Department of Architecture and Planning, College of Engineering, King Khalid University, Abha, Kingdom of Saudi Arabia.
Department of Geography, Faculty of Natural Science, Jamia Millia Islamia, New Delhi, India.
Environ Sci Pollut Res Int. 2024 Apr;31(20):29048-29070. doi: 10.1007/s11356-024-33091-6. Epub 2024 Apr 3.
Rapid urbanisation has led to significant environmental and climatic changes worldwide, especially in urban heat islands where increased land surface temperature (LST) poses a major challenge to sustainable urban living. In the city of Abha in southwestern Saudi Arabia, a region experiencing rapid urban growth, the impact of such expansion on LST and the resulting microclimatic changes are still poorly understood. This study aims to explore the dynamics of urban sprawl and its direct impact on LST to provide important insights for urban planning and climate change mitigation strategies. Using the random forest (RF) algorithm optimised for land use and land cover (LULC) mapping, LULC models were derived that had an overall accuracy of 87.70%, 86.27% and 93.53% for 1990, 2000 and 2020, respectively. The mono-window algorithm facilitated the derivation of LST, while Markovian transition matrices and spatial linear regression models assessed LULC dynamics and LST trends. Notably, built-up areas grew from 69.40 km in 1990 to 338.74 km in 2020, while LST in urban areas showed a pronounced warming trend, with temperatures increasing from an average of 43.71 °C in 1990 to 50.46 °C in 2020. Six landscape fragmentation indices were then calculated for urban areas over three decades. The results show that the Largest Patch Index (LPI) increases from 22.78 in 1990 to 65.24 in 2020, and the number of patches (NP) escalates from 2,531 in 1990 to an impressive 10,710 in 2020. Further regression analyses highlighted the morphological changes in the cities and attributed almost 97% of the LST variability to these urban patch dynamics. In addition, water bodies showed a cooling trend with a temperature decrease from 33.76 °C in 2000 to 29.69 °C in 2020, suggesting an anthropogenic influence. The conclusion emphasises the urgent need for sustainable urban planning to counteract the warming trends associated with urban sprawl and promote climate resilience.
快速的城市化进程导致了全球范围内显著的环境和气候变化,特别是在城市热岛,那里不断升高的土地表面温度(LST)对可持续城市生活构成了重大挑战。在沙特阿拉伯西南部的阿巴市,一个正在经历快速城市扩张的地区,这种扩张对 LST 的影响以及由此产生的小气候变化仍然知之甚少。本研究旨在探索城市扩张的动态及其对 LST 的直接影响,为城市规划和气候变化缓解策略提供重要的见解。使用随机森林(RF)算法对土地利用和土地覆盖(LULC)进行优化,得出的 LULC 模型在 1990 年、2000 年和 2020 年的整体准确性分别为 87.70%、86.27%和 93.53%。单窗算法促进了 LST 的推导,而马尔可夫转移矩阵和空间线性回归模型则评估了 LULC 动态和 LST 趋势。值得注意的是,建成区面积从 1990 年的 69.40 公里增长到 2020 年的 338.74 公里,而城市地区的 LST 则呈现出明显的变暖趋势,平均温度从 1990 年的 43.71°C上升到 2020 年的 50.46°C。然后,为三个十年的城市地区计算了六个景观破碎化指数。结果表明,最大斑块指数(LPI)从 1990 年的 22.78 增加到 2020 年的 65.24,斑块数量(NP)从 1990 年的 2531 个增加到 2020 年的 10710 个。进一步的回归分析强调了城市的形态变化,并将 LST 变化的近 97%归因于这些城市斑块的动态。此外,水体呈现出降温趋势,温度从 2000 年的 33.76°C下降到 2020 年的 29.69°C,这表明存在人为影响。研究结论强调了迫切需要进行可持续的城市规划,以应对与城市扩张相关的变暖趋势,并提高气候适应能力。