Fish and Fisheries in Estuaries. Группа авторов

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figure 1)).

      For the anadromous alosine Alosa sapidissima in the Connecticut River (USA), a Ricker model fitted to spawner abundance explained little of the observed recruitment variability (Crecco & Savoy 1984, Crecco et al. 1986). Including a freshwater‐discharge variable in the S‐R model improved the modelled result (r 2 increased from 0.02 to 0.26). This relationship, while still far from a reliable predictor of recruitment, convincingly indicated that freshwater discharge (in this case a negative factor) may control recruitment and, in many years, may be more important than abundance of adult spawners.

Schematic illustration of modified Ricker stock–recruitment model.

      (from Houde (2008, his figure 6)).

upper R Subscript y Baseline equals alpha upper S exp left-parenthesis minus beta 1 upper S minus beta 2 upper Delta upper L right-parenthesis plus epsilon Subscript y upper T h e f i t t e d m o d e l i s colon upper R Subscript y Baseline equals 365 upper S exp left-parenthesis minus 0.19 upper S minus 1.35 upper Delta upper L right-parenthesis r squared equals 0.89

      where R y = recruitment level, S = estimated baywide A. mitchilli spawning stock biomass, ΔL = centre of latitudinal location of the A. mitchilli spawning stock. A high percentage of the annual variability in recruitment was explained by the modified Ricker model.

       3.4.2.3 Predicting and forecasting recruitment

Schematic illustration of recruitment time series for Sander lucioperca in the Archipelago Sea, Finland.

      (modified from Heikinheimo et al. (2014, their figure 7)).

      The complexity of estuaries and the life cycles of fishes that reproduce in and recruit to estuaries add to the challenge of successful forecasting. The complexity itself suggests that forecasting based on adult abundance alone is insufficient and that environmental variables must be incorporated into analyses and models to account for factors driving recruitment variability. For many estuary‐dependent and ‐associated species in which egg, larval and juvenile stages occupy different habitats, identifying variables and life stages most linked to recruitment variability is particularly challenging. Incorporating freshwater flow and temperature variables into stock‐recruitment models for estuarine‐associated fishes has gained considerable success in predicting recruitments in the past three decades. Two notable examples include the clupeid Brevoortia patronus in the Gulf of Mexico, in which freshwater discharge from the Mississippi River has predictive power (Vaughan et al. 2011) and the sciaenid Micropogonias undulatus along the coast of the northeast USA in which winter temperatures are directly related to recruitment success (Figure 3.17a) (Hare et al. 2010). Predictive models presented in Figures 3.16 and 3.17 for two estuary‐dependent species are good examples of how S‐R models that include adult biomass and environmental variables can be effective for hindcasting but are not necessarily used or effective for forecasting (Haltuch et al. 2019).

      Climate variability in marine ecosystems often is expressed in patterns that dominate for periods of a few years to decades and thus has the potential for predicting and forecasting trends in fish recruitment. Both oscillating climate regimes and directional climate shifts may affect reproduction and recruitment in marine and estuarine fishes (Nye et al. 2014, Gillanders et al. 2022). Using a synoptic climatology approach, inter‐annual recruitment variability in several offshore‐spawning, estuary‐dependent and anadromous fishes was investigated (Wood 2000, Wood & Austin 2009). These analyses indicated considerable potential and ability to hindcast recruitment and to predict probable trends for these species.

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