{
  "annotation_id": "84b641dd-34ba-4feb-97ed-7f39805df15e",
  "date_created": "2026-03-02T18:01:14.140000Z",
  "date_modified": "2026-03-02T18:01:14.140000Z",
  "file_hash": "db5888280a2e52eb80a202bbef4fc32bab293563baf5955916864c5f03b52c30",
  "private": false,
  "record": {
    "abstract": "The 24 September 2001 College Park, Maryland, tornado was remarkable because\nof its long-track that passed within a close range of two Doppler radars. This\ntornado featured many similarities to previous significant tornado events that\nresulted in widespread damage in urban areas, such as the Oklahoma City tornado\nof 3 May 1999. The College Park tornado was the third in a series of three\ntornadoes associated with a supercell storm that developed over central\nVirginia. This paper presents a synoptic and mesoscale overview of favorable\nconditions and forcing mechanisms that resulted in the severe convective\noutbreak associated with the College Park tornado. Convective morphology will\nbe examined in terms of Doppler radar and satellite imagery. This study\nconcludes with a discussion of the effectiveness of using MM5 guidance in\nconjunction with satellite and radar imagery in the operational environment of\nforecasting severe convection.",
    "arxiv_id": "physics/0610217",
    "authors": [
      "Kenneth Pryor"
    ],
    "categories": [
      "physics.ao-ph"
    ],
    "title": "The Development of the College Park Tornado of 24 September 2001",
    "url": "https://arxiv.org/abs/physics/0610217"
  },
  "schema_id": "dorsal/arxiv",
  "source": {
    "execution_id": "bd5f087c-5872-4b0e-8a56-717a183131ea",
    "id": "arXiv Dataset IDs",
    "type": "Model",
    "variant": "snapshot-2026-03-01",
    "version": "0.1.0"
  },
  "user_id": 1000002
}