Starten Sie Ihre Suche...


Wir weisen darauf hin, dass wir technisch notwendige Cookies verwenden. Weitere Informationen

Modeling Urban Land Surface Temperature Using Physics-Informed Neural Networks (PINNs)

ISPRS Annals of the Photogrammetry, Remote Sensing and Spatial Information Sciences. Bd. X-4/W8-2025. ISPRS Annals of the Photogrammetry, Remote Sensing and Spatial Information Sciences: Copernicus GmbH 2026 S. 277 - 283

Erscheinungsjahr: 2026

Publikationstyp: Diverses (Konferenzbeitrag)

Sprache: Englisch

Doi/URN: 10.5194/isprs-annals-x-4-w8-2025-277-2026

Volltext über DOI/URN

Geprüft:Bibliothek

Inhaltszusammenfassung


A compact physics-informed neural network (PINN) is developed to (i) quantify city-scale accuracy of 30 m urban land surface temperature (LST) maps, (ii) identify influential predictors, and (iii) contrast climate-dependent patterns between New York City (NYC) (humid to sub-humid) and Austin, Texas (humid subtropical). Inputs combine selected Landsat-8 spectral indices, a digital elevation model, and meteorological covariates. LST targets are retrieved from Landsat-8 thermal band 10 (single-c...A compact physics-informed neural network (PINN) is developed to (i) quantify city-scale accuracy of 30 m urban land surface temperature (LST) maps, (ii) identify influential predictors, and (iii) contrast climate-dependent patterns between New York City (NYC) (humid to sub-humid) and Austin, Texas (humid subtropical). Inputs combine selected Landsat-8 spectral indices, a digital elevation model, and meteorological covariates. LST targets are retrieved from Landsat-8 thermal band 10 (single-channel), quality-screened, and resampled to 30 m for May–September 2023. The loss combines data mean squared error term with a lightweight temporal smoothness prior implemented as a finite-difference term (Δ𝑇⁄Δ𝑡) on same-pixel pairs to reflect heat storage behaviour and discourage unrealistically rapid day to day changes. On the study pixels (in-sample), performance reaches R² = 0.88 (RMSE = 1.2 °C) in NYC and R² = 0.91 (RMSE = 0.9 °C) in Austin; errors are approximately Gaussian with minimal bias. Feature patterns differ by climate: vegetation-related signals dominate cooling in NYC, whereas shortwave-radiation and impervious-surface proxies (e.g., NDBI/NDISI) are strongest in Austin. These findings show that a shallow PINN with a minimal temporal constraint yields accurate, interpretable LST maps suitable for urban-heat-island assessment and climate-sensitive heat-mitigation planning.» weiterlesen» einklappen

  • Land Surface Temperature (LST)
  • Landsat-8
  • Urban Heat Island (UHI)
  • Physics-Informed Neural Network (PINN)
  • Spectral Indices
  • Meteorological Variables

Autoren


Ghanbari, Ronak (Autor)
Linderman, Marc (Autor)
Torabzadeh, Hossein (Autor)
Heidari Mozaffar, Morteza (Autor)

Klassifikation


DFG Fachgebiet:
3.43-02 - Geodäsie, Photogrammetrie, Fernerkundung, Geoinformatik, Kartographie

DDC Sachgruppe:
Geowissenschaften

Verknüpfte Personen