POLYHEDRAL GEOMETRY

# Polyhedral Earth: Structural Geometry, Solar Reception, and Cross-Scale Invariance **Author:** Christopher Macachor **ORCID:** https://orcid.org/0009-0008-0100-2856 **Research site:** https://earth.macachor.org/ **Research corpus:** https://scalar.macachor.org/ **Record status:** Metadata and publication-package draft; Zenodo DOI not yet assigned. ## Abstract This research examines polyhedral geometry as a structural representation for investigating planetary form, solar reception, and cross-scale geometric relationships. A polyhedron retains discrete planar faces, edges, vertices, face areas, and face-normal directions. These geometric properties provide measurable quantities for examining orientation, projected area, directional exposure, and structural differentiation. The planetary research program focuses on the June solstice and Arctic regions of North America, Greenland, and northern Eurasia. Locations north of the Arctic Circle experience continuous daylight during the relevant seasonal interval. Daylight duration, solar declination, geographic latitude, Earth–Sun distance, incident irradiance, and regional temperature are treated as distinct variables. Temperature comparisons require identified stations, defined climatological periods, and traceable observational sources. The mathematical program includes face-resolved solar incidence and projected-area calculations. For a planar face i, the idealized direct-beam contribution may be expressed as P_i = E(r) A_i max(0, n_i · s), where E(r) is solar irradiance at the relevant Earth–Sun distance, A_i is the face area, n_i is the outward unit normal, and s is the unit vector toward the incoming source. This equation describes geometric projection; it does not establish that Earth is physically a regular polyhedron. The cross-scale research direction investigates whether polyhedral descriptors—faces, edges, vertices, adjacency, orientation, and scale-dependent measurements—can serve as a comparative structural language across atomic, molecular, biological, and planetary examples. Similarity of mathematical description is not, by itself, evidence of a shared physical mechanism. The work follows the Macachor territory–cartography distinction: territory is reality; cartography is representation; correspondence is the test. Models are representations whose validity must be assessed through mathematical consistency, correspondence with observations, explicit uncertainty, and falsifiable comparisons. This record presents a research framework and model-development program. It distinguishes observed measurements, derived geometric quantities, proposed interpretations, and unresolved empirical questions. It does not claim that a polyhedral Earth geometry has been established by the evidence presented here. ## Research scope 1. **Polyhedral geometry:** compare selectable polyhedral families using explicit face, edge, vertex, normal-vector, area, and adjacency descriptors.2. **Planetary solar geometry:** calculate solar declination, local hour angle, latitude-dependent daylight duration, Earth–Sun distance scaling, face incidence, and projected area.3. **Arctic observational comparison:** document 24-hour daylight conditions north of the Arctic Circle around the June solstice and compare regional temperatures only where station identity, averaging period, units, and authoritative source are recorded.4. **Cross-scale comparison:** investigate whether geometric descriptors can be meaningfully compared across atomic, molecular, biological, and planetary examples without assuming that geometric analogy proves common physical ontology.5. **Empirical adjudication:** compare predictions against observations and conventional reference models; report uncertainty, assumptions, and possible falsifiers. ## Core geometric expression For a planar face *i* under direct illumination: `P_i = E(r) A_i max(0, n_i · s)` where: - `P_i` is the idealized incident power on the face;- `E(r)` is direct-beam irradiance at Earth–Sun distance `r`;- `A_i` is the face area;- `n_i` is the outward unit face-normal vector;- `s` is the unit vector toward the incoming source. This is a projected-area relationship. A complete planetary energy budget must additionally account for the actual planetary boundary geometry, atmospheric transmission and scattering, clouds, albedo, surface properties, rotation, orbital geometry, and spatial integration. The face-resolved equation alone does not establish a polyhedral physical Earth. ## Arctic summer-solstice treatment The June-solstice analysis must distinguish: - axial tilt and solar declination;- geographic latitude and local hour angle;- polar-day conditions and local solar incidence;- Earth–Sun distance and irradiance scaling;- observed temperature and its multiple climatic controls. The Arctic Circle is approximately 66.56° N under the present obliquity. Continuous daylight at higher latitudes near the June solstice follows from the Sun's daily path remaining above the local horizon. It should not be attributed to a planar face or to Earth being closer to the Sun. Earth reaches perihelion in early January and aphelion in early July; the solstice and aphelion are distinct orbital events. Temperature tables must not be populated with unsupported illustrative numbers. Each station record should include station name, country/region, coordinates, elevation where available, dataset/provider, climatological normal period, month, statistic, units, retrieval date, and a persistent citation or URL. ## Evidence and claim classification Use the following labels consistently: - **Observed:** directly reported by a traceable observational source.- **Derived:** calculated from stated inputs and equations.- **Model assumption:** chosen for a simulation and not asserted as an observation.- **Hypothesis:** a proposed interpretation requiring testing.- **Open:** unresolved or lacking sufficient evidence. ## Author contributions and AI attribution Christopher Macachor is the author and originator of the research direction and underlying intellectual framework. Contributions include polymathic discovery, cross-domain synthesis, semantic compression, structural-invariant identification, and structural reconstruction. Artificial intelligence tools may be credited for assistance with mathematical notation, formal representations, code, and visualization. AI-assisted mathematical representations are not presented as independent authorship or as original mathematical discoveries by the AI. Final intellectual authorship and responsibility remain with Christopher Macachor. ## Related research and provenance This work is intended to sit within the Macachor Research Corpus and should be linked to the following existing records: - Macachor Research Corpus landing record: https://doi.org/10.5281/zenodo.23972588- Macachor Scalar Field v3.0: https://doi.org/10.5281/zenodo.23964606 These identifiers are related corpus records, not the DOI for this Polyhedral Earth record. A DOI for this record must be added only after Zenodo assigns it. ## Suggested files for the Zenodo upload - `README.md` — this research description and methodological scope.- `.zenodo.json` — draft Zenodo deposition metadata.- `citation.cff` — citation metadata.- `index.html` — scholarly landing-page metadata template.- `provenance-manifest.json` — file hashes and provenance notes. ## Publication and versioning Freeze the exact files before publication. Compute SHA-256 hashes for the deposited artifacts and preserve the manifest with the release. Substantive changes should be published as a new version with a new version-specific artifact identity. Do not silently overwrite a frozen canonical artifact. ## Important limitation The research website could not be retrieved during preparation because the host returned HTTP 403. This package is therefore a metadata and manuscript draft based on the author's previously supplied framework and prototype material; it is not a verified extraction of the current live website. Review the title, abstract, affiliations, related-record relationships, license, and final files before depositing.

