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Record W4416773151 · doi:10.1002/hyp.70329

Beach Infiltration and Morphodynamics Revealed Through Multi‐Depth Sediment Temperatures

2025· article· en· W4416773151 on OpenAlexafffundabout
Julia A. Cantelon, Craig B. Lake, Barret L. Kurylyk

Bibliographic record

VenueHydrological Processes · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicOceanographic and Atmospheric Processes
Canadian institutionsDalhousie University
FundersCanadian Geophysical UnionKillam TrustsCanada Research ChairsNatural Sciences and Engineering Research Council of CanadaCanadian Water Resources AssociationGeological Society of AmericaParks CanadaAmerican Geophysical UnionOcean Frontier InstituteMarine Environmental Observation Prediction and Response Network
KeywordsBeach morphodynamicsSedimentInfiltration (HVAC)Hydrology (agriculture)SeawaterSediment transportPore water pressure

Abstract

fetched live from OpenAlex

ABSTRACT Seawater flooding on sandy beaches can mobilise sediments, elevate water tables, and salinize fresh groundwater, driving complex fluid, solute, and heat fluxes that are challenging to monitor. While past studies have assessed vertical saltwater intrusion, they seldom consider the thermal dynamics of beach sediments or how temperature signals can yield insights into other coastal dynamics. This study examines the influence of seawater flooding and erosion/accretion on beach sediment temperature dynamics to identify distinct thermal signatures for future quantitative applications of heat as a tracer of coastal zone dynamics. Over 1 year of multi‐depth beach sediment temperature, groundwater level, and electrical conductivity data collected on Sable Island, Canada, reveal the influence of meteorologic, oceanic, hydrogeologic, and morphologic drivers on beach thermal regimes. Meteorological forcing expectedly exerts a dominant diurnal and seasonal control on shallow sediment temperatures in clear conditions. During seawater flooding, shallow sediment temperatures rapidly change to equilibrate with local sea surface temperatures as seawater infiltration drives ‘thermal plug flow’ due to advection‐dominated heat transport. Winter floods warm beach sediments while spring floods cool beach sediments, revealing seasonally distinct thermal disturbances due to flooding. Beach morphodynamics influence the propagation of sediment temperature dynamics because erosion (accretion) increases (decreases) the amplitude ratios between sediment temperatures at the surface and a fixed subsurface elevation. Thermal consonance timing (TCT) and an analytical solution to the one‐dimensional heat diffusion equation yield time series of morphologic evolution that match manual measurements. Complex temperature signals from moisture, salinity, and thermal dynamics limit the applicability of established heat tracing approaches for quantifying vertical porewater fluxes in beaches; however, distinct thermal signatures help qualitatively trace seawater flooding and erosion/accretion. Results lay the foundation for future quantitative algorithms that use heat to infer concurrent beach morphodynamics and groundwater fluxes and their influence on biogeochemical processes and coastal ecosystem functioning.

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)0.000
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 score0.146
Threshold uncertainty score0.291

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
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 head0.015
GPT teacher head0.240
Teacher spread0.225 · 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
Published2025
Admission routes3
Has abstractyes

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