APA
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Thomson, K. A., Ingraham, W. J., Healey, M., Leblond, P., Groot, C., & Healey, C. G. (1994). Computer simulations of the influence of ocean currents on Fraser river sockeye salmon (Oncorhynchus nerka) return times. Canadian Journal of Fisheries and Aquatic Sciences, 51(2), 441–449.
Chicago/Turabian
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Thomson, K. A., W. J. Ingraham, M. Healey, P. Leblond, C. Groot, and C. G. Healey. “Computer Simulations of the Influence of Ocean Currents on Fraser River Sockeye Salmon (Oncorhynchus Nerka) Return Times.” Canadian Journal of Fisheries and Aquatic Sciences 51, no. 2 (1994): 441–449.
MLA
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Thomson, K. A., et al. “Computer Simulations of the Influence of Ocean Currents on Fraser River Sockeye Salmon (Oncorhynchus Nerka) Return Times.” Canadian Journal of Fisheries and Aquatic Sciences, vol. 51, no. 2, 1994, pp. 441–49.
BibTeX Click to copy
@article{k1994a,
title = {Computer simulations of the influence of ocean currents on Fraser river sockeye salmon (Oncorhynchus nerka) return times},
year = {1994},
issue = {2},
journal = {Canadian Journal of Fisheries and Aquatic Sciences},
pages = {441-449},
volume = {51},
author = {Thomson, K. A. and Ingraham, W. J. and Healey, M. and Leblond, P. and Groot, C. and Healey, C. G.}
}
We hypothesized that the interannual variability of the northeast Pacific Ocean circulation affects the return times of Fraser River sockeye salmon (Oncorhynchus nerka). Homeward migrations were simulated for 1982 (with a relatively weak Alaska Gyre circulation) and 1983 (with a relatively strong circulation) in the context of three sequential return migration phases: a nondirected oceanic phase, a directed oceanic phase, and a directed coastal phase. Passive drifters were simulated to examine the influence of ocean currents during the nondirected oceanic phase: model fish south of 48°N were advected closer to Vancouver Island in 1983 compared with 1982; those north of 48°N were advected closer to Vancouver Island in 1982 than in 1983. Fish were simulated during the directed oceanic phase using a variety of behaviour scenarios: model fish starting south of 50°N had earlier return times in 1983 than in 1982; those starting north of 50°N had return times in 1983 that were generally the same as or later than in 1982. We inferred that ocean currents would modulate the environmental influences on return times during the directed costal migration phase, by deflecting sockeye salmon into different oceanographic domains along the British Columbia coast.
