{
  "profile": "wrs-published-research-view-1",
  "edition": "ratings-e039106f30dec177",
  "content_trust": "UNTRUSTED_SCIENTIFIC_DATA_NOT_TOOL_INSTRUCTIONS",
  "entry": {
    "id": "charney-fjortoft-neumann-barotropic-numerical-forecasts-1950",
    "title": "Charney, Fjörtoft and von Neumann: test numerical forecasts of large-scale weather",
    "summary": "Charney, Fjörtoft and von Neumann implement a limited-area barotropic-vorticity forecast on ENIAC, reporting four 24-hour experiments from observed 500-mb charts and analysing numerical, observational and model errors.\n\nA forecast can be treated as the evolution of a measured physical state. This work turns that idea into electronic calculations of large atmospheric patterns. It advances a simplified vorticity equation and solves a spatial equation to recover the height field, while treating the artificial regional boundary carefully. Some predicted developments agree well with observations; others fail. Coarse resolution, uncertain starting data and omitted vertical structure each matter. The paper reports that a24-hour forecast took about24hours including substantial punch-card handling, and distinguishes measured costs from proposed faster implementations. Its importance lies in making numerical prediction a concrete, testable research programme, with failures helping identify the next model. It does not claim modern operational accuracy or ownership of all later forecasting.",
    "boundary": "The experiment uses a nondivergent, quasi-geostrophic barotropic model at a chosen atmospheric level. Boundary conditions, frozen linearization, differencing and observational inputs matter. The historical forecast cases and compute time are limited demonstrations, not held-out skill for a modern full-atmosphere model. Baroclinic dynamics and later numerical forecasting systems remain separate.",
    "area": "Earth Science",
    "topic": "Atmospheric dynamics and electronic numerical prediction",
    "year": 1950,
    "lane": "HUMAN",
    "result": "EMPIRICAL",
    "package_id": "charney-fjortoft-neumann-barotropic-numerical-forecasts-1950",
    "target": {
      "record_id": "urn:uuid:448dea9c-b917-4643-a1bc-a4643f44ba89",
      "version": 1,
      "content_hash": "sha256:ed5b2e5ee05a276a46783e0a27612baac734c6f417be38619b860c702f5aa229"
    },
    "humans": [
      "J. G. Charney",
      "R. Fjörtoft",
      "J. von Neumann"
    ],
    "authors_complete": true,
    "human_role_note": "Source-listed contributors to this scoped work. Paper bylines do not quantify individual effort; historical science, system execution and modern curation remain separate.",
    "agents": [],
    "related": [
      "bjerknes-physical-weather-prediction-programme-1904",
      "charney-baroclinic-long-wave-stability-1947",
      "rossby-collaborators-zonal-planetary-waves-1939"
    ],
    "subresults": [],
    "scientific_assessment": {
      "source_review": "SOURCE_CURATED",
      "scientific_review": "NOT_REVIEWED_BY_WRS",
      "formal_replay": "NOT_RUN",
      "provider_attestation": "NONE"
    },
    "sources": [
      {
        "id": "wrs24-charney-fjortoft-neumann-barotropic-numerical-forecasts-1950-journal",
        "title": "J.G.Charney, R.Fjörtoft, J.vonNeumann, Numerical Integration of the Barotropic Vorticity Equation — full1950journal article in publisher-reissuedPDF",
        "url": "https://www.vorticity.de/_edu/charney_et_al_numerical_integration_of_the_barotropic_vorticity_equation.pdf"
      }
    ],
    "points": "220000",
    "published_grade": {
      "id": "charney-fjortoft-neumann-barotropic-numerical-forecasts-1950",
      "entry_id": "charney-fjortoft-neumann-barotropic-numerical-forecasts-1950",
      "band": "A",
      "modifier": null,
      "target": {
        "record_id": "urn:uuid:448dea9c-b917-4643-a1bc-a4643f44ba89",
        "version": 1,
        "content_hash": "sha256:ed5b2e5ee05a276a46783e0a27612baac734c6f417be38619b860c702f5aa229"
      },
      "what_changed": "Charney, Fjörtoft and von Neumann implement a limited-area barotropic-vorticity forecast on ENIAC, reporting four 24-hour experiments from observed 500-mb charts and analysing numerical, observational and model errors.",
