Preprint / Version 1

(Sub)Urban Heat Islands

Analyzing the Relationship Between Air Temperature and Impervious Surface and Distance to Coastline in Palo Alto, CA

##article.authors##

  • Jenna Mu The Kehillah School

DOI:

https://doi.org/10.58445/rars.4194

Keywords:

Urban Heat Island, Albedo, Impervious Surface, Extreme Heat

Abstract

Record-breaking temperatures are being measured across the world, and California is no exception. Extreme heat is worsened by the Urban Heat Island (UHI) Effect – where urban areas experience significantly higher surface and air temperatures than surrounding rural areas. The UHI Effect is driven by multiple environmental factors: two of which are impervious surface concentration and distance to a body of water. This study analyzes the relationship between these two variables and air temperature across three time windows—morning (6-7 AM), afternoon (3-4 pm), and evening (7-8 pm)—on a hot day in Palo Alto. This analysis, although limited to Palo Alto, informs how higher impervious surface concentrations and longer distances to water can be associated with more extreme heat. The findings in this study provide insight into how future urban planning can reduce extreme heat risk.

References

Akima, H., & Gebhardt, A. (1998). akima: Interpolation of Irregularly and Regularly Spaced Data [Dataset]. https://doi.org/10.32614/cran.package.akima

Faurie, C. (2023). Increased temperatures and child health outcomes: a systematic review. European Journal of Public Health, 33. https://doi.org/10.1093/eurpub/ckad160.1161

Nakayama, T., & Hashimoto, S. (2010). Analysis of the ability of water resources to reduce the urban heat island in the Tokyo megalopolis. Environmental Pollution, 159(8–9), 2164–2173. https://doi.org/10.1016/j.envpol.2010.11.016

Núñez-Rodríguez, S., Collazo-Riobó, C., Sedano, J., Sánchez-Iglesias, A. I., & González-Santos, J. (2025). Heat tolerance in Older Adults: A Systematic review of thermoregulation, vulnerability, environmental change, and health outcomes. Healthcare, 13(21), 2785. https://doi.org/10.3390/healthcare13212785

Oke, T. R. (1982). The energetic basis of the urban heat island. Quarterly Journal of the Royal Meteorological Society, 108(455), 1–24. https://doi.org/10.1002/qj.49710845502

Phelan, P. E., Kaloush, K., Miner, M., Golden, J., Phelan, B., Silva, H., & Taylor, R. A. (2015). Urban Heat Island: mechanisms, implications, and possible remedies. Annual Review of Environment and Resources, 40(1), 285–307.

https://doi.org/10.1146/annurev-environ-102014-021155

Völker, S., & Kistemann, T. (2011). The impact of blue space on human health and well-being – Salutogenetic health effects of inland surface waters: A review. International Journal of Hygiene and Environmental Health, 214(6), 449–460. https://doi.org/10.1016/j.ijheh.2011.05.001

Yuan, F., & Bauer, M. (2007). Comparison of impervious surface area and normalized difference vegetation index as indicators of surface urban heat island effects in Landsat imagery. Remote Sensing of Environment, 106(3), 375–386. https://doi.org/10.1016/j.rse.2006.09.003

Zou, X., Zhang, S., & Zhu, D. (2021). Impact of Urban Water Networks on Microclimate and PM2.5 Distribution in Downtown Areas: A Case Study of Wuhan. Building and Environment, 203(108073). https://doi.org/10.1016/j.buildenv.2021.108138

Ziter, C. D., Pedersen, E. J., Kucharik, C. J., & Turner, M. G. (2019). Scale-dependent interactions between tree canopy cover and impervious surfaces reduce daytime urban heat during summer. Proceedings of the National Academy of Sciences, 116(15), 7575–7580. https://doi.org/10.1073/pnas.1817561116

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Posted

2026-09-27