2019
DOI: 10.1126/sciadv.aau4299
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Urban heat island: Aerodynamics or imperviousness?

Abstract: More than half of the world’s population now live in cities, which are known to be heat islands. While daytime urban heat islands (UHIs) are traditionally thought to be the consequence of less evaporative cooling in cities, recent work sparks new debate, showing that geographic variations of daytime UHI intensity were largely explained by variations in the efficiency with which urban and rural areas convect heat from the land surface to the lower atmosphere. Here, we reconcile this debate by demonstrating that… Show more

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Cited by 237 publications
(172 citation statements)
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References 31 publications
(54 reference statements)
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“…3.1. Spatial anomaly of temperature and moisture Similar to other cities, Madison is largely influenced by the local effect of urbanization and surface heterogeneity (Li et al 2019), where a remarkable intraurban spatial variability of temperature and absolute humidity are observed with a strong seasonality (e.g., figure 1 for July and figure S3 is available online at stacks.iop. org/ERL/15/034041/mmedia for January).…”
Section: Resultsmentioning
confidence: 86%
“…3.1. Spatial anomaly of temperature and moisture Similar to other cities, Madison is largely influenced by the local effect of urbanization and surface heterogeneity (Li et al 2019), where a remarkable intraurban spatial variability of temperature and absolute humidity are observed with a strong seasonality (e.g., figure 1 for July and figure S3 is available online at stacks.iop. org/ERL/15/034041/mmedia for January).…”
Section: Resultsmentioning
confidence: 86%
“…Thus, it is critical to understand clearly the urbanization effects on winds and their feedback to the urban environment. Secondly, because reduced evaporative cooling in cities is among the dominant drivers of the urban heat island (UHI) phenomenon (Zhao et al 2014, Li et al 2019a, the reduction in wind speed by urbanization and associated reduction in evaporation will further enhance UHI (McVicar et al 2012). In conclusion, our results emphasize the importance of considering the wind-related urbanization effects in addition to the traditional hotspottemperature, for better understanding and predicting of the environment change in urban areas.…”
Section: Discussionmentioning
confidence: 73%
“…Both observational and modeling studies show that urbanization can be significantly related to the reduced surface wind speed in Beijing , Hou et al 2013. The potential impact of urbanization on surface wind speed has also been identified in large cities in China (Wu et al 2016, 2019a, Peng et al 2018. The declining trends in surface wind speed show large regional variations in China with relatively smaller decreases in southern regions compared to northern regions (Shi et al 2015), indicating that background regional climate changes may partly counteract the urbanization effect.…”
Section: Introductionmentioning
confidence: 98%
“…The rapid increase in land surface temperature (LST) and increased UHI are primarily resulting from expanding urban developed land which encroaches upon cultivated land, grassland, and forest land [2,3]. During the process of urbanization, constant changes in underlying surface features and land use cover result in decreased latent heat flux and the increased sensible heat flux, which are the root causes of an increased UHI effect [4]. At present, the urban heat problem is no longer a simple climate and environmental issue, but a major risk to the sustainable development of the urban environment [5].…”
Section: Introductionmentioning
confidence: 99%
“…At present, research on urban heat environment risk focuses on mapping heat risk and vulnerability in various environments [5][6][7], especially in the context of global climate change and heat waves [8][9][10]. Researchers have endeavored to employ theoretical and technical methods, such as statistical [11][12][13][14][15][16][17][18][19], energy-balance [3,4,20], numerical [21][22][23], analytical [24], and physical models [25]. For this process, researchers usually grade and evaluate air temperature data from meteorological stations and the LST data observed via remote sensing from the perspective of climate vulnerability or human exposure [26], and developed some vulnerability and risk indexes, such as manual indicator removal [27], as well as more complicated techniques, such as Monte Carlo simulation and variance-based global sensitivity analysis [28].…”
Section: Introductionmentioning
confidence: 99%