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Record W6962975721 · doi:10.17630/sta/1288

Tree rings and volcanoes : the climate of NW North America

2025· article· en· W6962975721 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

aboutThe title or abstract carries a Canadian signal from the geographic lexicon.
no affNo Canadian affiliation: this work is invisible to an affiliation-only frame.
No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Bibliographic record

VenueSt Andrews Research Repository (St Andrews Research Repository) · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicTree-ring climate responses
Canadian institutionsnot available
Fundersnot available
KeywordsContext (archaeology)GloomEctothermPopulation

Abstract

fetched live from OpenAlex

This thesis aimed to refine temperature reconstruction strategies for Northwest North America (NWNA), introducing new applications of the latewood blue intensity parameter (LWBI), and pooling multiple regional datasets to create a new millennial-length temperature reconstruction. Currently, NWNA is underrepresented by long tree records in comparison to Eurasia. Such records are crucial for contextualizing modern warming in the context of past variability. The NWNA region represents the origin of the “Divergence Problem”, a phenomenon referring to the loss/weakening of temperature sensitivity over time. To address this, a strategy was developed, using a network of sites in the southern Yukon, to minimise its impact and optimise the temperature signal. Trees growing within 100m of upper treeline provide the most temporally stable signal, making them the optimal targets for a temperature reconstruction. The successful use of LWBI for developing temperature reconstructions is well-documented, yet its application for dating is less understood. LWBI was utilised to absolutely date the 9th century Mt. Churchill eruption for the first time using dendrochronological techniques, a result not possible using RW. By demonstrating that LWBI can be effectively used for crossdating between species, dated subfossil trees preserved in the volcanic ash placed the eruption between 852-853 CE. The final LWBI reconstruction provided temperature variability for NWNA back to the 3rd century CE. While full period modelling (1901-2014) explained 46% of the temperature variance, the fidelity of the reconstruction reduced significantly prior to 933 CE due to decreased replication and significant underestimation of extreme warm season years was noted. The NWNA BI-based reconstruction demonstrates the most time stable temperature signal compared to other NWNA reconstructions but struggles to capture long term trends. Future research should integrate these data for a multi-parameter reconstruction for a more comprehensive, robust reflection of NWNA temperature variability.

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.

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.005
metaresearch head score (Gemma)0.001
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow), Science and technology studies, Scholarly communication, Research integrity
Consensus categoriesScience and technology studies
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.087
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0050.001
Meta-epidemiology (narrow)0.0010.000
Meta-epidemiology (broad)0.0010.000
Bibliometrics0.0020.003
Science and technology studies0.0040.004
Scholarly communication0.0010.001
Open science0.0020.001
Research integrity0.0000.002
Insufficient payload (model declined to judge)0.0000.000

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 head0.038
GPT teacher head0.322
Teacher spread0.284 · 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