{
  "annotation_id": "c0f59d92-d85f-4e27-a251-d48dbcb53939",
  "date_created": "2026-03-02T18:00:43.206000Z",
  "date_modified": "2026-03-02T18:00:43.206000Z",
  "file_hash": "7f3a058ba02a18cd240900782ba497c39c2a4623fdf300424d9986e08e90d048",
  "private": false,
  "record": {
    "abstract": "A high altitude nuclear electromagnetic pulse (EMP) with a peak field\nintensity of 5 x 10^4 V/m carries momentum that results in a retarding force on\nthe average Compton electron (radiating coherently to produce the waveform)\nwith magnitude near that of the geomagnetic force responsible for the coherent\nradiation. The retarding force results from a self field effect. The Compton\nelectron interaction with the self generated magnetic field due to the other\nelectrons accounts for the momentum density in the propagating wave;\ninteraction with the self generated electric field accounts for the energy flux\ndensity in the propagating wave. Coherent addition of radiation is also\nquantitatively modeled.",
    "arxiv_id": "physics/0306028",
    "authors": [
      "Charles N. Vittitoe",
      "Mario Rabinowitz"
    ],
    "categories": [
      "physics.gen-ph",
      "physics.class-ph"
    ],
    "doi": "10.1103/PhysRevA.37.1969",
    "journal_ref": "Phys.Rev.A37:1969-1977,1988",
    "title": "Radiative Reactions and Coherence Modeling in the High Altitude   Electromagnetic Pulse",
    "url": "https://arxiv.org/abs/physics/0306028"
  },
  "schema_id": "dorsal/arxiv",
  "source": {
    "execution_id": "bf8e11b5-9c83-4874-a989-004ead20d797",
    "id": "arXiv Dataset IDs",
    "type": "Model",
    "variant": "snapshot-2026-03-01",
    "version": "0.1.0"
  },
  "user_id": 1000002
}