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Record W7105651414 · doi:10.24400/527896/a03-2018.2602

Pathways, impacts and fate of marine debris generated by the 2011 tsunami in Japan, derived from a synthesis of numerical models and observational reports

2018· article· W7105651414 on OpenAlexaboutno aff

Bibliographic record

VenueCentre National d’Etudes Spatiales · 2018
Typearticle
Language
FieldEnvironmental Science
TopicOil Spill Detection and Mitigation
Canadian institutionsnot available
Fundersnot available
KeywordsDebrisMarine debrisShoreNumerical modelsOcean currentEast coastLagrangianCurrent (fluid)

Abstract

fetched live from OpenAlex

March 11, 2011 tsunami devastated the east coast of Japan and produced millions of tons of marine debris that drifted across the North Pacific. The extraordinary amount and unusual composition of tsunami debris allowed to trace its drift across the ocean and arrivals on remote shores and helped to better understand the pathways of floating marine debris. A suite of ocean models synthesized with these observations produced most complete picture of the debris dynamics, pathways, and fate. While observations allowed to optimize such model parameters as windage and source distribution, the models filled large gaps in sparse observations and produced estimates of the total budgets. For example, the study suggests that the original number of boats lost to the tsunami was about 1,000 and about 100 of these boats may be still floating in the ocean. Detailed analysis of model fluxes on the US/Canada West Coast and their comparison with reports of tsunami boats from the same region revealed serious difficulties that even best OGCMs (Ocean General Circulation Models), such as the HYCOM (Hybrid Coordinate Model, operated by the US Navy and used for coordination of such operational activity as oil spill response), have serious problems with reproducing even main peaks in observations. The best correspondence was achieved in a simple diagnostic model (SCUD), whose coefficients were optimized using historical data of satellite altimetry, scatterometry and trajectories of Lagrangian floats (Figure). In this presentation we discuss methods available to numerically study the drift of marine debris (particles versus tracer), to calibrate/validate models using sparse observational data and to maximize the utility of satellite and model products in various applications. Figure. Model fluxes on the North America west coast between 40 and 51N as function of time and windage. Rows (from top to bottom) correspond to SCUD (a and f), SCUD-HYCOM (b and g), MOVE (c and h), FORA (d and i), and GNOME (e and j) models. Left column shows original model fluxes and right column same fluxes smoothed in time with a Gaussian 1.5-month half-width filter. White dots and lines mark peaks in model fluxes for different windages. Vertical magenta lines mark five main peaks in observations. Horizontal grey lines mark the optimal windage parameter values, derived from model comparison with boat reports, and span over the periods of the comparison. Color scale is strongly nonlinear and model flux units are fraction of the released tracer per a year. White dashed line in (d) illustrates faster drift and earlier arrival of higher windages.

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 score0.207
Threshold uncertainty score1.000

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 studies0.0000.001
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 head0.028
GPT teacher head0.227
Teacher spread0.199 · 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

Citations0
Published2018
Admission routes1
Has abstractyes

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