2022
DOI: 10.1016/j.envpol.2022.119631
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Fate of river-derived microplastics from the South China Sea: Sources to surrounding seas, shores, and abysses

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Cited by 11 publications
(4 citation statements)
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“…In this high‐latitude region, the East Greenland Coastal Current interacts with the widely turning coast at Cape Farewell (Bacon et al., 2002; Sutherland & Pickart, 2008). Other global examples of plumes interacting with coastal corners are the Western Iberian plume at Cape Finisterre (Alvarez et al., 2011; Otero et al., 2008, 2009), the Mekong plume at Ca Mau Cape during the winter monsoon (e.g., Matsushita et al., 2022; Nguyen et al., 2022; Zeng et al., 2022), and the Ayeyarwady (Irrawaddy) plume at Mawtin Point (Liu et al., 2020; Sandeep & Pant, 2019). There are other pronounced coastal orientation changes near major rivers such as the Ob, Yenisei, and Yukon that influence wind response and plume behavior (Clark & Mannino, 2022; Frey & Osadchiev, 2021; Osadchiev et al., 2017).…”
Section: Discussionmentioning
confidence: 99%
“…In this high‐latitude region, the East Greenland Coastal Current interacts with the widely turning coast at Cape Farewell (Bacon et al., 2002; Sutherland & Pickart, 2008). Other global examples of plumes interacting with coastal corners are the Western Iberian plume at Cape Finisterre (Alvarez et al., 2011; Otero et al., 2008, 2009), the Mekong plume at Ca Mau Cape during the winter monsoon (e.g., Matsushita et al., 2022; Nguyen et al., 2022; Zeng et al., 2022), and the Ayeyarwady (Irrawaddy) plume at Mawtin Point (Liu et al., 2020; Sandeep & Pant, 2019). There are other pronounced coastal orientation changes near major rivers such as the Ob, Yenisei, and Yukon that influence wind response and plume behavior (Clark & Mannino, 2022; Frey & Osadchiev, 2021; Osadchiev et al., 2017).…”
Section: Discussionmentioning
confidence: 99%
“…Other wave effects, such as Stokes drift, wave setup, wave-driven nearshore currents, breaker-enhanced turbulent mixing, and wave-induced bottom streaming (e.g., Uchiyama et al, 2009;Uchiyama et al, 2010;Weir et al, 2011;Marchesiello et al, 2015;Uchiyama et al, 2017a;Akan et al, 2020;Wang et al, 2020;Wang et al, 2021), are also anticipated to significantly influence Lagrangian transport in coastal areas. The linear addition of Stokes drift to the Lagrangian equation of motion of the particle tracking models has been reported to improve reproducibility in the open ocean to a certain extent (e.g., Iwasaki et al, 2017;Matsushita et al, 2022). Nearshore currents, in particular transient rip currents (e.g., Fujimura et al, 2017;Uchiyama et al, 2017a;Fujimura et al, 2018), which occur intermittently and promote cross-shore exchange and dispersal extensively, must be considered to represent inter-reef larval transport.…”
Section: Discussionmentioning
confidence: 99%
“…The 3-D Lagrangian transport of coral larvae was then numerically simulated using the precomputed 3-D flow field of the ROMS-L4 model output provided at 2 h intervals. An offline 3-D Lagrangian particle tracking model for ROMS was exploited (Carr et al, 2008), which has frequently been used in numerical studies on Lagrangian dispersal of virtual fluid parcels (e.g., Romero et al, 2013;Romero et al, 2016;Masunaga et al, 2022), larvae and eggs of marine fauna (Mitarai et al, 2009;Uchiyama et al, 2018b;Uchiyama et al, 2018c;Takeda et al, 2021), and even microplastic particles (Matsushita et al, 2022) with ample validations against in situ datasets of Lagrangian floats and drifters. Corals have various biological characteristics, such as larval behavior, larval precompetency period, and larval reproduction duration, depending on their species, habitat, and other conditions (Shlesinger and Loya, 1985;Baird et al, 2009).…”
Section: Offline Lagrangian Particle Tracking Model For Romsmentioning
confidence: 99%
“…The initial and side boundary conditions for the ROMS were provided by monthly climatology of the assimilative JCOPE2 oceanic reanalysis (Miyazawa et al, 2009). A one-way offline nesting technique was employed to convey the parent JCOPE2 to the child ROMS model with grid resolution refinement (e.g., Mason et al, 2010;Uchiyama et al, 2014;Kamidaira et al, 2017;Uchiyama et al, 2017;Kamidaira et al, 2018;Uchiyama et al, 2018a;Uchiyama et al, 2018b;Uchiyama et al, 2018c;Tada et al, 2018;Masunaga et al, 2018;Kamidaira et al, 2019;Masunaga et al, 2019;Zhang et al, 2019;Kurosawa et al, 2020;Kamidaira et al, 2021;Takeda et al, 2021;Uchiyama et al, 2022;Masunaga et al, 2022;Matsushita et al, 2022). Therefore, the horizontal grid spacing was successfully reduced from 1/12°(~10 km) of the JCOPE2 reanalysis to 3 km of the ROMS model, and vertically into stretched 32 s-layers (Shchepetkin and McWilliams, 2005) with grid height refinement near the surface and bottom to adequately resolve the boundary layers.…”
Section: Ocean Circulation Modelmentioning
confidence: 99%