MétaCan
Menu
Back to cohort
Record W7026367240

Analyse du recul latéral d'un marais salé subarctique sous l'influence d'une structure rigide de protection

2024· other· fr· W7026367240 on OpenAlexfundaboutno aff

Bibliographic record

VenueSémaphore (Université du Québec à Rimouski) · 2024
Typeother
Languagefr
FieldEarth and Planetary Sciences
TopicGroundwater and Isotope Geochemistry
Canadian institutionsnot available
FundersNatural Sciences and Engineering Research Council of Canada
KeywordsBody segmentCoastal zoneStatistical analysis
DOInot available

Abstract

fetched live from OpenAlex

« Les marais salés sont des milieux influencés par divers facteurs comme les conditions météo-océaniques, les apports sédimentaires, les activités humaines et la glace de mer dans les régions froides. Dans l'estuaire du Saint-Laurent au Québec, les communautés côtières font face à des problèmes tels que l'érosion, qui affecte des infrastructures vitales comme les autoroutes. À Rivière-du-Loup, un brise-lames en pierre a été érigé pour protéger à la fois le rivage du marais et l'autoroute. Cette étude examine l'impact de ce brise-lames ainsi que d'autres facteurs comme l'énergie des vagues, la température de l'eau et les conditions locales sur le mouvement latéral du marais salé à Rivière-du-Loup. Une analyse sur la période de 1927 à 2023, combinant les mesures de recul du marais, les données de télédétection et les informations météorologiques, révèle une variabilité significative dans les taux et les schémas d'érosion. La partie nord-est a subi les reculs les plus importants, qui diminuent graduellement vers le sud-ouest, en adéquation avec les variations de densité de végétation de Spartine dans le schorre. Sur les 3,5 km de marais analysés, un recul moyen de 63,10 m a été enregistré depuis 1927. Un recul maximal de 178,5 m est observé, indiquant un taux moyen de recul à long terme de 0,7 ± 0,12 m/an. L'installation du brise lames a entraîné une réduction immédiate de l'impact des vagues dans la zone protégée, réduisant les taux moyens de recul d'environ quatre fois. Le brise-lames induit une diminution de l'énergie des vagues incidentes qui varie considérablement selon le niveau l'immersion du brise-lames, allant de 96% à 66%. Une analyse à court terme révèle des taux de recul plus élevés pendant la saison de fonte des glaces au printemps, mais l'absence prolongée de glace a le plus grand impact cumulatif sur l'érosion. Ces taux sont significativement liés à l'énergie des vagues et au dégel printanier. L'énergie des vagues entraîne principalement le recul de schorre supérieur pendant les périodes sans glace, tandis que le dégel prédomine pendant la saison de fonte des glaces printanière. Pour la gestion du littoral, il importe donc de bien prendre en compte les variabilités saisonnières dans les processus côtiers, car ceux-ci induisent des reculs différents tout au long de l'année. -- Mot(s) clé(s) en français : Marais salés, dynamique côtière, évolution du trait de côte, brise-lames, énergie des vagues, érosion glaciale. »-- « Salt marshes are environments influenced by various factors such as meteo-oceanic conditions, sediment inputs, human activities, and sea ice in cold regions. In the St. Lawrence Estuary in Quebec, coastal communities face issues such as erosion, which affects vital infrastructure like highways. In Rivière-du-Loup, a stone breakwater has been installed to protect both the marsh shoreline and the highway 20. This study examines the impact of this breakwater as well as other factors such as wave energy and local conditions on the lateral movement of the salt marsh at Rivière-du-Loup. An analysis spanning from 1927 to 2023, combining marsh retreat measurements, remote sensing data, and meteorological information, reveals significant variability in erosion rates and patterns. The northeast part experienced the most substantial retreats, gradually decreasing towards the southwest, in line with variations in Spartina vegetation density in the tidal flat. Over the 3.5 km of marsh analyzed, an average retreat of 63.10 m has been recorded since 1927. A maximum retreat of 178.5 m is observed, indicating a long-term average retreat rate of 0.7±0.12 m/yr. The installation of the breakwater led to an immediate reduction in wave impact in the protected area, reducing average retreat rates by about four times. The breakwater induces a decrease in incident wave energy that varies significantly depending on the breakwater immersion level, ranging from 96% to 66%. Short-term analysis reveals higher retreat rates during the spring ice melting season, but the prolonged absence of ice has the greatest cumulative impact on erosion. These rates are significantly linked to wave energy and spring thawing. Wave energy primarily drives marsh retreat during ice-free periods, while thawing predominates during the spring ice melting season. For coastal management, it is essential to consider seasonal variability in coastal processes, as they induce different retreats throughout the year. -- Mot(s) clé(s) en anglais : Saltmarshes, shoreline change, coastal dynamics, breakwater, wave power, glacial erosion. »--

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 score0.753
Threshold uncertainty score0.491

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0020.000

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 head0.005
GPT teacher head0.164
Teacher spread0.159 · 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
Published2024
Admission routes2
Has abstractyes

Explore more

Same venueSémaphore (Université du Québec à Rimouski)Same topicGroundwater and Isotope GeochemistryFrench-language works237,207