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Record W2084181144 · doi:10.5589/m02-029

Wind direction estimation from SAR images of the ocean using wavelet analysis

2002· article· en· W2084181144 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

venuePublished in a venue whose home country is Canada.
no affNo Canadian affiliation: this work is invisible to an affiliation-only frame.
No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Bibliographic record

VenueCanadian Journal of Remote Sensing · 2002
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicOcean Waves and Remote Sensing
Canadian institutionsnot available
Fundersnot available
KeywordsSynthetic aperture radarWind directionGeologyRemote sensingOrientation (vector space)WaveletGridSmoothingGeodesyComputer scienceWind speedGeographyMeteorologyComputer visionMathematicsGeometry

Abstract

fetched live from OpenAlex

AbstractWe present a method for the automatic estimation of wind directions from synthetic aperture radar (SAR) images of the ocean. The method is based on a wavelet analysis and assumes that the wind direction aligns with boundary-layer atmospheric roll vortices, which often appear as streaks at kilometre scales in SAR images of the ocean, and measures the orientation of the streaks. Unlike estimation methods that use the discrete Fourier transform (DFT), the streaks in SAR images are described quantitatively as a natural output of this method. Furthermore, more optimal wind directions are obtained by comparing the directional orientation of the streaks at different spatial scales. Sub-scenes in which the streaks are too weak to determine wind direction do not return a direction, as governed by a user-selected threshold. Wind directions for these sub-scenes are based on those in neighbouring sub-scenes by using an adaptive smoothing technique. Quality control involves tuning the threshold level. We apply the method to two examples of RADARSAT-1 SAR images. The results are compared with those of a DFT-based wind direction analysis, and it is shown that a robust wind direction field is obtained. Mesoscale wind structures can be described by using a finer computing grid. The estimated wind directions still include a 180° direction ambiguity.Nous présentons une méthode pour l'estimation automatique des directions de vent à partir d'images du radar à synthèse d'ouverture (RSO) de l'océan. La méthode est basée sur l'analyse en ondelettes et repose sur la prémisse que la direction du vent s'aligne suivant les vortex des rouleaux à la couche limite de l'atmosphère, qui se manifestent souvent sous forme de stries à l'échelle kilométrique dans les images RSO de l'océan, et mesure l'orientation de ces stries. Contrairement aux méthodes d'estimation utilisant la transformée de Fourier discrète (TFD), les stries dans les images RSO peuvent être décrites quantitativement comme un produit naturel de cette méthode. De plus, des directions plus optimales de vent sont obtenues en comparant l'orientation directionnelle des stries à différentes échelles spatiales. Les sous-scènes dans lesquelles les stries sont trop faibles pour permettre de déterminer la direction du vent ne retournent pas de direction tel que défini par le seuil choisi par l'utilisateur. Les directions de vent pour ces sous-scènes sont basées sur celles des sous-scènes avoisinantes en utilisant une technique adaptative de lissage. Le contrôle de la qualité implique un ajustement du niveau de seuillage. Nous appliquons la méthode à deux exemples d'images RSO de RADARSAT-1. Les résultats sont comparés aux résultats de l'analyse des directions de vent basée sur la TFD et il est démontré qu'il est possible d'obtenir un champ robuste de directions de vent. Des structures de vent à méso-échelle peuvent être décrites en utilisant une grille de calcul plus fine. Les directions de vent estimées comportent toujours une ambiguïté de direction de 180°.[Traduit par la Rédaction]

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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 categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Simulation or modeling · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.869
Threshold uncertainty score0.987

Codex and Gemma teacher scores by category

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

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 head0.016
GPT teacher head0.195
Teacher spread0.180 · 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