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Original Articles

Investigating the Effect of Oceanographic Conditions and Swimming Behaviours on the Movement of Particles in the Gulf of St. Lawrence Using an Individual-Based Numerical Model

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Pages 278-298 | Received 07 Sep 2014, Accepted 29 Jul 2015, Published online: 19 Oct 2015

Figures & data

Fig. 1 The model domain and its major bathymetric features. Abbreviations are used for Rivière-du-Loup (RdL), the St. Lawrence Estuary (SLE), Strait of Belle Isle (SBI), Prince Edward Island (PEI), and the Bay of Fundy (BoF). Black lines with circles indicate idealized channels that represent rivers in the model. The initial release area of particles is outlined with a solid red line in the SLE. The dashed red line at the mouth of the SLE indicates the location at which STST ceases. Atlantic Zone Monitoring Program (AZMP) stations are indicated by numbers, and tide gauges are indicated by letters.

Fig. 1 The model domain and its major bathymetric features. Abbreviations are used for Rivière-du-Loup (RdL), the St. Lawrence Estuary (SLE), Strait of Belle Isle (SBI), Prince Edward Island (PEI), and the Bay of Fundy (BoF). Black lines with circles indicate idealized channels that represent rivers in the model. The initial release area of particles is outlined with a solid red line in the SLE. The dashed red line at the mouth of the SLE indicates the location at which STST ceases. Atlantic Zone Monitoring Program (AZMP) stations are indicated by numbers, and tide gauges are indicated by letters.

Fig. 2 Monthly-mean fields of salinity and currents for November 2011 calculated from model results at depths of (a) 5, (b) 20, (c) 50, and (d) 100 m in the St. Lawrence Estuary, Gulf of St. Lawrence, and eastern Scotian Shelf. Velocity vectors are shown at every fourth grid point. The dashed lines in (a) outline the area that will be shown in .

Fig. 2 Monthly-mean fields of salinity and currents for November 2011 calculated from model results at depths of (a) 5, (b) 20, (c) 50, and (d) 100 m in the St. Lawrence Estuary, Gulf of St. Lawrence, and eastern Scotian Shelf. Velocity vectors are shown at every fourth grid point. The dashed lines in (a) outline the area that will be shown in Fig. 3.

Fig. 3 Monthly-mean fields of salinity and currents for November 2011 calculated from model results at depths of (a) 5, (b) 20, (c) 50, and (d) 100 m in the St. Lawrence Estuary. Velocity vectors are shown at every model grid point.

Fig. 3 Monthly-mean fields of salinity and currents for November 2011 calculated from model results at depths of (a) 5, (b) 20, (c) 50, and (d) 100 m in the St. Lawrence Estuary. Velocity vectors are shown at every model grid point.

Fig. 4 (a) The life cycle of the American eel. Spawning takes place in the Sargasso Sea, and the larvae (leptocephali) are transported by ocean currents towards the east coast of North America. The juveniles (glass eels) migrate into coastal and inland waters and eventually metamorphose into yellow eels. During their seaward spawning migration, they metamorphose into silver eels. (Image reproduced by permission of the American Eel Monitoring Program at the Virginia Institute of Marine Science (http://www.vims.edu/research/departments/fisheries/programs/eel_survey/life_history/index.php). (b) Depth recorded every 15 minutes by an electronic tag attached to a silver American eel, released from Rivière-du-Loup in the SLE (). This dataset was also used in of Béguer-Pon et al. (Citation2012).

Fig. 4 (a) The life cycle of the American eel. Spawning takes place in the Sargasso Sea, and the larvae (leptocephali) are transported by ocean currents towards the east coast of North America. The juveniles (glass eels) migrate into coastal and inland waters and eventually metamorphose into yellow eels. During their seaward spawning migration, they metamorphose into silver eels. (Image reproduced by permission of the American Eel Monitoring Program at the Virginia Institute of Marine Science (http://www.vims.edu/research/departments/fisheries/programs/eel_survey/life_history/index.php). (b) Depth recorded every 15 minutes by an electronic tag attached to a silver American eel, released from Rivière-du-Loup in the SLE (Fig. 1). This dataset was also used in Fig. 2 of Béguer-Pon et al. (Citation2012).

