Fajary Faiz Rohman, Lee Han Soo, Kubota Tetsu, Bhanage Vinayak, Pradana Radyan Putra, Nimiya Hideyo, Putra I Dewa Gede Arya
Transdisciplinary Science and Engineering Program, Graduate School of Advanced Science and Engineering, Hiroshima University, 1-5-1 Kagamiyama, Higashi-Hiroshima, 739-8529, Hiroshima, Japan.
Atmospheric Science Research Group, Faculty of Earth Science and Technology, Institut Teknologi Bandung, Bandung, 40132, West Java, Indonesia.
Heliyon. 2024 Jun 27;10(13):e33708. doi: 10.1016/j.heliyon.2024.e33708. eCollection 2024 Jul 15.
Urban heat island (UHI) and thermal comfort conditions are among the impacts of urbanization, which have been extensively studied in most cities around the world. However, the comprehensive studies in Indonesia in the context of urbanization is still lacking. This study aimed to classify land use and land cover (LULC) and analyse urban growth and its effects on surface urban heat islands (SUHIs) and urban thermal conditions as well as contributing factors to SUHI intensity (SUHII) using remote sensing in the western part of Java Island and three focused urban areas: the Jakarta metropolitan area (JMA), the Bandung and Cimahi Municipalities (BC), and the Sukabumi Municipality (SKB). Landsat imagery from three years was used: 2000, 2009, and 2019. Three types of daytime SUHII were quantified, namely the SUHII of urban central area and two SUHIIs of urban sprawl area. In the last two decades, urban areas have grown by more than twice in JMA and SKB and nearly 1.5 times in BC. Along with the growth of the three cities, the SUHII in the urban central area has almost reached a magnitude of 6 °C in the last decade. Rates of land surface temperature change of the unchanged urban pixels have magnitudes of 0.25, 0.15, and 0.14 °C/year in JMA, SKB, and BC, respectively. The urban thermal field variance index (UTFVI) and discomfort index (DI) showed that the strongest SUHI effect was most prevalent in urban pixels and the regions were mostly in the and categories. Anthropogenic heat flux and urban ratio have positive contributions to SUHII variation, while vegetation and water ratios are negative contributors to SUHII variation. For each city, the contributing factors have a unique magnitude that can be used to evaluate SUHII mitigation options.
城市热岛(UHI)和热舒适状况是城市化的影响因素之一,在世界上大多数城市都已得到广泛研究。然而,印度尼西亚在城市化背景下的综合研究仍然不足。本研究旨在利用遥感技术对爪哇岛西部以及三个重点城市地区(雅加达大都市区(JMA)、万隆和芝马希市(BC)以及茂物市(SKB))的土地利用和土地覆盖(LULC)进行分类,并分析城市增长及其对地表城市热岛(SUHIs)和城市热状况的影响,以及SUHI强度(SUHII)的影响因素。使用了来自2000年、2009年和2019年这三年的陆地卫星图像。对三种类型的白天SUHII进行了量化,即城市中心区域的SUHII和城市蔓延区域的两种SUHII。在过去二十年中,JMA和SKB的城市面积增长了两倍多,BC的城市面积增长了近1.5倍。随着这三个城市的发展,城市中心区域的SUHII在过去十年中几乎达到了6°C的幅度。JMA、SKB和BC中未变化的城市像素的地表温度变化率分别为每年0.25°C、0.15°C和0.14°C。城市热场方差指数(UTFVI)和不适指数(DI)表明,最强的SUHI效应在城市像素中最为普遍,这些区域大多属于 和 类别。人为热通量和城市比率对SUHII变化有正向贡献,而植被和水的比率对SUHII变化有负向贡献。对于每个城市,影响因素具有独特的幅度,可用于评估SUHII缓解方案。