Characterization of the urban heat Island effect from remotely sensed data based on a hierarchical model

This study attempts to statistically characterize the Urban Heat Island Intensity (UHII) (ΔT) for 55 cities under three climate regimes – arid, snow and temperate – across the US. The study uses remotely sensed data products, daily temperature from MODIS and daily evapotranspiration from SSEBop mode...

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Main Authors: Lucas Ford, Dingbao Wang, Mukesh Kumar, A. Sankarasubramanian
Format: Article
Language:English
Published: Elsevier 2024-12-01
Series:Journal of Hydrology X
Online Access:http://www.sciencedirect.com/science/article/pii/S2589915524000142
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author Lucas Ford
Dingbao Wang
Mukesh Kumar
A. Sankarasubramanian
author_facet Lucas Ford
Dingbao Wang
Mukesh Kumar
A. Sankarasubramanian
author_sort Lucas Ford
collection DOAJ
description This study attempts to statistically characterize the Urban Heat Island Intensity (UHII) (ΔT) for 55 cities under three climate regimes – arid, snow and temperate – across the US. The study uses remotely sensed data products, daily temperature from MODIS and daily evapotranspiration from SSEBop model, to calculate the urban–rural difference in daily-mean temperature and daily-mean evapotranspiration (ΔT and ΔET respectively) for the selected cities. By developing a hierarchical model that explains UHII using temporally-varying ΔET and spatially-varying urban morphometric characteristics (total urban area and percentage impervious area) available for each city, we find that 89% of the spatio-temporal variability in annual ΔT can be explained. The relationship between ΔT and ΔET is found to be negative indicating increased difference in daily means of ET (ΔET) result in increased difference in daily means of temperature (ΔT) between urban and rural paracels The variation of ΔT per unit ΔET is found to be highest in arid and snowy environments and smallest in temperate environments in the south-southeast US. The relation between ΔT and ΔET is negative for most cities, except Madison (WI) and Sacramento (CA), across the US. Both the selected urban morphometric properties are found to be statistically significant in explaining the spatial variability in UHII, but the difference in urban–rural difference in evapotranspiration is the primary driver for UHII.
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spelling doaj-art-09342f4c41d54fb1b617d7e5f91fae042024-11-23T06:31:30ZengElsevierJournal of Hydrology X2589-91552024-12-0125100184Characterization of the urban heat Island effect from remotely sensed data based on a hierarchical modelLucas Ford0Dingbao Wang1Mukesh Kumar2A. Sankarasubramanian3Department of Civil, Construction and Environmental Engineering, North Carolina State University, Raleigh, NC, USADepartment of Civil, Environmental and Construction Engineering, University of Central Florida, Orlando, FL, USADepartment of Civil, Construction and Environmental Engineering, University of Alabama, Tuscaloosa, AL, USADepartment of Civil, Construction and Environmental Engineering, North Carolina State University, Raleigh, NC, USA; Corresponding author.This study attempts to statistically characterize the Urban Heat Island Intensity (UHII) (ΔT) for 55 cities under three climate regimes – arid, snow and temperate – across the US. The study uses remotely sensed data products, daily temperature from MODIS and daily evapotranspiration from SSEBop model, to calculate the urban–rural difference in daily-mean temperature and daily-mean evapotranspiration (ΔT and ΔET respectively) for the selected cities. By developing a hierarchical model that explains UHII using temporally-varying ΔET and spatially-varying urban morphometric characteristics (total urban area and percentage impervious area) available for each city, we find that 89% of the spatio-temporal variability in annual ΔT can be explained. The relationship between ΔT and ΔET is found to be negative indicating increased difference in daily means of ET (ΔET) result in increased difference in daily means of temperature (ΔT) between urban and rural paracels The variation of ΔT per unit ΔET is found to be highest in arid and snowy environments and smallest in temperate environments in the south-southeast US. The relation between ΔT and ΔET is negative for most cities, except Madison (WI) and Sacramento (CA), across the US. Both the selected urban morphometric properties are found to be statistically significant in explaining the spatial variability in UHII, but the difference in urban–rural difference in evapotranspiration is the primary driver for UHII.http://www.sciencedirect.com/science/article/pii/S2589915524000142
spellingShingle Lucas Ford
Dingbao Wang
Mukesh Kumar
A. Sankarasubramanian
Characterization of the urban heat Island effect from remotely sensed data based on a hierarchical model
Journal of Hydrology X
title Characterization of the urban heat Island effect from remotely sensed data based on a hierarchical model
title_full Characterization of the urban heat Island effect from remotely sensed data based on a hierarchical model
title_fullStr Characterization of the urban heat Island effect from remotely sensed data based on a hierarchical model
title_full_unstemmed Characterization of the urban heat Island effect from remotely sensed data based on a hierarchical model
title_short Characterization of the urban heat Island effect from remotely sensed data based on a hierarchical model
title_sort characterization of the urban heat island effect from remotely sensed data based on a hierarchical model
url http://www.sciencedirect.com/science/article/pii/S2589915524000142
work_keys_str_mv AT lucasford characterizationoftheurbanheatislandeffectfromremotelysenseddatabasedonahierarchicalmodel
AT dingbaowang characterizationoftheurbanheatislandeffectfromremotelysenseddatabasedonahierarchicalmodel
AT mukeshkumar characterizationoftheurbanheatislandeffectfromremotelysenseddatabasedonahierarchicalmodel
AT asankarasubramanian characterizationoftheurbanheatislandeffectfromremotelysenseddatabasedonahierarchicalmodel