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Record W2286848708

Where, how fast, and why arctic permafrost coasts undergo coastal erosion?

2010· article· en· W2286848708 on OpenAlexaboutno aff
Hugues Lantuit, Pier Paul Overduin

Bibliographic record

VenueHelmholtz-Zentrum für Polar-und Meeresforschung (Alfred-Wegener-Institut) · 2010
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicClimate change and permafrost
Canadian institutionsnot available
Fundersnot available
KeywordsPermafrostArcticThermokarstCoastal erosionArctic ecologyErosionOceanographyStormPhysical geographyGlobal warmingClimate changeGeologyEnvironmental scienceGeographyGeomorphology
DOInot available

Abstract

fetched live from OpenAlex

Permafrost coasts represent 34 % of the global coastline and are likely to become one of the most impacted environments of the Earth under changing climate conditions. The lengthening of the open-water season and the increasing open-water area, the warming of permafrost, the increasing occurrence of coastal thermokarst, and the increase in sea surface temperatures are all thought to impact the pace of coastal erosion. In particular, storms are predicted to hit the coasts later in the fall season. These storms are thought to bear staggering threats to the coasts in the form of destruction of community and industry infrastructure as well as dramatic changes in sedi-ment and nutrient pathways in the nearshore zone. Alas, there is little data available to provide a cir-cumarctic picture of coastal erosion and to indicate erosion trends. Indeed, arctic coasts remain largely unknown and unexplored, which puts current adap-tation and mitigation strategies in northern commu-nities into jeopardy.In this presentation, we present the latest results from the Arctic Coastal Dynamics project, initiated by the International Permafrost Association and the International Arctic Science Committee in 1999. A classification, built to consistently describe the geo-morphological characteristics and processes ob-served at the coast along the arctic rim, indicates that the geomorphological setting of arctic coasts is highly spatially variable. This dataset highlights the major influence of this setting on the erosion rates observed and the in fine difficulty in providing sta-tistics at the global level. It shows, however that some striking regional traits can be deduced from the dataset. Alaskan and Canadian coasts in the Beaufort Sea are characterized by larger ground ice contents but also by much smaller cliff heights than other arctic coasts. Overall it shows that circumpolar coastal erosion is on average 0.5 m/yr, but again with strong differences between arctic regions, with rates close to 10 m/yr in some areas and stable coasts in others. A second outcome of the ACD project is a recent as-sessment of erosion rates and their evolution throughout the second half of the twentieth century and the beginning of the twenty-first century. Despite the recent media attention to coastal erosion, reliable long-term datasets asserting an increase in coastal erosion are scarce in the Arctic. This presen-tation will present the latest datasets published in the literature and compare their spatial coverage to the extent of permafrost coasts at the arctic scale.

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)0.001
metaresearch head score (Gemma)0.003
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 score0.054
Threshold uncertainty score0.108

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0010.003
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.003
Science and technology studies0.0010.000
Scholarly communication0.0030.001
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 head0.019
GPT teacher head0.246
Teacher spread0.227 · 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

Citations1
Published2010
Admission routes1
Has abstractyes

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