Assessment of U.S. Urban Surface Temperature using GOES-16 and 17 Data: Urban Heat Island and Temperature Inequality

Jangho Lee
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Abstract

This study utilizes hourly Land Surface Temperature (LST) data from the Geostationary Operational Environmental Satellite (GOES) to analyze the seasonal and diurnal characteristics of Surface Urban Heat Island Intensity (SUHII) across 120 of the largest U.S. cities and its surroundings. Distinct patterns emerge in the classification of seasonal daytime and nighttime SUHII. Specifically, vegetation index (EVI) and albedo (ALB) play pivotal roles in influencing these temperature variations. The diurnal cycle of SUHII further reveals different trends, suggesting that climate conditions, urban and non-urban land covers, and anthropogenic activities during nighttime hours affect SUHII peaks. Exploring intracity LST dynamics, the study reveals a significant correlation between urban intensity (UI) and LST, with LST rising as UI increases. Notably, populations identified as more vulnerable by the Social Vulnerability Index (SVI) are found in high UI regions. This results in a discernible LST inequality, where the more vulnerable communities are under higher LST conditions, possibly leading to higher heat exposure. This comprehensive study accentuates the significance of tailoring city-specific climate change mitigation strategies, illuminating LST variations and their intertwined societal implications.
利用 GOES-16 和 17 数据评估美国城市地表温度:城市热岛和温度不均
本研究利用地球静止业务环境卫星(GOES)提供的每小时陆地表面温度(LST)数据,分析了美国 120 个最大城市及其周边地区的地表城市热岛强度(SUHII)的季节和昼夜特征。在对季节性白天和夜间 SUHII 进行分类时发现了不同的模式。具体来说,植被指数(EVI)和反照率(ALB)在影响这些温度变化方面起着关键作用。SUHII 的昼夜周期进一步揭示了不同的趋势,表明气候条件、城市和非城市土地覆盖以及夜间的人为活动影响着 SUHII 的峰值。在探索城市内低温层动态时,研究发现城市强度(UI)与低温层之间存在显著相关性,随着 UI 的增加,低温层也随之升高。值得注意的是,被社会脆弱性指数(SVI)确定为更脆弱的人群位于高 UI 区域。这导致了明显的 LST 不平等,即更脆弱的社区处于更高的 LST 条件下,可能导致更高的热暴露。这项综合研究强调了针对具体城市制定气候变化减缓战略的重要性,揭示了低热层的变化及其相互交织的社会影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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