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Zenodo (CERN European Organization for Nuclear Research)
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2026-11-11
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https://doi.org/10.5281/zenodo.24124560
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Historical Geography and Cartography
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article
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article

POLYHEDRAL GEOMETRY

Christopher Macachor
Zenodo (CERN European Organization for Nuclear Research)
Historical Geography and Cartography
article

POLYHEDRAL GEOMETRY

Christopher Macachor
article en

Abstract

# Polyhedral Earth: Structural Geometry, Solar Reception, and Cross-Scale Invariance **Author:** Christopher Macachor **ORCID:** https://orcid.org/0009-0008-0100-2856 **Research site:** https://earth.macachor.org/ **Research corpus:** https://scalar.macachor.org/ **Record status:** Metadata and publication-package draft; Zenodo DOI not yet assigned. ## Abstract This research examines polyhedral geometry as a structural representation for investigating planetary form, solar reception, and cross-scale geometric relationships. A polyhedron retains discrete planar faces, edges, vertices, face areas, and face-normal directions. These geometric properties provide measurable quantities for examining orientation, projected area, directional exposure, and structural differentiation. The planetary research program focuses on the June solstice and Arctic regions of North America, Greenland, and northern Eurasia. Locations north of the Arctic Circle experience continuous daylight during the relevant seasonal interval. Daylight duration, solar declination, geographic latitude, Earth–Sun distance, incident irradiance, and regional temperature are treated as distinct variables. Temperature comparisons require identified stations, defined climatological periods, and traceable observational sources. The mathematical program includes face-resolved solar incidence and projected-area calculations. For a planar face i, the idealized direct-beam contribution may be expressed as P_i = E(r) A_i max(0, n_i · s), where E(r) is solar irradiance at the relevant Earth–Sun distance, A_i is the face area, n_i is the outward unit normal, and s is the unit vector toward the incoming source. This equation describes geometric projection; it does not establish that Earth is physically a regular polyhedron. The cross-scale research direction investigates whether polyhedral descriptors—faces, edges, vertices, adjacency, orientation, and scale-dependent measurements—can serve as a comparative structural language across atomic, molecular, biological, and planetary examples. Similarity of mathematical description is not, by itself, evidence of a shared physical mechanism. The work follows the Macachor territory–cartography distinction: territory is reality; cartography is representation; correspondence is the test. Models are representations whose validity must be assessed through mathematical consistency, correspondence with observations, explicit uncertainty, and falsifiable comparisons. This record presents a research framework and model-development program. It distinguishes observed measurements, derived geometric quantities, proposed interpretations, and unresolved empirical questions. It does not claim that a polyhedral Earth geometry has been established by the evidence presented here. ## Research scope 1. **Polyhedral geometry:** compare selectable polyhedral families using explicit face, edge, vertex, normal-vector, area, and adjacency descriptors.2. **Planetary solar geometry:** calculate solar declination, local hour angle, latitude-dependent daylight duration, Earth–Sun distance scaling, face incidence, and projected area.3. **Arctic observational comparison:** document 24-hour daylight conditions north of the Arctic Circle around the June solstice and compare regional temperatures only where station identity, averaging period, units, and authoritative source are recorded.4. **Cross-scale comparison:** investigate whether geometric descriptors can be meaningfully compared across atomic, molecular, biological, and planetary examples without assuming that geometric analogy proves common physical ontology.5. **Empirical adjudication:** compare predictions against observations and conventional reference models; report uncertainty, assumptions, and possible falsifiers. ## Core