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Record W6929233223 · doi:10.48336/hjf0-b309

The impacts of glacial runoff and pCO₂ on centennial-to millennial-scale climate variability during the last glacial cycle

2022· article· en· W6929233223 on OpenAlexaff

Bibliographic record

VenueMemorial University Research Repository (Memorial University) · 2022
Typearticle
Languageen
FieldEnvironmental Science
TopicFecal contamination and water quality
Canadian institutionsMemorial University of Newfoundland
Fundersnot available
KeywordsFreshwater ecosystemClimate changeGlacial periodAbrupt climate changeSurface runoffClimate modelWater cycleClimate oscillationGlacier

Abstract

fetched live from OpenAlex

Freshwater is hypothesized to have a critical role in previous centennial-to millennial-scale climate variability(CMCV),e.g. Dansgaard Oeschger events, the Younger Dryas, and may play a central role in future climate change as ice sheet and glacier melt accelerates. Similarly, anthropogenic climate change demonstrates the need to understand the impact of carbon dioxide (pCO₂) on climate variability. The relationship between freshwater and rapid climate change in the paleoclimate records has been a subject of intense study, but past approaches have generally relied upon an approximation of freshwater entering the oceans via wide bands in the North Atlantic in `hosing' experiments. This design element of hosing experiments, which supports the relationship between freshwater and climate cooling, artificially amplifies the climate response by introducing freshwater directly over sites of deep water formation. As well, previous studies have yet to characterize the role of either pCO₂ or freshwater on CMCV under appropriate boundary conditions. This thesis explores the impact two likely controls of CMCV, freshwater and pCO₂ concentrations. I achieve this by first determining where coastally released freshwater is transported using an eddy permitting ocean model configured for the the Younger Dryas interval during the last deglaciation. It is found that by explicitly resolving features important for the transport of coastally released freshwater, such as mesoscale eddies, that hosing overestimates the amount of freshwater transported to sites of deepwater formation by 2-4x. Next, using these results I then derive a novel method of freshwater injection, the freshwater fingerprint, and examine the relative climate impact of different freshwater injection distributions. In comparing the fingerprint method against both conventional band hosing and regional injection methods I conclude that the fingerprint methodology allows for emulation of some features of the eddy permitting representation in a coarse resolution coupled climate model. Finally, I examine the impact that pCO₂ and freshwater has on a specific form of CMCV, Dansgaard-Oeschger events during Marine Isotope Stage 3 (MIS3), with boundary conditions consistent with the MIS3 interval. When examining characteristics of CMCV I find that both increasing freshwater and decreasing carbon dioxide levels lead to similar changes in interstadial & stadial durations.

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)0.001
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 score0.014
Threshold uncertainty score0.028

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
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 science0.0000.001
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 head0.013
GPT teacher head0.235
Teacher spread0.222 · 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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