Abstract

Changes in snow and ice conditions are some of the most distinctive impacts of global warming in cold temperate and Arctic regions, altering the environment during a critical period for survival for most animals. Laboratories studies have suggested that reduced ice cover may reduce the survival of stream dwelling fishes in Northern environments. This, however, has not been empirically investigated in natural populations in large rivers. Here, we examine how the winter survival of juvenile Atlantic salmon in a large natural river, the River Alta (Norway, 70°N), is affected by the presence or absence of surface ice. Apparent survival rates for size classes corresponding to parr and presmolts were estimated using capture-mark-recapture and Cormack-Jolly-Seber models for an ice-covered and an ice-free site. Apparent survival (Φ) in the ice-covered site was greater than in the ice-free site, but did not depend on size class (0.64 for both parr and presmolt). In contrast, apparent survival in the ice-free site was lower for larger individuals (0.33) than smaller individuals (0.45). The over-winter decline in storage energy was greater for the ice-free site than the ice-covered site, suggesting that environmental conditions in the ice-free site caused a strong depletion in energy reserves likely affecting survival. Our findings highlight the importance of surface ice for the winter survival of juvenile fish, thus, underpinning that climate change, by reducing ice cover, may have a negative effect on the survival of fish adapted to ice-covered habitats during winter.

Highlights

  • In seasonal temperate environments, changes in snow and ice conditions are one of the most distinct impacts of global warming (Smol et al 2005; Kausrud et al 2008)

  • The apparent survival probability was greater in the icecovered site (Φ = 0.64 for both parr and presmolts) than in the ice-free site (Fig 4)

  • Specific energy and movements Condition factor declined between mark and recapture for both size classes at both sites (Mann–Whitney U-tests: ice-covered site, parr P < 0.001, presmolts P < 0.001; icefree site, parr P = 0.005, presmolts P < 0.001) (Fig 5)

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Summary

Introduction

Changes in snow and ice conditions are one of the most distinct impacts of global warming (Smol et al 2005; Kausrud et al 2008). Surface ice may prevent the formation of anchor ice (Power et al 1993; Roussel et al 2004) Both historical time-series and future scenario modeling emphasize reduction in ice cover in Northern hemisphere watersheds as one of the major responses to global warming (Magnuson et al 2000; Dibike et al 2011). This reduction in ice cover may impact on salmonids by increasing metabolic activity and reducing energy intake, thereby causing a depletion of energy stores.

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