Fig. 5 Scatterplots between observed and simulated amplitudes and phases of tidal elevations for the M2 and K1 tidal constituents for 2011 at the eight tide gauge locations shown in .

Fig. 5 Scatterplots between observed and simulated amplitudes and phases of tidal elevations for the M2 and K1 tidal constituents for 2011 at the eight tide gauge locations shown in Fig. 1.

Fig. 6 Scatterplots between simulated and observed salinity for 2011 at AZMP stations: (a) Rimouski, (b) Anticosti, (c) Gaspé, and (d) Shediac.

Fig. 6 Scatterplots between simulated and observed salinity for 2011 at AZMP stations: (a) Rimouski, (b) Anticosti, (c) Gaspé, and (d) Shediac.

Fig. 7 Schematic diagram for the manner in which the numerical particle-tracking scheme moves particles that have moved into a dry grid cell of the model back to a wet grid cell. The grey squares represent wet grid cells, and the white squares represent dry grid cells. (a) The particle is in cell 1 (a wet grid cell) at time t (at the position denoted by a square), but its calculated position for time tt (denoted by a circle) is in cell 3 (a dry grid cell); (b) the particle-tracking scheme determines that the closest grid cell to the particle's provisional new position is cell 4, followed by cell 1; (c) however, the particle cannot move into cell 4 because it also is a dry grid cell; and (d) the particle moves northward into cell 1, and its new meridional distance from the coast (Δy2) is of the same magnitude as the meridional distance by which it had moved inland in the provisional position (Δy1).

Fig. 7 Schematic diagram for the manner in which the numerical particle-tracking scheme moves particles that have moved into a dry grid cell of the model back to a wet grid cell. The grey squares represent wet grid cells, and the white squares represent dry grid cells. (a) The particle is in cell 1 (a wet grid cell) at time t (at the position denoted by a square), but its calculated position for time t+Δt (denoted by a circle) is in cell 3 (a dry grid cell); (b) the particle-tracking scheme determines that the closest grid cell to the particle's provisional new position is cell 4, followed by cell 1; (c) however, the particle cannot move into cell 4 because it also is a dry grid cell; and (d) the particle moves northward into cell 1, and its new meridional distance from the coast (Δy2) is of the same magnitude as the meridional distance by which it had moved inland in the provisional position (Δy1).

Table 1. Sunrise and sunset times used in experiments that include DVM.

Table 2. List of the 19 numerical experiments conducted in this study. In experiments H1, H2, S1, S2, and W1, the lateral swimming speed is 0.5 m s−1. The experiments are grouped as follows: Group A (experiments P1, P2, P3, P4, HM1, HP1, VM1, VP1, P1H, and P1D), Group B (experiments M1, M2, M3, and T1), and Group C (experiments H1, H2, S1, S2, and W1).

Fig. 8 Distributions of particles after 60 days in (a) experiment P1 (passive particles released at 20 m depth), (b) experiment P2 (passive particles released near the bottom), (c) experiment P3 (similar to P1 but with no vertical advection), (d) experiment P4 (similar to P2 but with no vertical advection). The blue circle indicates the location of the centre of mass of the particles, and the area outlined in green represents the release area for the particles.

Fig. 8 Distributions of particles after 60 days in (a) experiment P1 (passive particles released at 20 m depth), (b) experiment P2 (passive particles released near the bottom), (c) experiment P3 (similar to P1 but with no vertical advection), (d) experiment P4 (similar to P2 but with no vertical advection). The blue circle indicates the location of the centre of mass of the particles, and the area outlined in green represents the release area for the particles.

Fig. 9 Means (circles) and standard deviations (crosses) for (a) horizontal distances of particles relative to the centre of mass and (b) depths of particles after 60 days, in experiments P1 to P4 and the experiments in group B (in which the horizontal eddy diffusivity of the random walk component is decreased (HM1) or increased (HP1) by an order of magnitude, or the vertical eddy diffusivity is decreased (VM1) or increased (VH1) by an order of magnitude.)

