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Record W7051410834

Peatlands to the Rescue! Late Holocene History of Climate and Storms as Told by Coastal Peatlands on the Magdalen Islands, Québec, Canada

2022· dissertation· en· W7051410834 on OpenAlexaboutno aff

Bibliographic record

VenueSpectrum Research Repository (Concordia University) · 2022
Typedissertation
Languageen
FieldPhysics and Astronomy
TopicMagnetic confinement fusion research
Canadian institutionsnot available
Fundersnot available
KeywordsPeatStormOmbrotrophicHoloceneClimate changeWinter stormPeriod (music)PaleoclimatologyStorm trackGlobal warming
DOInot available

Abstract

fetched live from OpenAlex

Storms are pervasive dangers to coastal communities in Eastern Canada and, under future climate scenarios, these extreme weather events are projected to increase in intensity. However, the impacts of climate change on storm variability have not been studied extensively in this region, in part due to the short and incomplete instrumental storm records. Environmental paleo-data archives recording high-impact storms on multi-centennial to multi-millennial timescales can provide invaluable information to document past storm variabilities and to support and inform adaptation strategies. First, a review of the literature on paleo-storm studies from the North Atlantic was conducted. Then, a reconstruction of late Holocene environmental changes and storms is presented, based on the analyses of two ombrotrophic peat cores from the Magdalen Islands, Québec, in the Gulf of St. Lawrence. The cores were dated by 14C and 210Pb, with the bottommost peat dating to ~4920 BP and ~4720 BP. We used a multi-proxy approach based on sedimentological and geochemical analysis to examine the evolution of the peatlands, as well as local climate on the Magdalen Islands during the past 4000 years, and to reconstruct storms during the past 1000 years, i.e., the period for which both cores display clear ombrotrophic conditions. The storm reconstruction was validated using the hurricane record from the Magdalen Islands over the past 150 years, and shows a particularly active period between 1400-1650 CE, when heightened activity was also identified in other studies from the northwestern North Atlantic, as well as a notable increase in storms since 1930 CE. While warm sea-surface temperature (SST) anomalies seem to have contributed to more frequent storms since 1930 CE, the 1400-1650 CE active period occurred during the Little Ice Age (LIA), a period of generally cooler SSTs in the North Atlantic. Our study is the first to use ombrotrophic peat cores to track storm frequency in eastern North America, as well as one of the northernmost paleotempestological studies on the continent. Future research should focus on understanding the climatic factors that control storm variation in Eastern Canada, especially over the last millennium.

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: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.012
Threshold uncertainty score0.085

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.002
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0030.000

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 head0.010
GPT teacher head0.229
Teacher spread0.219 · 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 designObservational
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
Published2022
Admission routes1
Has abstractyes

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