Abstract:Surface temperature is often used to examine heat exposure in multi‐city studies and for informing urban heat mitigation efforts due to scarcity of urban air temperature measurements. Cities also have lower relative humidity, traditionally not accounted for in large‐scale observational urban heat risk assessments. Here, using crowdsourced measurements from over 40,000 weather stations in ≈600 urban clusters in Europe, we show the moderating effect of this urbanization‐induced humidity reduction on outdoor heat… Show more
“…Moreover, it is also one of the first to use these methods to predict the spatial variability of RH, and thus estimates of ambient moist heat stress. We find that, when combined with other ancillary information, satellite-derived LST can be a strong predictor of ambient air temperature, even though using LST directly as a proxy for urban heat exposure may be misleading (Chakraborty et al 2022, Turner et al 2022. Overall, since our ML model identified LST from both the Landsat two-month average and the closest time period as being the variables contributing the most predictive power to our model, this means that the air temperature variability is embedded within LST variability, as reflected in the feature importance scores (figure 2).…”
Section: Discussionmentioning
confidence: 90%
“…Studies have found positive correlation between satellite-derived LST and air temperature (Mildrexler et al 2011, Zhang et al 2014, particularly during nighttime (Chakraborty et al 2022), and LST data have been widely used as a proxy for urban heat exposure in the past (Chakraborty et al 2019, Manoli et al 2019, Hoffman et al 2020, Hsu et al 2021, McDonald et al 2021, Mentaschi et al 2022. In this study, the LST data from satellite sensors Landsat 8 and MODIS were examined, since both data sources have their advantages and trade-offs.…”
Through conversion of land cover to more built-up, impervious surfaces, cities create hotter environments than their surroundings for urban residents, with large differences expected between different parts of the city. Existing measurements of ambient air temperature and heat stress, however, are often insufficient to capture the intra-urban variability in heat exposure. This study provides a replicable method for modeling air temperature, humidity, and moist heat stress over the urban area of Chapel Hill while engaging citizens to collect high-temporal and spatially-resolved air temperature and humidity measurements. We use low-cost, consumer-grade sensors combined with satellite remote sensing data and machine learning to map urban air temperature and relative humidity over various land-cover classes to understand intra-urban spatial variability of ambient heat exposure at a relatively high resolution (10 meters). Our findings show that individuals may be exposed to higher levels of air temperature and moist heat stress than weather station data suggest, and that the ambient heat exposure varies according to land cover type, with tree-covered land the coolest and built-up areas the warmest, and time of day, with higher air temperatures observed during the early afternoon. Combining our resulting dataset with sociodemographic data, policymakers and urban planners in Chapel Hill can use data output from this method to identify areas exposed to high temperature and moist heat stress as a first step to design effective mitigation measures.
“…Moreover, it is also one of the first to use these methods to predict the spatial variability of RH, and thus estimates of ambient moist heat stress. We find that, when combined with other ancillary information, satellite-derived LST can be a strong predictor of ambient air temperature, even though using LST directly as a proxy for urban heat exposure may be misleading (Chakraborty et al 2022, Turner et al 2022. Overall, since our ML model identified LST from both the Landsat two-month average and the closest time period as being the variables contributing the most predictive power to our model, this means that the air temperature variability is embedded within LST variability, as reflected in the feature importance scores (figure 2).…”
Section: Discussionmentioning
confidence: 90%
“…Studies have found positive correlation between satellite-derived LST and air temperature (Mildrexler et al 2011, Zhang et al 2014, particularly during nighttime (Chakraborty et al 2022), and LST data have been widely used as a proxy for urban heat exposure in the past (Chakraborty et al 2019, Manoli et al 2019, Hoffman et al 2020, Hsu et al 2021, McDonald et al 2021, Mentaschi et al 2022. In this study, the LST data from satellite sensors Landsat 8 and MODIS were examined, since both data sources have their advantages and trade-offs.…”
Through conversion of land cover to more built-up, impervious surfaces, cities create hotter environments than their surroundings for urban residents, with large differences expected between different parts of the city. Existing measurements of ambient air temperature and heat stress, however, are often insufficient to capture the intra-urban variability in heat exposure. This study provides a replicable method for modeling air temperature, humidity, and moist heat stress over the urban area of Chapel Hill while engaging citizens to collect high-temporal and spatially-resolved air temperature and humidity measurements. We use low-cost, consumer-grade sensors combined with satellite remote sensing data and machine learning to map urban air temperature and relative humidity over various land-cover classes to understand intra-urban spatial variability of ambient heat exposure at a relatively high resolution (10 meters). Our findings show that individuals may be exposed to higher levels of air temperature and moist heat stress than weather station data suggest, and that the ambient heat exposure varies according to land cover type, with tree-covered land the coolest and built-up areas the warmest, and time of day, with higher air temperatures observed during the early afternoon. Combining our resulting dataset with sociodemographic data, policymakers and urban planners in Chapel Hill can use data output from this method to identify areas exposed to high temperature and moist heat stress as a first step to design effective mitigation measures.
