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Radiation of mixed layer near-inertial oscillations into the ocean interior

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Jeff Moehlis, Stefan G. Llewellyn Smith

Atmospheric and Oceanic Physics · Submitted 14 Dec 1999

abstract compiled · 2026-09-23 · no language-model review

The authors' main claim The resulting decay of near-inertial mixed layer energy in the presence of the beta effect occurs on a timescale similar to that observed.

how it is stated · asserted 0.97 read the record →

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arXiv IDphysics/9912030 (version 1)
Pith IDPIK2L6SU, Pith's permanent record of this paper and its review
CitationJeff Moehlis, Stefan G. Llewellyn Smith. "Radiation of mixed layer near-inertial oscillations into the ocean interior." arXiv:physics/9912030 (1999). https://pith.science/paper/PIK2L6SU
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The compiled record

The paper's own sentences, arranged. Each label is drawn from a closed vocabulary; the number beside it is the probability the classifier gave that label. Numbers in the tables are the authors', checked by code. No sentence in this record was written by a model.

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Compiled by classifier-1.13.0 via TypeSafe API, question bank abstract-p1-20260923, 2026-09-23: 1 request, 3,619 input tokens.

What the abstract itself states, as probabilities: claims first 0.04 · states limitation 0.43 · human participants 0.01 · controlled comparison 0.03 · randomized assignment 0.01 · states quantitative result 0.10 · compares with prior results 0.34 · mentions code or data availability 0.02.

The abstract, sentence by sentence

arXiv listing abstract v1. Results and the main claim are underlined; .

The radiation from the mixed layer into the interior of the ocean of near-inertial oscillations excited by a passing storm in the presence of the beta effect is reconsidered as an initial-value problem. Making use of the fact that the mixed layer depth is much smaller than the total depth of the ocean, the solution is obtained in the limit of an ocean that is effectively infinitely deep. For a uniform initial condition, analytical results for the velocity, horizontal kinetic energy density and fluxes are obtained. The resulting decay of near-inertial mixed layer energy in the presence of the beta effect occurs on a timescale similar to that observed.

background contribution method result interpretation main claim

What the classifier reports for each sentence. The number is the probability it gave the label.
#sentencerolethe authors' own workstates the main conclusionstrength
s0 The radiation from the mixed layer into the interior of the ocean of near-inertial oscillations excited by a passing storm in the presence of the beta effect is reconsidered as an initial-value problem. contribution 0.80 0.64 0.11 asserted 0.86
s1 Making use of the fact that the mixed layer depth is much smaller than the total depth of the ocean, the solution is obtained in the limit of an ocean that is effectively infinitely deep. method 0.99 0.89 0.06 asserted 0.99
s2 For a uniform initial condition, analytical results for the velocity, horizontal kinetic energy density and fluxes are obtained. result 0.53 0.91 0.09 asserted 1.00
s3 The resulting decay of near-inertial mixed layer energy in the presence of the beta effect occurs on a timescale similar to that observed. result 0.84 0.84 0.58 asserted 0.97

What kind of paper the classifier reports this is: theoretical result 1.00 · evidence from proof or derivation 1.00.

What was examined, and what was not

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  • references and citing sentences
  • relations to other papers
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  • T body sentences
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Every quoted sentence on this record is the authors'. Every label is from Pith's closed vocabulary, with the probability shown beside it. Every number in the measurements table is the authors', checked by code. Record as JSON

The paper
Original abstract

The radiation from the mixed layer into the interior of the ocean of near-inertial oscillations excited by a passing storm in the presence of the beta effect is reconsidered as an initial-value problem. Making use of the fact that the mixed layer depth is much smaller than the total depth of the ocean, the solution is obtained in the limit of an ocean that is effectively infinitely deep. For a uniform initial condition, analytical results for the velocity, horizontal kinetic energy density and fluxes are obtained. The resulting decay of near-inertial mixed layer energy in the presence of the beta effect occurs on a timescale similar to that observed.

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