{
  "annotation_id": "4591f575-acd3-4709-8118-97d6917ede46",
  "date_created": "2026-03-02T18:01:25.013000Z",
  "date_modified": "2026-03-02T18:01:25.013000Z",
  "file_hash": "71f5923ace19f3c25c6310d0cec6b1243b9dba4704fee17822ca2219790367d0",
  "private": false,
  "record": {
    "abstract": "The radiation from the mixed layer into the interior of the ocean of\nnear-inertial oscillations excited by a passing storm in the presence of the\nbeta effect is reconsidered as an initial-value problem. Making use of the fact\nthat the mixed layer depth is much smaller than the total depth of the ocean,\nthe solution is obtained in the limit of an ocean that is effectively\ninfinitely deep. For a uniform initial condition, analytical results for the\nvelocity, horizontal kinetic energy density and fluxes are obtained. The\nresulting decay of near-inertial mixed layer energy in the presence of the beta\neffect occurs on a timescale similar to that observed.",
    "arxiv_id": "physics/9912030",
    "authors": [
      "Jeff Moehlis",
      "Stefan G. Llewellyn Smith"
    ],
    "categories": [
      "physics.ao-ph"
    ],
    "title": "Radiation of mixed layer near-inertial oscillations into the ocean   interior",
    "url": "https://arxiv.org/abs/physics/9912030"
  },
  "schema_id": "dorsal/arxiv",
  "source": {
    "execution_id": "68874301-22f1-42f0-9007-282886c8f75c",
    "id": "arXiv Dataset IDs",
    "type": "Model",
    "variant": "snapshot-2026-03-01",
    "version": "0.1.0"
  },
  "user_id": 1000002
}