“…Hence, fine-scale LST observations can still provide valuable insights into intracity temperature gradients and complexities at detailed levels that are difficult to achieve with meteorological temperature data alone. Moving forward, more urban-scale in situ observations of air temperature and other relevant meteorological variables are urgently needed to better understand urban heat exposure ( 26 ).…”
Cities worldwide are experiencing record-breaking summer temperatures. Urban environments exacerbate extreme heat, resulting in not only the urban heat island but also intracity variations in heat exposure. Understanding these disparities is crucial to support equitable climate mitigation and adaptation efforts. We found persistent negative correlations between daytime land surface temperature (LST) and median household income across the Los Angeles metropolitan area based on Ecosystem Spaceborne Thermal Radiometer Experiment on Space Station observations from 2018 to 2021. Lower evapotranspiration resulting from the unequal distribution of vegetation cover is a major factor leading to higher LST in low-income neighborhoods. Disparities worsen with higher regional mean surface temperature, with a $10,000 decrease in income leading to ~0.2°C LST increase at 20°C and up to ~0.7°C at 45°C. With more frequent and intense heat waves projected in the future, equitable mitigation measures, such as increasing surface albedo and tree cover in low-income neighborhoods, are necessary to address these disparities.
“…Additionally, different data processing techniques applied to this study compared to the previous studies might have resulted in different outcomes. t is challenging to explain heat measures' relationship with the individual variable comparison results directly since the effect of RH on HI is nonlinear according to Ta increase, and WBGT is the weighted sum of natural wet bulb temperature, black globe temperature, and air temperature (Chakraborty et al, 2022).…”
Extreme heat is a great threat to human health, and a growing public health concern, with recent higher intensity and duration of heat days coupled with increasing population exposure to hot environments. Utilizing accurate weather information and measures that reflect what people experience is a key component to understanding extreme heat impacts on human health. Numerous studies have suggested various heat metrics Heat Index (HI) and Wet Bulb Globe Temperature (WBGT) have been widely used in heat exposure guidelines. However, there are few systematic comparisons of daily heat measures and weather variables such as daily relative humidity, wind speed, and solar radiation which are highly related to human body thermoregulation and physiologic impact of heat. We compared three relevant heat measures (HImax, WBGTBernard, and WBGTLiljegren), derived from three widely-used gridded weather datasets (ERA5, PRISM, and Daymet) with ground-based weather observations. The heat measures calculated from gridded weather data and station data showed fairly strong agreement (R2 0.82–0.96, Root Mean Square Error (RMSE) 1.69–5.37°C). However, the discrepancies varied according to Köppen-Geiger climates (e.g., Adjusted R2 HImax (0.61–0.96), WBGTBernard (0.64–0.94), and WBGTLiljegren (0.34–0.94)). Gridded weather datasets offer a fairly reliable approach to assessing heat exposure of meteorological variables and heat measures. However, further research and establishing local ground station networks are necessary to reduce exposure measurement error and improve accuracy to ultimately better and more robustly understand the links between humid heat and health outcomes.
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