2021
DOI: 10.5194/essd-13-1807-2021
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A climate index for the Newfoundland and Labrador shelf

Abstract: Abstract. This study presents in detail a new climate index for the Newfoundland and Labrador (NL) shelf. The NL climate index (NLCI) aims to describe the environmental conditions on the NL shelf and in the Northwest Atlantic as a whole. It consists of the average of 10 normalized anomalies, or subindices, derived annually: winter North Atlantic Oscillation, air temperature, sea ice season severity, iceberg count, seasonal sea surface temperature, vertically averaged temperature and salinity at the Atlantic Zo… Show more

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Cited by 22 publications
(24 citation statements)
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References 21 publications
(16 reference statements)
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“…Indeed, 55% of interviewees that shared knowledge about deep-water spawning also noted shifts between beach and deep-water habitat use among years and 94% of these interviewees stated temperature was the primary factor causing these shifts. However, as water temperatures were similar during 2018 and 2019, and were warmer relative to the local long-term average (Cyr and Galbraith, 2021;DFO, 2021), we would expect extensive use of deep-water spawning sites because beaches may have been too warm (≥ 12°C) later in the summer. Therefore, temperature was likely not a limiting factor for detecting deep-water spawning sites in our study.…”
Section: Discussionmentioning
confidence: 99%
“…Indeed, 55% of interviewees that shared knowledge about deep-water spawning also noted shifts between beach and deep-water habitat use among years and 94% of these interviewees stated temperature was the primary factor causing these shifts. However, as water temperatures were similar during 2018 and 2019, and were warmer relative to the local long-term average (Cyr and Galbraith, 2021;DFO, 2021), we would expect extensive use of deep-water spawning sites because beaches may have been too warm (≥ 12°C) later in the summer. Therefore, temperature was likely not a limiting factor for detecting deep-water spawning sites in our study.…”
Section: Discussionmentioning
confidence: 99%
“…We considered including the role of (1) climatic variability on habitat availability and predator–prey overlap using the Newfoundland and Labrador (NL) climate index (NLCI; Cyr & Galbraith, 2021), mean normalized anomalies of the spring bottom‐water temperature derived from multiple data sources (Cyr et al., 2021), and the mean normalized anomalies of the summer cold‐intermediate layer (CIL) area over hydrographic sections on the NL shelf (Cyr & Galbraith, 2021), (2) prey availability using a time series of capelin biomass (Koen‐Alonso et al., 2021) and northern sand lance abundance (Robertson, Koen‐Alonso, et al., 2022) and (3) a potential competitor for food and habitat, thorny skate using a survey time series of estimated biomass for this species (Simpson et al., 2018).…”
Section: Methodsmentioning
confidence: 99%
“…To illustrate the modelling framework, we applied it to assess the population and ecosystem processes that affected the differential recovery of two flatfish populations on the Newfoundland Grand Banks (Northwest Atlantic Fisheries Organization [NAFO] Divisions 3LNO) over the past three decades. In response to prolonged intense fishing pressure and a period of anomalous environmental conditions (e.g., record low temperatures; Cyr & Galbraith, 2021), fish community biomass on the Newfoundland Grand Banks collapsed in the early 1990s (Dempsey et al., 2017). Since this collapse, yellowtail flounder ( Limanda ferruginea , Pleuronectidae) has recovered while American plaice ( Hippoglossoides platessoides , Pleuronectidae) has remained at a low population level.…”
Section: Grand Bank Applicationmentioning
confidence: 99%
“…Largest TA values, reaching nearly as high as reach 2400 µmol kg −1 , are found within the upper 150 m of the southern NL and Scotian slope waters. Following the seasonal cycle of salinity, TA generally decreases from spring to summer/fall on the NL/Scotian Shelves, reflecting respectively the continued freshening of the NL coast (Cyr and Galbraith, 2021) and the freshwater export from the LSLE exiting the Gulf of St. Lawrence at Cabot Strait (Dever et al, 2016). Although the TA of the Atlantic Zone bottom waters follows a similar spatial pattern as the surface, the values are higher and the range is much narrower (Figure 7b).…”
Section: Total Alkalinitymentioning
confidence: 95%