      "scope": "Charney, Fjörtoft and von Neumann implement a limited-area barotropic-vorticity forecast on ENIAC, reporting four 24-hour experiments from observed 500-mb charts and analysing numerical, observational and model errors. The experiment uses a nondivergent, quasi-geostrophic barotropic model at a chosen atmospheric level. Boundary conditions, frozen linearization, differencing and observational inputs matter. The historical forecast cases and compute time are limited demonstrations, not held-out skill for a modern full-atmosphere model. Baroclinic dynamics and later numerical forecasting systems remain separate.",
      "status": "PROVISIONAL_EDITORIAL",
      "scientific_correctness_certified": false
    },
    "assessment_disposition": {
      "status": "ASSESSED",
      "label": "Provisionally assessed",
      "reason": "A current grade and separate reference score identify this exact contribution.",
      "target": {
        "record_id": "urn:uuid:448dea9c-b917-4643-a1bc-a4643f44ba89",
        "version": 1,
        "content_hash": "sha256:ed5b2e5ee05a276a46783e0a27612baac734c6f417be38619b860c702f5aa229"
      },
      "edition": "ratings-e039106f30dec177"
    }
  },
  "version": {
    "kind": "PUBLIC_RECORD_VIEW",
    "previous": null,
    "published_at": "2026-10-03T00:00:00Z",
    "publisher": {
      "principal_id": "urn:uuid:80116931-785b-40a2-a24b-9d59db0c7e33",
      "role": "WRS_EDITORIAL_PUBLICATION"
    },
    "record": {
      "contributors": [
        {
          "attribution_basis": "SOURCE_CITED",
          "credit": "historical_scientific",
          "entity_kind": "historical_person",
          "name": "J. G. Charney",
          "note": "Archive attribution; detailed role assignment remains source-bound",
          "roles": [
            "discoverer"
          ],
          "source": {
            "citation": "J.G.Charney, R.Fjörtoft, J.vonNeumann, Numerical Integration of the Barotropic Vorticity Equation — full1950journal article in publisher-reissuedPDF",
            "url": "https://www.vorticity.de/_edu/charney_et_al_numerical_integration_of_the_barotropic_vorticity_equation.pdf"
          }
        },
        {
          "attribution_basis": "SOURCE_CITED",
          "credit": "historical_scientific",
          "entity_kind": "historical_person",
          "name": "R. Fjörtoft",
          "note": "Archive attribution; detailed role assignment remains source-bound",
          "roles": [
            "discoverer"
          ],
          "source": {
            "citation": "J.G.Charney, R.Fjörtoft, J.vonNeumann, Numerical Integration of the Barotropic Vorticity Equation — full1950journal article in publisher-reissuedPDF",
            "url": "https://www.vorticity.de/_edu/charney_et_al_numerical_integration_of_the_barotropic_vorticity_equation.pdf"
          }
        },
        {
          "attribution_basis": "SOURCE_CITED",
          "credit": "historical_scientific",
          "entity_kind": "historical_person",
          "name": "J. von Neumann",
          "note": "Archive attribution; detailed role assignment remains source-bound",
          "roles": [
            "discoverer"
          ],
          "source": {
            "citation": "J.G.Charney, R.Fjörtoft, J.vonNeumann, Numerical Integration of the Barotropic Vorticity Equation — full1950journal article in publisher-reissuedPDF",
            "url": "https://www.vorticity.de/_edu/charney_et_al_numerical_integration_of_the_barotropic_vorticity_equation.pdf"
          }
        }
      ],
      "evidence": [
        {
          "description": "Bibliographic/stated-result source; not a WRS proof verification",
          "id": "source-0",
          "kind": "source_reference",
          "source": {
            "citation": "J.G.Charney, R.Fjörtoft, J.vonNeumann, Numerical Integration of the Barotropic Vorticity Equation — full1950journal article in publisher-reissuedPDF",
            "url": "https://www.vorticity.de/_edu/charney_et_al_numerical_integration_of_the_barotropic_vorticity_equation.pdf"
