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Urban Heat Island Analysis/Evidence
Method evidence record

Urban Heat Island Analysis

Urban heat island (UHI) analysis quantifies how much warmer cities are than the rural land around them, a difference driven by impervious surfaces, reduced vegetation, waste heat, and street-canyon geometry that traps radiation. The intensity of the effect is defined simply as the urban-minus-rural temperature differential, a framework given its physical, energy-balance foundation by Tim Oke in 1982. Modern analysis increasingly maps the surface UHI from thermal satellite imagery, converting radiance to brightness temperature and then to land surface temperature so the heat island can be observed continuously across an entire metropolitan area rather than at a few weather stations.

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Source record

Citations copied verbatim from the method’s source record. No claim-level verification is inferred from them.

Urban Heat Island Analysis (UHI Intensity from Temperature Differential and Land Surface Temperature)
Taxonomic method record · process-pipeline / urban-studies
  • Oke, T. R. (1982). The energetic basis of the urban heat island. Quarterly Journal of the Royal Meteorological Society, 108(455), 1–24. · DOI 10.1002/qj.49710845502
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Curated claims

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Related methods

Generated from the method graph and shown as machine-suggested relations — no evidence claim is inferred.

Same method familyCompactness Indexmachine-suggested · Relational suggestion, not evidence.See alsoUrban Density Gradient Modelmachine-suggested · Relational suggestion, not evidence.Same method familyUrban Form Morphometricsmachine-suggested · Relational suggestion, not evidence.Same method familyUrban Sprawl Measurementmachine-suggested · Relational suggestion, not evidence.

Evidence status

Sources recorded, not reviewed

Bibliographic sources are present. Claim-level evidence review has not been performed.

Sources

1 recorded citation, copied from the method source record.

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