Spatio-Temporal Modeling of the Urban Heat Island in the Phoenix Metropolitan Area: Land Use Change Implications
Abstract
This study examines the spatial and temporal patterns of the surface urban heat island (SUHI) intensity in the Phoenix metropolitan area and the relationship with land use land cover (LULC) change between 2000 and 2014. The objective is to identify specific regions in Phoenix that have been increasingly heated and cooled to further understand how LULC change influences the SUHI intensity. The data employed include MODerate-resolution Imaging Spectroradiometer (MODIS) land surface temperature (LST) 8-day composite June imagery, and classified LULC maps generated using 2000 and 2014 Landsat imagery. Results show that the regions that experienced the most significant LST changes during the study period are primarily on the outskirts of the Phoenix metropolitan area for both daytime and nighttime. The conversion to urban, residential, and impervious surfaces from all other LULC types has been identified as the primary cause of the UHI effect in Phoenix. Vegetation cover has been shown to significantly lower LST for both daytime and nighttime due to its strong cooling effect by producing more latent heat flux and less sensible heat flux. We suggest that urban planners, decision-makers, and city managers formulate new policies and regulations that encourage residential, commercial, and industrial developers to include more vegetation when planning new construction.
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The combination of urban surfaces and reduced vegetation creates steep temperature gradients between densely populated urban centers and their surroundings, with urban areas containing higher temperatures.
“The combination of urban surfaces and reduced vegetation create steep temperature gradients between densely populated urban centers and their surroundings, with urban areas containing higher temperatures (Trlica et al., 2017; Wang et al., 2016).”
From Review of emerging contaminants in green stormwater infrastructure: antibiotic resistance genes, microplastics, tire wear particles, PFAS, and temperature (2024) · cites this paper as Wang et al., 2016
The Discussion (section 5; page unavailable) links impervious surfaces and reduced vegetation to higher land-surface temperatures and urban heat-island effects. It does not establish steep gradients centered on densely populated urban cores; instead, it says the largest increases in urban–rural temperature difference occurred on the city outskirts, not within developed areas. (LLM, conf=0.84)
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Sorted by citations
Liu, W., Agusdinata, D. B., & Myint, S. W. (2019) · International Journal of Applied Earth Observation and Geoinformation · doi:10.1016/j.jag.2019.04.016 · Cited by 162 · see citing works
Self-citationBodus, B., O'Malley, K., Dieter, G., Gunawardana, C., & McDonald, W. (2024) · Science of The Total Environment · doi:10.1016/j.scitotenv.2023.167195 · Cited by 76 · see citing works
- Authors
- Wang, C., Myint, S., Wang, Z., & Song, J.
- Affiliations
- School of Geographical Sciences and Urban Planning, Arizona State University, Tempe, AZ 85287, USA
- School of Sustainable Engineering and the Built Environment, Arizona State University, Tempe, AZ 85287, USA
- ORCID
- Wang, Chuyuan
- Venue
- Remote Sensing
- Publisher
- MDPI AG
- Published
- 2016-02-26
- Volume
- 8
- Issue
- 3
- Pages
- 185
- ISSN
- 2072-4292
- Cited by
- 119
- References
- 1
- Language
- en
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