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Record W4408428649 · doi:10.5194/egusphere-egu25-13727

Rising temperatures will drive summer streamflow droughts and threaten Chinook salmon habitat throughout western North America

2025· preprint· en· W4408428649 on OpenAlexaff
Sacha Ruzzante, Marta E. Ulaski, Tom Gleeson

Bibliographic record

Venuenot available
Typepreprint
Languageen
FieldEnvironmental Science
TopicFish Ecology and Management Studies
Canadian institutionsOcean Networks Canada SocietySimon Fraser UniversityUniversity of Victoria
Fundersnot available
KeywordsChinook windStreamflowHabitatFisheryGeographyEnvironmental scienceClimatologyEcologyFish <Actinopterygii>OncorhynchusBiologyGeologyCartography

Abstract

fetched live from OpenAlex

Chinook salmon (Oncorhynchus tshawytscha) are a keystone species for many ecosystems of western North America, are culturally and spiritually significant for many Indigenous Peoples, and underpin a multi-million dollar industry. However, in recent years extreme summer streamflow droughts have disrupted Chinook migration and rearing patterns. Climate change is driving hydrologic changes throughout the region, but future changes to summer low flows remain highly uncertain. Here we study 375 near-natural catchments throughout the habitat range of Chinook salmon from California to Alaska. The streams span rainfall-dominated, hybrid, snowmelt-dominated, and glacial regimes. Summer discharge has decreased in most catchments, with rainfall-dominated and hybrid catchments seeing the most severe declines.We develop linear regression models which outperform existing process-based models, and project changes to 2100 under four emissions scenarios. Summer low flows have historically been primarily driven by variability in summer precipitation and moderately influenced by winter snow accumulation and summer temperature. However, we find that future changes will probably be driven by rising temperatures because future summer temperatures could greatly exceed the historical envelope of variability. Some further declines in low flows are probably inevitable in rainfall-dominated and hybrid catchments: under a low-emissions scenario, low flows will continue to decline to mid-century but then stabilize. Under a high-emissions scenario, 1-in-50-year low flows could occur almost every summer in many rainfall and hybrid catchments. In glacial catchments summer discharge has been relatively stable in recent years because increased glacial meltwater flows have compensated for increased evapotranspiration. However, many of these glaciers are projected to disappear within 20 to 30 years, and we project severe declines in summer streamflow when this does occur.Many populations of Chinook rear or migrate during the summer months for which we project extraordinary future streamflow droughts. It is unknown whether Chinook populations can shift their life stage timing or find alternate habitats quickly enough to avoid catastrophic impacts. Bold climate action and local mitigation strategies are urgently required to safeguard this ecologically, culturally, and economically vital species against future extreme events.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Simulation or modeling · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.184
Threshold uncertainty score0.366

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.009
GPT teacher head0.247
Teacher spread0.238 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designSimulation or modeling
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations0
Published2025
Admission routes1
Has abstractyes

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