Abstract

The commercially important Norwegian spring spawning herring is characterized by its extensive annual migrations and, on a decadal timescale, large shifts in migration patterns. These changes are not well understood, but have previously been linked to temperature, food availability, and size and age composition of the stock. Acoustic and trawl data from the International Ecosystem Surveys in the Nordic Seas, carried out annually in May since 1996, were used to analyze the spatial distribution of herring in the period 1996–2020. The dataset was disaggregated into age classes, and information about where the different age classes feed in May was derived. The analysis of herring feeding patterns in May confirms that the youngest age classes are generally found close to the Norwegian shelf, whereas the older age classes display larger variations in where they are distributed. During the period 1996–1998, the oldest age classes were found in the central and western Norwegian Sea. During the period 1999–2004, the whole stock migrated north after spawning, leaving the regions in the southern Norwegian Sea void of herring. Since 2005 the oldest herring has again congregated in the south-western Norwegian Sea, in the frontal zone between the cooler East Icelandic water and the warmer Atlantic water. There was a significant positive relationship both between stock size and distribution area and between stock size and density. Moreover, it is likely that the strong year classes 1991/1992 and 1998/1999, which were relatively old when the respective changes in migration patterns occurred, were important contributors to the changes observed in 1999 and 2005, respectively.

Highlights

  • IntroductionThe Norwegian spring spawning herring (hereafter herring) stock varies greatly, both in size and distribution area

  • The Norwegian spring spawning herring stock varies greatly, both in size and distribution area

  • In 2008–2009 the stock reached its maximum size since the 1950s, after which it has declined again (Dragesund, 1980; Dragesund et al, 1997; ICES, 2021b)

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Summary

Introduction

The Norwegian spring spawning herring (hereafter herring) stock varies greatly, both in size and distribution area. The stock started to grow again in the late 1980s after the strong 1983 year class recruited, and in the mid 1990s the herring reoccupied large parts of the Norwegian Sea following good recruitment in the early 1990s. Since the reappearance of the stock in the Norwegian Sea (Figure 1), spawning has occurred along the Norwegian coast from around 62◦30 N to 68◦20 N (Holst and Slotte, 1998; Salthaug et al, 2020). The mature part of the stock starts its feeding migration. As prior to the stock collapse in the 1960s, the main feeding is in the Norwegian Sea and adjacent waters (Marti, 1956; Misund et al, 1997; Nøttestad et al, 1999; ICES, 2021b). Since the reappearance, some variation has been observed in the distribution pattern during summer, with a more northerly distribution during the period 1999–2004 as compared to the period prior and after this (Utne et al, 2012; Gudmundsdottir et al, 2014)

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