{
  "annotation_id": "515ba85c-f9c0-4eca-8aae-e57da426e845",
  "date_created": "2026-03-02T18:00:42.410000Z",
  "date_modified": "2026-03-02T18:00:42.410000Z",
  "file_hash": "81da2ea3035f74a1958c20909c54b7073943313ca12cbe030f314185fa37b12d",
  "private": false,
  "record": {
    "abstract": "In a recent letter [K. Fraedrich and R. Blender, Phys. Rev. Lett. 90, 108501\n(2003)], Fraedrich and Blender studied the scaling of atmosphere and ocean\ntemperature. They analyzed the fluctuation functions F(s) ~ s^alpha of monthly\ntemperature records (mostly from grid data) by using the detrended fluctuation\nanalysis (DFA2) and claim that the scaling exponent alpha over the inner\ncontinents is equal to 0.5, being characteristic of uncorrelated random\nsequences. Here we show that this statement is (i) not supported by their own\nanalysis and (ii) disagrees with the analysis of the daily observational data\nfrom which the grid monthly data have been derived. We conclude that also for\nthe inner continents, the exponent is between 0.6 and 0.7, similar as for the\ncoastline-stations.",
    "arxiv_id": "physics/0305080",
    "authors": [
      "Armin Bunde",
      "Jan F. Eichner",
      "Shlomo Havlin",
      "Eva Koscielny-Bunde",
      "Hans J. Schellnhuber",
      "Dmitry Vjushin"
    ],
    "categories": [
      "physics.ao-ph",
      "cond-mat.stat-mech",
      "physics.data-an"
    ],
    "doi": "10.1103/PhysRevLett.92.039801",
    "title": "Comment on \"Scaling of atmosphere and ocean temperature correlations in   observations and climate models\"",
    "url": "https://arxiv.org/abs/physics/0305080"
  },
  "schema_id": "dorsal/arxiv",
  "source": {
    "execution_id": "7a096b54-5bf2-43be-935c-4fb6e25d5d38",
    "id": "arXiv Dataset IDs",
    "type": "Model",
    "variant": "snapshot-2026-03-01",
    "version": "0.1.0"
  },
  "user_id": 1000002
}