Return migration of Atlantic salmon in the River Tana: the role of environmental factors

Multi‐sea‐winter Atlantic salmon (75–115 cm fork length L F , 2–4‐winter fish) were radio‐tagged in the Tanafjord (700 N), Norway, in 1992–1993, and 130 fish entered the large subarctic River Tana (Teno). They entered the fresh water at any time of the tidal cycle but more so during the high and ebb...

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Bibliographic Details
Published in:Journal of Fish Biology
Main Authors: Erkinaro, J., ØKland, F., Moen, K., Niemelä, E., Rahiala, M.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1999
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Online Access:http://dx.doi.org/10.1111/j.1095-8649.1999.tb00695.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1095-8649.1999.tb00695.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1095-8649.1999.tb00695.x
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Summary:Multi‐sea‐winter Atlantic salmon (75–115 cm fork length L F , 2–4‐winter fish) were radio‐tagged in the Tanafjord (700 N), Norway, in 1992–1993, and 130 fish entered the large subarctic River Tana (Teno). They entered the fresh water at any time of the tidal cycle but more so during the high and ebbing tides. No diel rhythm was detected in river entry under polar day conditions. There were no differences in the change of flow between days when salmon moved and when they did not, but during active migration increasing discharge was associated with increased swimming activity of salmon, especially later in the summer. Increasing air temperature was also associated with enhanced migration activity. Low river flow was associated with increasing delay in salmon passing the first riffle area of the river, 35 km from the sea.