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Record W1958306938 · doi:10.1080/07055900.2015.1074883

Conversion of Pressure to Depth for Moored Instruments Using a Reference Bottom Mounted Pressure Sensor

2015· article· en· W1958306938 on OpenAlexvenueno aff
Junde Li, Chujin Liang, Changming Dong, Weifang Jin, Guanghong Liao, Beifeng Zhou, Tao Ding, Xiaodong Lü, Xiangming Zhang

Bibliographic record

VenueATMOSPHERE-OCEAN · 2015
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicUnderwater Acoustics Research
Canadian institutionsnot available
Fundersnot available
KeywordsPressure sensorGeodesyDisplacement (psychology)Vertical displacementPressure measurementGeologyPerturbation (astronomy)AccelerationObservational errorMeasuring instrumentGravimeterAcousticsMarine engineeringRemote sensingMeteorologyMathematicsPhysicsEngineeringStatisticsGeophysicsMechanical engineering

Abstract

fetched live from OpenAlex

A new method is proposed to convert pressure measured by an instrument to water depth using an additional available bottom-moored pressure sensor.A perturbation analysis is used in this analysis, which leads to a simple formula for calculating water depth (defined as one from the mean sea surface to the instrument) from the pressure data.In field experiments, this method is easier to apply than existing methods.Based on the theoretical derivation, the error associated with the method comes from two sources when the instrument depth is known at the beginning of the measurement: temporal variation of deep water density at depths deeper than the instrument and variation in the gravitational acceleration with instrument displacement.These two sources contribute up to 4% of the error relative to the vertical displacement of the instrument, assuming the pressure sensor is accurate.With the vertical displacement of the instrument being on the order of 10 m, the absolute error is on the order of 0.4 m, which is expected and acceptable in oceanic measurements.The method is applied to data from a field experiment that took place along the Myanmar coast in December 2012.RSUM [Traduit par la rdaction] Nous proposons une nouvelle mthode pour convertir la pression mesure par un instrument en une mesure de profondeur de l'eau, l'aide d'un capteur de pression supplmentaire existant, amarr au fond marin.Une analyse des perturbations taye cette tude, qui mne une formule simple servant calculer la profondeur de l'eau (soit la distance entre la surface moyenne de la mer et l'instrument) partir des donnes de pression.Dans le cadre d'expriences sur le terrain, cette mthode s'avre plus facile appliquer que les mthodes existantes.Selon des dductions thoriques, l'incertitude associe cette mthode provient de deux sources quand la profondeur de l'instrument est connue au dbut de la prise de mesure : la variation temporelle de la densit des eaux profondes sous l'instrument et la variation de l'acclration gravitationnelle associe au dplacement de l'instrument.Ces deux sources de variation produisent jusqu' 4% d'incertitude relativement au mouvement vertical de l'instrument, en supposant que le capteur de pression reste fiable.Comme le dplacement vertical de l'instrument est de l'ordre de 10 m, l'incertitude absolue est de l'ordre de 0,4 m, ce qui est normal et acceptable pour des mesures effectues en mer.Nous avons appliqu cette mthode aux donnes provenant d'une exprience sur le terrain qui s'est droule le long de la cte du Myanmar, en dcembre 2012.

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 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 score0.664
Threshold uncertainty score0.830

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 studies0.0000.000
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 head0.051
GPT teacher head0.288
Teacher spread0.236 · 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.

The models applied no category: nothing in the taxonomy fit this work.
Study designSimulation or modeling
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".

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Citations0
Published2015
Admission routes1
Has abstractyes

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