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Record W4405448523 · doi:10.1093/jrsssc/qlae082

Alexa A. Sochaniwsky and Paul D. McNicholas’s contribution to the Discussion of ‘Inference for extreme spatial temperature events in a changing climate with application to Ireland’ by Healy et al.

2024· article· en· W4405448523 on OpenAlexaff
Alexa A. Sochaniwsky, Paul D. McNicholas

Bibliographic record

VenueJournal of the Royal Statistical Society Series C (Applied Statistics) · 2024
Typearticle
Languageen
FieldEnvironmental Science
TopicAtmospheric and Environmental Gas Dynamics
Canadian institutionsMcMaster University
FundersHorizon 2020 Framework ProgrammeCenter for Research and Development in Mathematics and ApplicationsScience Foundation IrelandEuropean Commission
KeywordsInferenceClimate changeGeographySociologyEpistemologyPhilosophyGeologyOceanography

Abstract

fetched live from OpenAlex

We congratulate the authors on an interesting and timely contribution. In addition to being a valuable contribution to an important conversation, the use of the generalized Pareto distribution (GPD) in this manner sparks ideas about extensions. In addition to a couple of straightforward questions, our comments focus on a possible extension of this work using hidden Markov models (HMMs) to identify extreme spatial temperature events for climate data analysis. The notion of an ‘extreme temperature’, whilst important, is both subjective and location specific. The United Nations gives some examples of how one may characterize an extreme temperature.1 Can the authors please clarify what exactly they consider an extreme temperature in Ireland during the period in question and to what extent, if any, the threshold varies over time? Presumably, the station data would allow for more significant discovery when used altogether rather than using individual weather station data alone. If so, a longitudinal HMM with a GPD may be effective for the identification of extreme temperature events. HMMs with a GPD have been developed for various time series datasets, including work by Kordnoori et al. (2019), Pender et al. (2016), and Deidda (2010). In fact, Pender et al. (2016) and Deidda (2010) have developed HMMs to capture extreme streamflow and rainfall events, respectively. Gaussian longitudinal HMMs have been developed (e.g. Maruotti, 2011) and other advances have been made but, as far as we know, a longitudinal HMM with the GPD has not yet been developed. Additionally, findings from this work could inform the degree of parameter pooling and parameter initializations in such a model. Regarding the latter, occurrence rates of high threshold exceedances in temperature could inform the initialization of the transition matrix and the initial state probability distribution. Regarding pooling, the number of parameters that need to be estimated in a longitudinal HMM varies vastly depending on subject dependence or, in the context of these data, the spatial dependence. Complete independence or dependence of the weather stations would most likely be an unreasonable assumption for these data; however, partial pooling, where weather stations share parameter estimates—potentially, by region—might balance error and accuracy with computational cost. Conflicts of interest: none declared. Not applicable. The author replied later in writing as follows:

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)0.008
metaresearch head score (Gemma)0.081
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Not applicable · Consensus signal: Not applicable
GenreCandidate signal: Commentary · Consensus signal: Commentary
Teacher disagreement score0.015
Threshold uncertainty score0.041

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0080.081
Meta-epidemiology (narrow)0.0010.001
Meta-epidemiology (broad)0.0010.002
Bibliometrics0.0020.002
Science and technology studies0.0020.004
Scholarly communication0.0060.009
Open science0.0030.003
Research integrity0.0080.012
Insufficient payload (model declined to judge)0.0100.005

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 head0.004
GPT teacher head0.227
Teacher spread0.224 · 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 designNot applicable
Domainnot available
GenreCommentary

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
Published2024
Admission routes1
Has abstractyes

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