2019
DOI: 10.1016/j.jag.2018.09.015
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A simplified urban-extent algorithm to characterize surface urban heat islands on a global scale and examine vegetation control on their spatiotemporal variability

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Cited by 216 publications
(212 citation statements)
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“…We examine the associations between neighborhood-scale daytime surface UHI and the Δα, ΔNDVI, and ΔNDBI for each city ( figure 4). In general, we see a negative correlation between UHI and ΔNDVI, since more vegetated neighborhoods have higher evaporative cooling, and thus, lower surface temperatures, as demonstrated at various scales (Rizwan et al 2008, Peng et al 2011, Chakraborty et al 2017, Chakraborty and Lee 2019. A few cities, like Buenos Aires, Copenhagen, Melbourne, and Tokyo do show slight positive relationships between UHI and ΔNDVI.…”
Section: Physical Characteristics Of Cities and Their Impact On Uhi Imentioning
confidence: 68%
“…We examine the associations between neighborhood-scale daytime surface UHI and the Δα, ΔNDVI, and ΔNDBI for each city ( figure 4). In general, we see a negative correlation between UHI and ΔNDVI, since more vegetated neighborhoods have higher evaporative cooling, and thus, lower surface temperatures, as demonstrated at various scales (Rizwan et al 2008, Peng et al 2011, Chakraborty et al 2017, Chakraborty and Lee 2019. A few cities, like Buenos Aires, Copenhagen, Melbourne, and Tokyo do show slight positive relationships between UHI and ΔNDVI.…”
Section: Physical Characteristics Of Cities and Their Impact On Uhi Imentioning
confidence: 68%
“…Land surface temperatures (LSTs) derived from satellite sensor can be used to estimate the surface UHI (SUHI) from the contrast between urban pixels and surrounding rural ones (Zhou et al, 2019). However, the long-term trends of SUHI at the global scale were only investigated by Chakraborty and Lee (2019), showing that the trends of annual daytime and nighttime SUHII during 2003-2017 were 0.03°C per decade and 0.00°C per decade, respectively. However, the long-term trends of SUHI at the global scale were only investigated by Chakraborty and Lee (2019), showing that the trends of annual daytime and nighttime SUHII during 2003-2017 were 0.03°C per decade and 0.00°C per decade, respectively.…”
Section: Introductionmentioning
confidence: 99%
“…However, Chakraborty and Lee (2019) only computed the trends of annual mean SUHII and did not provide any seasonal differences. In addition, the data and methods in Chakraborty and Lee (2019) may lead to some uncertainties (for further discussion, see section 3.1). A systematic evaluation of SUHII and related drivers at a global scale is still needed.…”
Section: Introductionmentioning
confidence: 99%
“…Within the past decade several large-scale studies have documented a daytime 'urban cool island' effect for many dryland cities as surrounding landscapes with sparse xeric vegetation, grasses, and dry soils warm more rapidly than urban surfaces (Imhoff et al 2010, Peng et al 2014, Chakraborty and Lee 2019. Surrounding deserts then cool more rapidly at night than urban pavement and rooftops, leading to nighttime UHIs.…”
Section: Introductionmentioning
confidence: 99%