2015
DOI: 10.1073/pnas.1513511112
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Shifting patterns in Pacific climate, West Coast salmon survival rates, and increased volatility in ecosystem services

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Cited by 19 publications
(20 citation statements)
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“…Extreme events are, by definition, rare but are also predicted to increase rapidly in the future if gradual trends in average conditions are accompanied by greater climatic variability (Jentsch et al 2007). That dynamic could unfold for northwestern rivers if the long-term warming trends we document begin to interact with climatically enhanced variability in the North Pacific Ocean (Mantua 2015;Di Lorenzo and Mantua 2016). In some late-century scenarios for the Snake and Columbia rivers, for example, it has been predicted that the number of weeks with average temperatures exceeding 21°C could increase 10-fold relative to historical baselines (Mantua et al 2010).…”
Section: Biological Effectsmentioning
confidence: 84%
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“…Extreme events are, by definition, rare but are also predicted to increase rapidly in the future if gradual trends in average conditions are accompanied by greater climatic variability (Jentsch et al 2007). That dynamic could unfold for northwestern rivers if the long-term warming trends we document begin to interact with climatically enhanced variability in the North Pacific Ocean (Mantua 2015;Di Lorenzo and Mantua 2016). In some late-century scenarios for the Snake and Columbia rivers, for example, it has been predicted that the number of weeks with average temperatures exceeding 21°C could increase 10-fold relative to historical baselines (Mantua et al 2010).…”
Section: Biological Effectsmentioning
confidence: 84%
“…; Feist et al. ), and less‐favorable ocean conditions (Mantua ; Di Lorenzo and Mantua ) to negatively affect coldwater fishes. For some populations or fisheries that are heavily exposed and vulnerable, an additional 1–3°C of warming accompanied by those changes may well prove to be the road to ruin.…”
Section: Resultsmentioning
confidence: 99%
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“…T he Pacific Decadal Oscillation (PDO) and El Niño Southern Oscillation (ENSO) are recurring patterns of climate variability centered over the northeastern (NE) and equatorial Pacific, respectively, that fluctuate at scales of years (ENSO) to decades (PDO) (1,2). Distinct, yet also related, these patterns can amplify or dampen each other through atmospheric teleconnection (1,3).…”
mentioning
confidence: 99%
“…In the NE Pacific, they induce similar spatial patterns of sea surface temperature anomalies during positive (warm) and negative (cool) phases (4). Low-frequency physical variability attributed to the PDO and ENSO modulates large shifts in NE Pacific water temperature, ocean currents, and foodweb dynamics that can persist for months to years (2,5,6). Shifts in NE Pacific plankton communities occur as well (7)(8)(9)(10)(11)(12); however, climate impacts on phytoplankton ecology in this region are relatively underexplored, largely due to a lack of phytoplankton data at sufficient scales.…”
mentioning
confidence: 99%