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Record W4249121031 · doi:10.5860/choice.50-3866

Ice ages and interglacials: measurements, interpretation and models

2013· article· en· W4249121031 on OpenAlexaboutno aff

Bibliographic record

VenueChoice Reviews Online · 2013
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsnot available
Fundersnot available
KeywordsInterglacialInterpretation (philosophy)GeologyIce agePhysical geographyPaleontologyGlacial periodGeographyPhilosophyLinguistics

Abstract

fetched live from OpenAlex

The typical description of the past 800,000 years would be that the Earth has experienced about nine major periods of glaciation ("Ice Ages") spaced at various intervals ranging from 0.9 my to 1.1 my (see Fig. 8.23).This presupposes that Ice Ages are unusual departures from normalcy.Actually, it appears as if the natural state of the Earth during this period was an Ice Age, but there were about nine interruptions of the glacial state, during which the Arctic climate was much warmer for time periods of the order of 10,000 years or so.Each Ice Age required many tens of thousands of years to develop to its maximum state of glaciation.During the last glacial maximum, some 20,000 years ago, Canada and the northern USA were blanketed by huge ice sheets, up to 4 km in thickness.In addition, there was a large ice sheet covering Scandinavia that reached down into Northern Europe.The Antarctic ice sheet was somewhat more extensive than today.Local glaciations existed in mountainous regions of North America, Europe, South America and Africa, driving the tree line down by up to 700-800 m.The temperature of Greenland was lower by up to 20 °C, but the climate was probably only a few degrees colder than normal in the tropics.Conditions were very harsh 20,000 years ago at the last glacial maximum (LGM).These ice sheets tied up so much of the Earth's water that more than 150 m of ocean was removed.As a result, the shorelines of the continents moved outward by a considerable distance.The Beringia land bridge from Siberia to Alaska was created, allowing animals and humans to cross from one continent to the other.In the upper-mid latitudes, the climates were semi-arctic and the flora shifted to tundra.Humidity was reduced, and many lands dried out.At the LGM, the CO 2 concentration dropped below 200 ppm, and this combined with cold, led to plant starvation and desertification of marginal areas.The sharp temperature discontinuity at the edges of the ice sheets generated violent winds that swept up dust and dirt from dry regions, filling the atmosphere with dust.Dust deposited on the ice sheets preceded each termination of an Ice Age, allowing much greater solar absorption and the demise of the ice sheets.This last Ice Age began to wane around 17,000 years ago and dissipated through a series of gyrating climate oscillations, ending in a comparatively benign period that has lasted for the past *10,000 years, called the Holocene.

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)0.001
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation 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 score0.117
Threshold uncertainty score0.669

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
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 head0.101
GPT teacher head0.320
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 teacher head, 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

Citations2
Published2013
Admission routes1
Has abstractyes

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