Fig. 9 Means (circles) and standard deviations (crosses) for (a) horizontal distances of particles relative to the centre of mass and (b) depths of particles after 60 days, in experiments P1 to P4 and the experiments in group B (in which the horizontal eddy diffusivity of the random walk component is decreased (HM1) or increased (HP1) by an order of magnitude, or the vertical eddy diffusivity is decreased (VM1) or increased (VH1) by an order of magnitude.)

Fig. 10 Means (circles) and standard deviations (crosses) for (a) horizontal distances of particles relative to the centre of mass and (b) depths of particles, in experiment P1H (passive particles with release times varied in one-hour increments, up to 12 hours, before and after the release time used in experiment P1); (c) and (d) are similar to (a) and (b) but for experiment P1D (similar to experiment P1H but with particle release times varied in one-day increments, up to 15 days, before and after the release time used in experiment P1).

Fig. 10 Means (circles) and standard deviations (crosses) for (a) horizontal distances of particles relative to the centre of mass and (b) depths of particles, in experiment P1H (passive particles with release times varied in one-hour increments, up to 12 hours, before and after the release time used in experiment P1); (c) and (d) are similar to (a) and (b) but for experiment P1D (similar to experiment P1H but with particle release times varied in one-day increments, up to 15 days, before and after the release time used in experiment P1).

Fig. 11 Distributions of particles after 60 days in (a) experiment M1 (the upper limit of DVM is the 20 m depth and the lower limit is 20 m above the bottom or 90% of the water depth if the water depth < 60 m); (b) experiment M2 (the upper limit of DVM is changed to the 5 m depth); (c) experiment M3 (the lower limit of DVM is changed to 5 m above the bottom if the water depth is > 60 m); and (d) experiment T1 (DVM is the same as in experiment M1, but STST is added). The blue circle indicates the location of the centre of mass of the particles and the area outlined in green represents the release area of particles.

Fig. 11 Distributions of particles after 60 days in (a) experiment M1 (the upper limit of DVM is the 20 m depth and the lower limit is 20 m above the bottom or 90% of the water depth if the water depth < 60 m); (b) experiment M2 (the upper limit of DVM is changed to the 5 m depth); (c) experiment M3 (the lower limit of DVM is changed to 5 m above the bottom if the water depth is > 60 m); and (d) experiment T1 (DVM is the same as in experiment M1, but STST is added). The blue circle indicates the location of the centre of mass of the particles and the area outlined in green represents the release area of particles.

Fig. 12 Distributions of particles after 60 days in (a) experiment H1 (when outside the SLE, particles search for surrounding model grid points with deeper water every hour during the day and swim towards it if one is found; otherwise, they swim in random directions); (b) experiment H2 (similar to H1 but searching for deeper water every other hour during the day); (c) experiment S1 (when outside the SLE, particles search for surrounding model grid points with higher salinity every hour during the night and swim towards it if one is found; otherwise, they swim in random directions); (d) experiment S2 (similar to S1 but searching for higher salinity every four hours during the night); and (e) experiment W1 (particles swim in random directions during all hours when outside the SLE). (f) Distribution of particles after 120 days in experiment W1.

Fig. 12 Distributions of particles after 60 days in (a) experiment H1 (when outside the SLE, particles search for surrounding model grid points with deeper water every hour during the day and swim towards it if one is found; otherwise, they swim in random directions); (b) experiment H2 (similar to H1 but searching for deeper water every other hour during the day); (c) experiment S1 (when outside the SLE, particles search for surrounding model grid points with higher salinity every hour during the night and swim towards it if one is found; otherwise, they swim in random directions); (d) experiment S2 (similar to S1 but searching for higher salinity every four hours during the night); and (e) experiment W1 (particles swim in random directions during all hours when outside the SLE). (f) Distribution of particles after 120 days in experiment W1.

Table A1. List of major rivers in the St. Lawrence Estuary and Gulf of St. Lawrence, station names, and years of observation periods.

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