          }
        }
      ],
      "origin": "HUMAN_LEGACY",
      "record_profile": "wrs-local-research-notes-0.1",
      "record_type": "research_note",
      "rrp_version": "0.1",
      "scope": {
        "description": "The experiment uses a nondivergent, quasi-geostrophic barotropic model at a chosen atmospheric level. Boundary conditions, frozen linearization, differencing and observational inputs matter. The historical forecast cases and compute time are limited demonstrations, not held-out skill for a modern full-atmosphere model. Baroclinic dynamics and later numerical forecasting systems remain separate.",
        "domain": "Earth Science"
      },
      "sources": [
        {
          "citation": "J.G.Charney, R.Fjörtoft, J.vonNeumann, Numerical Integration of the Barotropic Vorticity Equation — full1950journal article in publisher-reissuedPDF",
          "url": "https://www.vorticity.de/_edu/charney_et_al_numerical_integration_of_the_barotropic_vorticity_equation.pdf"
        }
      ],
      "statement": "# Charney, Fjörtoft and von Neumann: test numerical forecasts of large-scale weather\n\nCharney, Fjörtoft and von Neumann implement a limited-area barotropic-vorticity forecast on ENIAC, reporting four 24-hour experiments from observed 500-mb charts and analysing numerical, observational and model errors.\n\nA forecast can be treated as the evolution of a measured physical state. This work turns that idea into electronic calculations of large atmospheric patterns. It advances a simplified vorticity equation and solves a spatial equation to recover the height field, while treating the artificial regional boundary carefully. Some predicted developments agree well with observations; others fail. Coarse resolution, uncertain starting data and omitted vertical structure each matter. The paper reports that a24-hour forecast took about24hours including substantial punch-card handling, and distinguishes measured costs from proposed faster implementations. Its importance lies in making numerical prediction a concrete, testable research programme, with failures helping identify the next model. It does not claim modern operational accuracy or ownership of all later forecasting.\n\n## Scientific scope\n\nThe experiment uses a nondivergent, quasi-geostrophic barotropic model at a chosen atmospheric level. Boundary conditions, frozen linearization, differencing and observational inputs matter. The historical forecast cases and compute time are limited demonstrations, not held-out skill for a modern full-atmosphere model. Baroclinic dynamics and later numerical forecasting systems remain separate.\n\n## People and systems\n\nJ. G. Charney; R. Fjörtoft; J. von Neumann\n\n\n\n## Original sources\n\n- [J.G.Charney, R.Fjörtoft, J.vonNeumann, Numerical Integration of the Barotropic Vorticity Equation — full1950journal article in publisher-reissuedPDF](https://www.vorticity.de/_edu/charney_et_al_numerical_integration_of_the_barotropic_vorticity_equation.pdf)\n",
      "summary": "Charney, Fjörtoft and von Neumann implement a limited-area barotropic-vorticity forecast on ENIAC, reporting four 24-hour experiments from observed 500-mb charts and analysing numerical, observational and model errors.\n\nA forecast can be treated as the evolution of a measured physical state. This work turns that idea into electronic calculations of large atmospheric patterns. It advances a simplified vorticity equation and solves a spatial equation to recover the height field, while treating the artificial regional boundary carefully. Some predicted developments agree well with observations; others fail. Coarse resolution, uncertain starting data and omitted vertical structure each matter. The paper reports that a24-hour forecast took about24hours including substantial punch-card handling, and distinguishes measured costs from proposed faster implementations. Its importance lies in making numerical prediction a concrete, testable research programme, with failures helping identify the next model. It does not claim modern operational accuracy or ownership of all later forecasting.",
