{
  "annotation_id": "bc91f895-274d-41d8-ae04-4860546b8874",
  "date_created": "2026-03-02T18:00:42.679000Z",
  "date_modified": "2026-03-02T18:00:42.679000Z",
  "file_hash": "887de446e9d64a1bd25f893a39170141eb8f5914e42501ba4d7977f8c7b53076",
  "private": false,
  "record": {
    "abstract": "The problem of submarine sediment slide which generates the surface water\nwaves is considered. To simulate numerically the landslide motion it is used\nthe method which permits to take into account detailed rheological properties\nof slide body constituents. The numerical simulation of landslide-induced\nsurface water waves is performed on the basis of nonlinear shallow water\nequations. It is studied a landslide behavior for two values of maximal\nfriction angle. The detailed comparison of landslide dynamics and evolution of\nlandslide-induced surface water waves during sliding is performed. Also, the\nevolution of dipolar water wave generated in the beginning of sediment sliding\nis studied. It is obtained that this dipolar wave is then transformed in two\nwave groups: crest and trough coming seaward and trough accompanied by crest\ncoming to the shoreline. The second wave group leads firstly to sea recession\nfrom the beach and only then to large runup (tsunami wave with first negative\nphase).",
    "arxiv_id": "physics/0212096",
    "authors": [
      "L. I. Lobkovsky",
      "G. A. Papadopoulos",
      "I. A. Garagash",
      "O. R. Kozyrev",
      "R. Kh. Mazova"
    ],
    "categories": [
      "physics.geo-ph",
      "physics.ao-ph"
    ],
    "title": "Submarine landslides and local tsunami waves (Corinthos Gulf, Greece)",
    "url": "https://arxiv.org/abs/physics/0212096"
  },
  "schema_id": "dorsal/arxiv",
  "source": {
    "execution_id": "0798bc08-86fd-416c-9cb6-a7e8a8614661",
    "id": "arXiv Dataset IDs",
    "type": "Model",
    "variant": "snapshot-2026-03-01",
    "version": "0.1.0"
  },
  "user_id": 1000002
}