快速城市化半干旱城市的地表热动力学和空气质量压力源:约旦大伊尔比德多传感器卫星评估(2000-2025)

IF 2.1 4区 地球科学
Bushra Obeidat, Mohammed J. Alshayeb, Javed Mallick
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引用次数: 0

摘要

中东的半干旱城市面临着来自城市快速增长、气温上升和持续空气污染的多重压力,但二级城市的长期证据仍然很少。方法本研究使用一个集成的多传感器卫星框架,研究了约旦大伊尔比德25年的日间地表热变化和当今的空气质量状况。利用Landsat 5、8和9 Collection 2 Level-2 2000 - 2025年6个时期的地表温度(LST)数据,基于全球人类住区层(GHSL)建筑地表的高程控制的农村参考,计算了白天地表热岛强度。根据Sentinel-5P对流层监测仪器(TROPOMI) 2019-2025年的记录,研究了五种空气质量压力源,即二氧化氮(NO2)、二氧化硫(SO2)、一氧化碳(CO)、甲醛(HCHO)和紫外线气溶胶指数(AI),以及两个背景变量臭氧(O3)和甲烷(CH4)。结果在研究的两个终点之间,该城市表现出典型的旱地地表冷岛,从- 6.26°C减弱到- 4.14°C,但在中间的几个时期,这种对比并非单调的。这种减弱与密集城市核心的2.2倍增长密切相关(r = 0.977, 95%置信区间0.80-1.00),并与密度驱动的相对变暖相一致。NO2在城市核心区达到峰值,冬夏比为1.93,HCHO和气溶胶在夏季达到峰值,CH4跟踪全球背景上升,证实了反演的一致性。结论研究结果确定了一个东南向地表热升高与污染加剧相对应的区域,为旱地城市的降温、绿化和排放管理提供了可复制的证据基础。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Surface thermal dynamics and air quality stressors in a rapidly urbanising semi-arid city: a multi-sensor satellite assessment of Greater Irbid, Jordan (2000–2025)

Background

Semi-arid cities of the Middle East face compounding pressures from rapid urban growth, rising temperatures and persistent air pollution, yet long-term evidence for secondary cities remains scarce.

Methods

This study examined twenty-five years of daytime surface thermal change and the present-day air quality regime of Greater Irbid, Jordan, using an integrated multi-sensor satellite framework. Land surface temperature (LST) was retrieved from Landsat 5, 8 and 9 Collection 2 Level-2 archives for six epochs between 2000 and 2025, and daytime surface thermal island intensity was computed against an elevation-controlled rural reference derived from epoch-matched Global Human Settlement Layer (GHSL) built-up surfaces. Five air quality stressors, namely nitrogen dioxide (NO2), sulphur dioxide (SO2), carbon monoxide (CO), formaldehyde (HCHO) and the ultraviolet aerosol index (AI), together with two contextual variables, ozone (O3) and methane (CH4), were characterised from Sentinel-5P TROPOspheric Monitoring Instrument (TROPOMI) records for 2019–2025.

Results

The city exhibited a daytime surface urban cool island typical of drylands that weakened from − 6.26 °C to − 4.14 °C between the study endpoints, though the contrast was not monotonic across the intervening epochs. This weakening was strongly associated with the 2.2-fold growth of the dense urban core (r = 0.977, 95 per cent confidence interval 0.80–1.00) and is consistent with densification-driven relative warming. NO2 peaked over the urban core with a winter to summer ratio of 1.93, HCHO and aerosols peaked in summer and CH4 tracked the global background rise, confirming retrieval consistency.

Conclusion

The results identify an east–south belt where elevated surface heat visually corresponds with pollution enhancements and provide a reproducible evidence base for cooling, greening and emission management in dryland municipalities.

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来源期刊
Acta Geophysica
Acta Geophysica GEOCHEMISTRY & GEOPHYSICS-
CiteScore
3.80
自引率
13.00%
发文量
251
期刊介绍: Acta Geophysica is open to all kinds of manuscripts including research and review articles, short communications, comments to published papers, letters to the Editor as well as book reviews. Some of the issues are fully devoted to particular topics; we do encourage proposals for such topical issues. We accept submissions from scientists world-wide, offering high scientific and editorial standard and comprehensive treatment of the discussed topics.
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