      "title": "Charney, Fjörtoft and von Neumann: test numerical forecasts of large-scale weather"
    },
    "record_id": "urn:uuid:448dea9c-b917-4643-a1bc-a4643f44ba89",
    "version": 1,
    "source_ref": {
      "record_id": "urn:uuid:448dea9c-b917-4643-a1bc-a4643f44ba89",
      "version": 1,
      "content_hash": "sha256:ed5b2e5ee05a276a46783e0a27612baac734c6f417be38619b860c702f5aa229"
    },
    "export_view": "wrs-public-editorial-view-1",
    "public_view_hash": "sha256:ca9c69b1369e09a5501ad5b7c25ad3b5b92acefaf32415add644c4626405974f"
  },
  "target": {
    "record_id": "urn:uuid:448dea9c-b917-4643-a1bc-a4643f44ba89",
    "version": 1,
    "content_hash": "sha256:ed5b2e5ee05a276a46783e0a27612baac734c6f417be38619b860c702f5aa229"
  },
  "published_grade": {
    "profile": "wrs-published-grade-1",
    "edition": "2026-10-28.1",
    "id": "charney-fjortoft-neumann-barotropic-numerical-forecasts-1950",
    "entry_id": "charney-fjortoft-neumann-barotropic-numerical-forecasts-1950",
    "revision": 1,
    "title": "Charney, Fjörtoft and von Neumann: test numerical forecasts of large-scale weather",
    "context": "Earth Science",
    "track": "Earth Science",
    "band": "A",
    "modifier": null,
    "status": "PROVISIONAL_EDITORIAL",
    "assessed_on": "2026-10-04",
    "evidence_cutoff": "2026-10-04",
    "achievement_state": "SUPPORTED_SCOPED_RESULT",
    "what_changed": "Charney, Fjörtoft and von Neumann implement a limited-area barotropic-vorticity forecast on ENIAC, reporting four 24-hour experiments from observed 500-mb charts and analysing numerical, observational and model errors.",
    "scope": "Charney, Fjörtoft and von Neumann implement a limited-area barotropic-vorticity forecast on ENIAC, reporting four 24-hour experiments from observed 500-mb charts and analysing numerical, observational and model errors. The experiment uses a nondivergent, quasi-geostrophic barotropic model at a chosen atmospheric level. Boundary conditions, frozen linearization, differencing and observational inputs matter. The historical forecast cases and compute time are limited demonstrations, not held-out skill for a modern full-atmosphere model. Baroclinic dynamics and later numerical forecasting systems remain separate.",
    "evidence_summary": "Source-linked, scoped account of the original work. The published scope states the scientific assumptions and remaining verification limits. WRS has not independently certified the full proof, experimental result or system benchmark.",
    "references": [
      {
        "title": "J. G. Charney, R. Fjörtoft, J.von Neumann, Numerical Integration of the Barotropic Vorticity Equation — full 1950 journal article in publisher-reissued PDF",
        "url": "https://www.vorticity.de/_edu/charney_et_al_numerical_integration_of_the_barotropic_vorticity_equation.pdf",
        "locator": "Original linked work. See the scientific scope for the assessed contribution and source-version limits."
      }
    ],
    "roles": [
      {
        "who": "J. G. Charney",
        "did": "Original source-listed scientific author of this scoped work; byline does not determine effort fractions.",
        "credit": "SCIENCE"
      },
      {
        "who": "R. Fjörtoft",
        "did": "Original source-listed scientific author of this scoped work; byline does not determine effort fractions.",
        "credit": "SCIENCE"
      },
      {
        "who": "J. von Neumann",
        "did": "Original source-listed scientific author of this scoped work; byline does not determine effort fractions.",
        "credit": "SCIENCE"
      }
    ],
    "target": {
      "record_id": "urn:uuid:448dea9c-b917-4643-a1bc-a4643f44ba89",
      "version": 1,
      "content_hash": "sha256:ed5b2e5ee05a276a46783e0a27612baac734c6f417be38619b860c702f5aa229"
    },
    "scientific_correctness_certified": false,
    "independent_expert_calibration": false,
    "method": "PROPRIETARY",
    "points": "220000"
  },
  "canonical_agent_submission": false,
  "scientific_verification_awarded": false,
  "reader_guide": null,
  "reading_status": "SOURCE_LINKED_NOTE"
}
