Winds of Change: The Role of Urban Expansion and Thermal Advection in Driving Phoenix's (AZ) Warming Trends

Abstract Urban expansion is a significant driver of near‐surface temperature increases in modified landscapes. While research often focuses on the effect of urban environments on downstream non‐urban locations, thermal advection from upstream urban development on existing urban environments remains understudied. We analyze historical observations for rapidly and non‐rapidly expanding cities in the southwestern US to isolate the primary driver responsible for urban canopy layer warming. Results indicate increasing minimum temperatures ( T min ) of 0.0835°C/year (0.0802°C/year) and decreasing diurnal cycles of −0.0506°C/year (−0.0664°C/year) for Phoenix, AZ (Las Vegas, NV). In contrast, non‐rapidly expanding cities show negligible T min increases of 0.0005°C/year (0.021°C/year) and negligible diurnal cycle changes of +0.0035°C/year and −0.00073°C/year for Williams (AZ) and Flagstaff (AZ), respectively. To fully quantify the hypothesized first‐order effect of thermal advection in regulating canopy layer warming, we examine the role of upstream urban expansion on observed temperature changes at Phoenix' Sky Harbor International Airport using the Weather Research and Forecasting (WRF) model and idealized (semi‐Lagrangian) simulations. Two sets of WRF monthly summertime simulations (June 2002 and June 2019) are conducted, with multiple scenarios whereby the urban extent around Sky Harbor Airport is modified. Consistent with multi‐decadal observations, WRF simulations identify upstream urban expansion as the primary driver of observed near‐surface temperature changes. Semi‐Lagrangian simulations corroborate WRF results, confirming the role of thermal advection through increasing T min and decreasing diurnal cycles. Our semi‐Lagrangian model offers a computationally efficient tool to predict future minimum temperature trends due to continued urban expansion, with potential application for semi‐arid cities globally.

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Publication Details

Journal
Journal of Geophysical Research Atmospheres
Published
2025-08-14
DOI
https://doi.org/10.1029/2024jd043166
Primary Topic
Geochemistry and Geologic Mapping
Type
article
Field-Weighted Citation Impact
0.00

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article

Winds of Change: The Role of Urban Expansion and Thermal Advection in Driving Phoenix's (AZ) Warming Trends

Journal of Geophysical Research Atmospheres
Geochemistry and Geologic Mapping
article

Winds of Change: The Role of Urban Expansion and Thermal Advection in Driving Phoenix's (AZ) Warming Trends

article en

Abstract

Abstract Urban expansion is a significant driver of near‐surface temperature increases in modified landscapes. While research often focuses on the effect of urban environments on downstream non‐urban locations, thermal advection from upstream urban development on existing urban environments remains understudied. We analyze historical observations for rapidly and non‐rapidly expanding cities in the southwestern US to isolate the primary driver responsible for urban canopy layer warming. Results indicate increasing minimum temperatures ( T min ) of 0.0835°C/year (0.0802°C/year) and decreasing diurnal cycles of −0.0506°C/year (−0.0664°C/year) for Phoenix, AZ (Las Vegas, NV). In contrast, non‐rapidly expanding cities show negligible T min increases of 0.0005°C/year (0.021°C/year) and negligible diurnal cycle changes of +0.0035°C/year and −0.00073°C/year for Williams (AZ) and Flagstaff (AZ), respectively. To fully quantify the hypothesized first‐order effect of thermal advection in regulating canopy layer warming, we examine the role of upstream urban expansion on observed temperature changes at Phoenix' Sky Harbor International Airport using the Weather Research and Forecasting (WRF) model and idealized (semi‐Lagrangian) simulations. Two sets of WRF monthly summertime simulations (June 2002 and June 2019) are conducted, with multiple scenarios whereby the urban extent around Sky Harbor Airport is modified. Consistent with multi‐decadal observations, WRF simulations identify upstream urban expansion as the primary driver of observed near‐surface temperature changes. Semi‐Lagrangian simulations corroborate WRF results, confirming the role of thermal advection through increasing T min and decreasing diurnal cycles. Our semi‐Lagrangian model offers a computationally efficient tool to predict future minimum temperature trends due to continued urban expansion, with potential application for semi‐arid cities globally.

Journal of Geophysical Research AtmospheresVol. 130(16)
Arizona State University (US)
U.S. Department of Energy
Sustainable cities and communities
Openalex Percentile: Top 62%
Geochemistry and Geologic Mapping
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Winds of Change: The Role of Urban Expansion and Thermal Advection in Driving Phoenix's (AZ) Warming Trends · Journal of Geophysical Research Atmospheres (2025) | TGRS Research Map | TGRS