globalchange  > 气候变化与战略
DOI: 10.1016/j.epsl.2021.116845
论文题名:
Preconditioning by sediment accumulation can produce powerful turbidity currents without major external triggers
作者: Bailey L.P.; Clare M.A.; Rosenberger K.J.; Cartigny M.J.B.; Talling P.J.; Paull C.K.; Gwiazda R.; Parsons D.R.; Simmons S.M.; Xu J.; Haigh I.D.; Maier K.L.; McGann M.; Lundsten E.; Monterey CCE Team
刊名: Earth and Planetary Science Letters
ISSN: 0012821X
出版年: 2021
卷: 562
语种: 英语
中文关键词: direct monitoring ; geohazard ; preconditioning ; submarine canyon ; triggering ; turbidity current
英文关键词: Offshore oil well production ; Pore pressure ; Rivers ; Sediment transport ; Storms ; Turbidity ; Direct monitoring ; External perturbations ; Pressure variations ; Seasonal patterns ; Sediment accumulation ; Sediment transfers ; Triggering mechanism ; Turbidity current ; Ocean currents ; accumulation ; pore pressure ; sediment transport ; submarine canyon ; trigger mechanism ; turbidity current ; California ; Monterey Canyon ; Pacific Ocean ; United States
英文摘要: Turbidity currents dominate sediment transfer into the deep ocean, and can damage critical seabed infrastructure. It is commonly inferred that powerful turbidity currents are triggered by major external events, such as storms, river floods, or earthquakes. However, basic models for turbidity current triggering remain poorly tested, with few studies accurately recording precise flow timing. Here, we analyse the most detailed series of measurements yet made of powerful (up to 7.2 m s−1) turbidity currents, within Monterey Canyon, offshore California. During 18-months of instrument deployment, fourteen turbidity currents were directly monitored. No consistent triggering mechanism was observed, though flows did cluster around enhanced seasonal sediment supply. We compare turbidity current timing at Monterey Canyon (a sandy canyon-head fed by longshore drift) to the only other systems where numerous (>10-100) flows have been measured precisely via direct monitoring; the Squamish Delta (a sandy fjord-head delta), and the Congo Canyon (connected to the mud-dominated mouth of the Congo River). A common seasonal pattern emerges, leading to a new model for preconditioning and triggering of turbidity currents initiating through slope failure in areas of sediment accumulation, such as canyon heads or river mouths. In this model, rapid or sustained sediment supply alone can produce elevated pore pressures, which may persist, thereby predisposing slopes to fail. Once preconditioned, a range of minor external perturbations, such as moderate storm-waves, result in local pore pressure variation, and thus become effective triggers. Major external triggers are therefore not always a prerequisite for triggering of powerful turbidity currents. © 2021
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/165403
Appears in Collections:气候变化与战略

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作者单位: National Oceanography Centre, Southampton, SO14 3ZH, United Kingdom; School of Ocean and Earth Science, University of Southampton, Southampton, SO14 3ZH, United Kingdom; Pacific Coastal and Marine Science Center, U.S. Geological Survey, Santa Cruz, CA 95060, United States; Departments of Geography and Earth Science, Durham University, Durham, DH1 3LE, United Kingdom; Monterey Bay Aquarium Research Institute, Moss Landing, CA 95039, United States; Energy and Environment Institute, University of Hull, Hull, HU6 7RX, United Kingdom; Southern University of Science and Technology, Shenzhen, 518055, China; National Institute of Water and Atmospheric Research, Wellington, 6241, New Zealand; Pacific Coastal and Marine Science Center, U.S. Geological Survey, Menlo Park, CA 94025, United States

Recommended Citation:
Bailey L.P.,Clare M.A.,Rosenberger K.J.,et al. Preconditioning by sediment accumulation can produce powerful turbidity currents without major external triggers[J]. Earth and Planetary Science Letters,2021-01-01,562
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