Mean Annual Discharge and Atlantic Salmon
mbakken
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Species Common Name
Atlantic Salmon
Latin Name (Genus species)
Salmo salar
Stressor Name
Flow
Specific Stressor Metric
Mean Annual Discharge (MAD)
Stressor Units
%
Vital Rate (Process)
Abundance
Life Stage
Season
Winter
Geography
Catamaran Brook, NB, Canada
Detailed SR Function Description
Final curve was derived from a linear regression.
System capacity was derived from smolt totals. This data was gathered using a fish-counting fence near the stream mouth to enumerate the smolts emigrating in the spring. Atlantic salmon smolts are typically age 3 when emigrating.
To normalize and rescale each ecological response, each value was scaled by the maximum ecological response observed in the study such that mean habitat capacity percentage (normalized response) = response / maximum ecological response observed.
Note that mean density in Cataman brook as estimated by digitizing densities from Fig. 2 pg. 512 of Imre et al. 2005.
Implicit pathway of effect: Total Atlantic salmon smolt outmigration in Catamaran Brook is positively associated with higher average winter discharge.
System capacity was derived from smolt totals. This data was gathered using a fish-counting fence near the stream mouth to enumerate the smolts emigrating in the spring. Atlantic salmon smolts are typically age 3 when emigrating.
To normalize and rescale each ecological response, each value was scaled by the maximum ecological response observed in the study such that mean habitat capacity percentage (normalized response) = response / maximum ecological response observed.
Note that mean density in Cataman brook as estimated by digitizing densities from Fig. 2 pg. 512 of Imre et al. 2005.
Implicit pathway of effect: Total Atlantic salmon smolt outmigration in Catamaran Brook is positively associated with higher average winter discharge.
Function Derivation
Observational data. Final curve was derived from linear regression.
Transferability of Function
Appropriate for winter stream flow impacts on Atlantic Salmon smolt. General transferability to other salmon stocks in unclear, but likely appropriate for other autumn-spawning salmonids (i.e., regions with similar hydrology to the Catamaran Brook).
The relationship may be unreliable if extrapolated to a flow range outside the original data (see the Average Salmonid flow-ecology SR function entry based on Rosenfeld and Enright (2025) for a more generalizable function across a wider range of flows).
The relationship may be unreliable if extrapolated to a flow range outside the original data (see the Average Salmonid flow-ecology SR function entry based on Rosenfeld and Enright (2025) for a more generalizable function across a wider range of flows).
Source of stressor Data
The winter streamflow data (discharge) for Catamaran Brook was collected using a streamflow gauging station located in the mid-basin. See methods of Cunjack et al. 2013 for details.
Data was then standardized by dividing absolute flow by MAD to achieve %MAD values (see Rosenfeld & Enright 2024). Such standardization allows for comparison of flow metrics across a wide range of stream sizes (see Rosenfeld et al. 2017).
Data was then standardized by dividing absolute flow by MAD to achieve %MAD values (see Rosenfeld & Enright 2024). Such standardization allows for comparison of flow metrics across a wide range of stream sizes (see Rosenfeld et al. 2017).
Function Type
continuous
Stressor Scale
linear
References Cited
Cunjak, R.A., Linnansaari, T., and Caissie, D. 2013. The complex interaction of ecology and
hydrology in a small catchment: a salmon's perspective. Hydrol. Process. 27: 741-749.
hydrology in a small catchment: a salmon's perspective. Hydrol. Process. 27: 741-749.
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Stressor Response csv data
Data_Atlantic_Flow_Catamaran_Smo_0.csv
(598 bytes)
| PERCENT_MAD | Mean System Capacity (%) | SD | low.limit | up.limit |
|---|---|---|---|---|
| 24.91769231 | 43.9710692 | 0 | 0 | 100 |
| 25.26738462 | 44.0514985 | 0 | 0 | 100 |
| 31.50723077 | 45.4866631 | 0 | 0 | 100 |
| 33.78138462 | 46.0097185 | 0 | 0 | 100 |
| 36.19030769 | 46.5637708 | 0 | 0 | 100 |
| 37.26046154 | 46.8099062 | 0 | 0 | 100 |
| 37.62738462 | 46.8942985 | 0 | 0 | 100 |
| 42.44338462 | 48.0019785 | 0 | 0 | 100 |
| 44.09461538 | 48.3817615 | 0 | 0 | 100 |
| 54.08276923 | 50.6790369 | 0 | 0 | 100 |
| 58.12476923 | 51.6086969 | 0 | 0 | 100 |
| 60.88615385 | 52.2438154 | 0 | 0 | 100 |
| 72.52969231 | 54.9218292 | 0 | 0 | 100 |
| 73.246 | 55.08658 | 0 | 0 | 100 |
| 74.80861538 | 55.4459815 | 0 | 0 | 100 |
| 85.37307692 | 57.8758077 | 0 | 0 | 100 |
| 98.56138462 | 60.9091185 | 0 | 0 | 100 |
Stressor Response Chart
Mean Response
±1 Standard Deviation
Upper/Lower Limits