2004
DOI: 10.1016/s0165-7836(03)00146-2
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Temporal and environmental influences on the variation in sea trout (Salmo trutta L.) smolt migration in the Burrishoole system in the west of Ireland from 1971 to 2000

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Cited by 27 publications
(27 citation statements)
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“…an early increase in temperature resulted in an early increase in downstream movement. In addition, several long-term studies have observed earlier initiating salmon (Friedland et al, 2003;Kennedy and Crozier, 2010;O'Maoiléidigh et al, 2003) and sea trout (Salmo trutta L.) (Byrne et al, 2004) smolt migrations associated with increasing spring temperatures. The timing of downstream migration of salmon has also been correlated with increased river flow (Allen, 1944;Hesthagen and Gärnäs, 1986;Ősterdahl, 1969).…”
Section: Control Yearsmentioning
confidence: 99%
“…an early increase in temperature resulted in an early increase in downstream movement. In addition, several long-term studies have observed earlier initiating salmon (Friedland et al, 2003;Kennedy and Crozier, 2010;O'Maoiléidigh et al, 2003) and sea trout (Salmo trutta L.) (Byrne et al, 2004) smolt migrations associated with increasing spring temperatures. The timing of downstream migration of salmon has also been correlated with increased river flow (Allen, 1944;Hesthagen and Gärnäs, 1986;Ősterdahl, 1969).…”
Section: Control Yearsmentioning
confidence: 99%
“…Smolting appears less stringent in brown trout than in Atlantic salmon and does not seem to be an obligatory process for seawater adaptation in this species. Usually, juvenile trout migrate from rivers in spring (March-June in Europe; Byrne, Poole, Dillane, Rogan, & Whelan, 2004;Flaten et al, 2016;, but may also migrate at other times of the year, for example during autumn Jonsson & Jonsson, 2009aPoole et al, 2007;Poole, Whelan, Dillane, Cooke, & Matthews, 1996;Taal et al, 2014;Winter et al, 2016), indicating that the time of seaward migration is highly plastic. Usually, juvenile trout migrate from rivers in spring (March-June in Europe; Byrne, Poole, Dillane, Rogan, & Whelan, 2004;Flaten et al, 2016;, but may also migrate at other times of the year, for example during autumn Jonsson & Jonsson, 2009aPoole et al, 2007;Poole, Whelan, Dillane, Cooke, & Matthews, 1996;Taal et al, 2014;Winter et al, 2016), indicating that the time of seaward migration is highly plastic.…”
Section: Phenotypic Plasticitymentioning
confidence: 99%
“…Most of the catchments are covered in blanket peat and overlie quartzite and schist bedrock. The catchment systems are described as acid oligotrophic and have a low buffering capacity (Byrne et al, 2004). The main land uses are forestry and sheep grazing and the catchments receive an average precipitation of over 2,000 mm per year (Dalton et al, 2010).…”
Section: Study Sites and Characterisationmentioning
confidence: 99%