geometric expression For a planar face *i* under direct illumination: `P_i = E(r) A_i max(0, n_i · s)` where: - `P_i` is the idealized incident power on the face;- `E(r)` is direct-beam irradiance at Earth–Sun distance `r`;- `A_i` is the face area;- `n_i` is the outward unit face-normal vector;- `s` is the unit vector toward the incoming source. This is a projected-area relationship. A complete planetary energy budget must additionally account for the actual planetary boundary geometry, atmospheric transmission and scattering, clouds, albedo, surface properties, rotation, orbital geometry, and spatial integration. The face-resolved equation alone does not establish a polyhedral physical Earth. ## Arctic summer-solstice treatment The June-solstice analysis must distinguish: - axial tilt and solar declination;- geographic latitude and local hour angle;- polar-day conditions and local solar incidence;- Earth–Sun distance and irradiance scaling;- observed temperature and its multiple climatic controls. The Arctic Circle is approximately 66.56° N under the present obliquity. Continuous daylight at higher latitudes near the June solstice follows from the Sun's daily path remaining above the local horizon. It should not be attributed to a planar face or to Earth being closer to the Sun. Earth reaches perihelion in early January and aphelion in early July; the solstice and aphelion are distinct orbital events. Temperature tables must not be populated with unsupported illustrative numbers. Each station record should include station name, country/region, coordinates, elevation where available, dataset/provider, climatological normal period, month, statistic, units, retrieval date, and a persistent citation or URL. ## Evidence and claim classification Use the following labels consistently: - **Observed:** directly reported by a traceable observational source.- **Derived:** calculated from stated inputs and equations.- **Model assumption:** chosen for a simulation and not asserted as an observation.- **Hypothesis:** a proposed interpretation requiring testing.- **Open:** unresolved or lacking sufficient evidence. ## Author contributions and AI attribution Christopher Macachor is the author and originator of the research direction and underlying intellectual framework. Contributions include polymathic discovery, cross-domain synthesis, semantic compression, structural-invariant identification, and structural reconstruction. Artificial intelligence tools may be credited for assistance with mathematical notation, formal representations, code, and visualization. AI-assisted mathematical representations are not presented as independent authorship or as original mathematical discoveries by the AI. Final intellectual authorship and responsibility remain with Christopher Macachor. ## Related research and provenance This work is intended to sit within the Macachor Research Corpus and should be linked to the following existing records: - Macachor Research Corpus landing record: https://doi.org/10.5281/zenodo.23972588- Macachor Scalar Field v3.0: https://doi.org/10.5281/zenodo.23964606 These identifiers are related corpus records, not the DOI for this Polyhedral Earth record. A DOI for this record must be added only after Zenodo assigns it. ## Suggested files for the Zenodo upload - `README.md` — this research description and methodological scope.- `.zenodo.json` — draft Zenodo deposition metadata.- `citation.cff` — citation metadata.- `index.html` — scholarly landing-page metadata template.- `provenance-manifest.json` — file hashes and provenance notes. ## Publication and versioning Freeze the exact files before publication. Compute SHA-256 hashes for the deposited artifacts and preserve the manifest with the release. Substantive changes should be published as a new version with a new version-specific artifact identity. Do not silently overwrite a frozen canonical artifact. ## Important limitation The research website could not be retrieved during preparation because the host returned HTTP 403. This package is therefore a metadata and manuscript draft based on the author's previously supplied framework and prototype material; it is not a verified extraction of the current live website. Review the title, abstract, affiliations, related-record relationships, license, and final files before depositing.

Zenodo (CERN European Organization for Nuclear Research)
Historical Geography and Cartography
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