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Factors affecting stranding of juvenile salmonids by wakes from ship passage in the Lower Columbia River
Author(s) -
Pearson W. H.,
Skalski J. R.
Publication year - 2011
Publication title -
river research and applications
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.679
H-Index - 94
eISSN - 1535-1467
pISSN - 1535-1459
DOI - 10.1002/rra.1397
Subject(s) - chinook wind , tributary , oncorhynchus , fishery , juvenile , channel (broadcasting) , juvenile fish , environmental science , oceanography , hydrology (agriculture) , fish <actinopterygii> , geography , geology , ecology , biology , geotechnical engineering , cartography , engineering , electrical engineering
The effects of deep‐draft vessel traffic in confined riverine channels on shorelines and fish are of widespread concern. In the Pacific Northwest of the United States, wakes and subsequent beach run‐up from ships transiting the Lower Columbia River have been observed to strand juvenile salmon and other fish. As part of a before‐and‐after study to assess stranding effects that may be associated with channel deepening, we measured 19 variables from observations of 126 vessel passages at three low‐slope beaches and used multiple logistic regression to discern the significant factors influencing the frequency of stranding. Subyearling Chinook salmon were 82% of the fish stranded over all sites and seasons. Given a low‐slope beach, stranding frequencies for juvenile salmon were significantly related to river location, salmon density in the shallows, a proxy for ship kinetic energy, tidal height and two interactions. The beach types selected for our study do not include all the beach types along the Lower Columbia River so that the stranding probabilities described here cannot be extrapolated river‐wide. A more sophisticated modelling effort, informed by additional field data, is needed to assess salmon losses by stranding for the entire lower river. Such modelling needs to include river‐scale factors such as beach type, berms, proximity to navigation channel, and perhaps, proximity to tributaries that act as sources of outmigrating juvenile salmon. At both river and beach scales, no one factor produces stranding; rather interactions among several conditions produce a stranding event and give stranding its episodic nature. Published in 2010 by John Wiley & Sons, Ltd.