{
  "annotation_id": "127f52f3-7ad0-4084-b5f9-cf9d056d1410",
  "date_created": "2026-03-02T18:00:57.375000Z",
  "date_modified": "2026-03-02T18:00:57.375000Z",
  "file_hash": "ef01ae34541c8ffb315af8d8a0e51122bcfd76c6316cd1fea889d7903b46ed26",
  "private": false,
  "record": {
    "abstract": "This is our response to a comment by Walter Eifler on our paper `A simple\nmodel for the short-time evolution of near-surface current and temperature\nprofiles\u0027 (arXiv:physics/0503186, accepted for publication in Deep-Sea Research\nII). Although Eifler raises genuine issues regarding our model\u0027s validity and\napplicability, we are nevertheless of the opinion that it is of value for the\nshort-term evolution of the upper-ocean profiles of current and temperature.\nThe fact that the effective eddy viscosity tends to infinity for infinite time\nunder a steady wind stress may not be surprising. It can be interpreted as a\nvertical shift of the eddy viscosity profile and an increase in the size of the\ndominant turbulent eddies under the assumed conditions of small stratification\nand infinite water depth.",
    "arxiv_id": "physics/0503187",
    "authors": [
      "Alastair D. Jenkins",
      "Brian Ward"
    ],
    "categories": [
      "physics.ao-ph",
      "physics.flu-dyn"
    ],
    "doi": "10.1016/j.dsr2.2005.03.003",
    "title": "Reply to comment on `A simple model for the short-time evolution of   near-surface current and temperature profiles\u0027",
    "url": "https://arxiv.org/abs/physics/0503187"
  },
  "schema_id": "dorsal/arxiv",
  "source": {
    "execution_id": "61aeb94c-4096-415c-bfd9-8de64887d833",
    "id": "arXiv Dataset IDs",
    "type": "Model",
    "variant": "snapshot-2026-03-01",
    "version": "0.1.0"
  },
  "user_id": 1000002
}