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Record W1966991368 · doi:10.3137/ao.460303

Glacial inceptions: Past and future

2008· article· en· W1966991368 on OpenAlexaffvenueabout
Lawrence A. Mysak

Bibliographic record

VenueATMOSPHERE-OCEAN · 2008
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsMcGill University
FundersEuropean Geosciences UnionEuropean Commission
KeywordsMilankovitch cyclesGlacial periodClimatologyPaleoclimatologyClimate stateClimate modelGeologyNorthern HemisphereClimate changeEffects of global warmingGlobal warmingOceanographyPaleontology

Abstract

fetched live from OpenAlex

Abstract The realistic simulation of northern hemisphere glacial inceptions, which occurred during the Quaternary period, has challenged scores of climate theoreticians and modellers. After reviewing the Milankovitch theory of glaciation, a number of earlier modelling studies of the last glacial inception (LGI) which have employed either high‐resolution General Circulation Models (GCMs) or Earth system Models of Intermediate Complexity (EMICs) are described. The latter class of models has been developed over the past two decades in order to investigate the many interactions and feedbacks among the geophysical and biospheric components of the Earth system that take place over long time scales. Following a description of the McGill Paleoclimate Model (MPM) and other EMICs, some recent McGill simulations of the LGI in response to orbital (Milankovitch) and radiative (atmospheric CO2) forcings are presented. Special attention is given to determining the relative roles of the ocean's thermohaline circulation, freshwater fluxes into the ocean, orography, cryospheric processes and vegetation dynamics during the inception phase. In particular, it is shown that with the vegetation‐albedo feedback included in the model, the buildup of ice sheets over North America is larger than over Eurasia, in agreement with observations. This paper concludes with a discussion on the (possible) occurrence of the next glacial period. To address this issue, which has been inspired by recent publications of Berger and Loutre, MPM simulations of the climate for the next 100 kyr, forced by various prescribed atmospheric CO2 levels, as well as the future insolation changes as calculated by the Berger algorithm, are presented. The influence of a near‐term global warming scenario on glacial inception is also examined. If it is assumed that after such a warming scenario the concentration of CO2in the atmosphere returns to pre‐industrial levels (in the range of 280–290 ppm), then the MPM predicts that the next glacial would start at around 50 kyr after present, which is consistent with the results of Berger and Loutre. Finally, recent simulations of future glacial inceptions using the Potsdam EMIC which includes an atmosphere‐ocean carbon cycle component are described. From one of these simulations in which 5000 GtC are released into the atmosphere due to human activities, it is concluded that the current interglacial will last for at least another half‐million years because of the limited ability of the oceans to absorb such a large carbon release to the atmosphere.

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 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)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.024
Threshold uncertainty score0.996

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0010.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0050.001

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 head0.224
Teacher spread0.210 · 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 teacher head, not a consensus.

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

Citations19
Published2008
Admission routes3
Has abstractyes

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