{
  "annotation_id": "8b598d74-f2a4-4153-b9b7-410fa73b943b",
  "date_created": "2026-03-02T18:01:17.809000Z",
  "date_modified": "2026-03-02T18:01:17.809000Z",
  "file_hash": "d45656c0c49adba8cc6f164c77fef1bad2ddfc9d8ad933bde77d9f0a7b891af0",
  "private": false,
  "record": {
    "abstract": "It is noted that the results of recent experiments on the enhancement of\nturbulent kinetic energy (TKE) dissipation below surface waves can be stated as\nfollows. TKE dissipation is enhanced by a factor $15 H_{ws}/z$ at depths $0.5\nH_{ws} \u003c z \u003c 20 H_{ws}$ with respect to the wall-layer result $\\epsilon =\nu_{*w}^3/\\kappa z$, where $u_{*w}$ is the friction velocity in water and\n$H_{ws}$ is the significant wind-sea wave height. For open ocean conditions,\nthis reduces in most cases to an enhancement factor $10^6 u_{*w}^2/gz \\approx\nU_{10}^2/gz$.",
    "arxiv_id": "physics/9610002",
    "authors": [
      "Gerrit Burgers"
    ],
    "categories": [
      "physics.ao-ph"
    ],
    "title": "Comment on Enhanced TKE Dissipation under Breaking Waves",
    "url": "https://arxiv.org/abs/physics/9610002"
  },
  "schema_id": "dorsal/arxiv",
  "source": {
    "execution_id": "0f233275-5f13-4054-946e-f8671206b0e9",
    "id": "arXiv Dataset IDs",
    "type": "Model",
    "variant": "snapshot-2026-03-01",
    "version": "0.1.0"
  },
  "user_id": 1000002
}