turbidity currents self-accelerate, thereby travelling much further, validating a long-proposed theory. These observations explain highly-efficient organic carbon transfer, and have important implications for hazards to seabed cables, or deep-sea impacts of terrestrial climate change. |
| first_indexed | 2024-03-07T07:49:33Z |
| format | Journal article |
| id | oxford-uuid:232d7991-11fc-4595-b02a-c176cb081ef5 |
| institution | University of Oxford |
| language | English |
| last_indexed | 2024-03-07T07:49:33Z |
| publishDate | 2022 |
| publisher | Springer Nature |
| record_format | dspace |
| spelling | oxford-uuid:232d7991-11fc-4595-b02a-c176cb081ef52023-07-11T09:50:55ZLongest sediment flows yet measured show how major rivers connect efficiently to deep seaJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:232d7991-11fc-4595-b02a-c176cb081ef5Physical oceanographyNatural hazardsEnglishSymplectic ElementsSpringer Nature2022Talling, PJBaker, MLPope, ELRuffell, SCJacinto, RSHeijnen, MSHage, SSimmons, SMHasenhündl, MHeerema, CJMcGhee, CApprioual, RFerrant, ACartigny, MJBParsons, DRClare, MATshimanga, RMTrigg, MACula, CAFaria, RGaillot, ABola, GWallance, DGriffiths, ANunny, RUrlaub, MPeirce, CBurnett, RNeasham, JHilton, RHere we show how major rivers can efficiently connect to the deep-sea, by analysing the longest runout sediment flows (of any type) yet measured in action on Earth. These seafloor turbidity currents originated from the Congo River-mouth, with one flow travelling >1,130 km whilst accelerating from 5.2 to 8.0 m/s. In one year, these turbidity currents eroded 1,338-2,675 [>535-1,070] Mt of sediment from one submarine canyon, equivalent to 19–37 [>7–15] % of annual suspended sediment flux from present-day rivers. It was known earthquakes trigger canyon-flushing flows. We show river-floods also generate canyon-flushing flows, primed by rapid sediment-accumulation at the river-mouth, and sometimes triggered by spring tides weeks to months post-flood. It is demonstrated that strongly erosional turbidity currents self-accelerate, thereby travelling much further, validating a long-proposed theory. These observations explain highly-efficient organic carbon transfer, and have important implications for hazards to seabed cables, or deep-sea impacts of terrestrial climate change. |
| spellingShingle | Physical oceanography Natural hazards Talling, PJ Baker, ML Pope, EL Ruffell, SC Jacinto, RS Heijnen, MS Hage, S Simmons, SM Hasenhündl, M Heerema, CJ McGhee, C Apprioual, R Ferrant, A Cartigny, MJB Parsons, DR Clare, MA Tshimanga, RM Trigg, MA Cula, CA Faria, R Gaillot, A Bola, G Wallance, D Griffiths, A Nunny, R Urlaub, M Peirce, C Burnett, R Neasham, J Hilton, R Longest sediment flows yet measured show how major rivers connect efficiently to deep sea |
| title | Longest sediment flows yet measured show how major rivers connect efficiently to deep sea |
| title_full | Longest sediment flows yet measured show how major rivers connect efficiently to deep sea |
| title_fullStr | Longest sediment flows yet measured show how major rivers connect efficiently to deep sea |
| title_full_unstemmed | Longest sediment flows yet measured show how major rivers connect efficiently to deep sea |
| title_short | Longest sediment flows yet measured show how major rivers connect efficiently to deep sea |
| title_sort | longest sediment flows yet measured show how major rivers connect efficiently to deep sea |
| topic | Physical oceanography Natural hazards |
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