Fill, flush, or shuffle: how is sediment carried through submarine channels to build lobes?

Accepted/In Press date: 1 March 2022

Published date: 15 April 2022

Additional Information: Funding Information: MSH was supported by European Union's Horizon 2020 research and innovation programme under the Marie Skłodowska-Curie grant agreement No. 721403 . MSH and MAC acknowledge funding through Climate Linked Atlantic Sector Science - NERC National Capability programme ( NE/R015953/1 ). MAC, MJCB, and PJT acknowledge funding from the Natural Environment Research Council (NERC), including “Environmental Risks to Infrastructure: Identifying and Filling the Gaps” ( NE/P005780/1 ), and “New field-scale calibration of turbidity current impact modelling” ( NE/P009190/1 ). MJBC was support by a Royal Society Research Fellowship ( DHF﹨R1﹨180166 ). Talling was supported by a NERC and Royal Society Industry Fellowship hosted by the International Cable Protection Committee. The authors also acknowledge discussions with collaborators as part of Talling's NERC International Opportunities Fund grant ( NE/M017540/1 ) “Coordinating and pump-priming international efforts for direct monitoring of active turbidity currents at global test sites”. ELP was supported by a Leverhulme Trust Early Career Fellowship ( ECF-2018-267 ). SH has received funding from the European Union's Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant agreement No 899546 . We further thank the Canadian Geological Survey and Canadian Hydrographic Survey for data collection and processing, in particular Peter Neelands and Brent Seymour. We also thank the captains and crew of CCGS Vector. We thank two reviewers and the editor for helpful and constructive comments that improved the manuscript. Funding Information: MSH was supported by European Union's Horizon 2020 research and innovation programme under the Marie Sk?odowska-Curie grant agreement No. 721403. MSH and MAC acknowledge funding through Climate Linked Atlantic Sector Science - NERC National Capability programme (NE/R015953/1). MAC, MJCB, and PJT acknowledge funding from the Natural Environment Research Council (NERC), including ?Environmental Risks to Infrastructure: Identifying and Filling the Gaps? (NE/P005780/1), and ?New field-scale calibration of turbidity current impact modelling? (NE/P009190/1). MJBC was support by a Royal Society Research Fellowship (DHF?R1?180166). Talling was supported by a NERC and Royal Society Industry Fellowship hosted by the International Cable Protection Committee. The authors also acknowledge discussions with collaborators as part of Talling's NERC International Opportunities Fund grant (NE/M017540/1) ?Coordinating and pump-priming international efforts for direct monitoring of active turbidity currents at global test sites?. ELP was supported by a Leverhulme Trust Early Career Fellowship (ECF-2018-267). SH has received funding from the European Union's Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant agreement No 899546. We further thank the Canadian Geological Survey and Canadian Hydrographic Survey for data collection and processing, in particular Peter Neelands and Brent Seymour. We also thank the captains and crew of CCGS Vector. We thank two reviewers and the editor for helpful and constructive comments that improved the manuscript. Publisher Copyright: © 2022 The Author(s)

Keywords: bypass, flushing, lobe, source to sink, submarine channel, turbidity current

Local EPrints ID: 457622

URI: http://eprints.soton.ac.uk/id/eprint/457622

DOI: doi:10.1016/j.epsl.2022.117481

ISSN: 0012-821X

PURE UUID: 7b6f6adc-ca64-4459-a2b3-6df0f4500aa3

Date deposited: 14 Jun 2022 16:43

Last modified: 15 Apr 2024 17:12