尼日利亚东南部Umuahia镇土地利用变化对城市地表温度的影响

Felix Ike, I. Mbah, C.R. Otah, J. Babington, L. Chikwendu
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引用次数: 0

摘要

热带湿热城市地区的地表暴露在大量的太阳辐射之下。增加的热量增加了城市不同的地表温度分布,导致不同的热不适阈值。本研究利用时序(1986年、2001年和2017年)陆地卫星数据,研究了土地利用变化对尼日利亚乌穆阿希亚城市温度分布的影响。研究结果表明,随着时间的推移,建成区的面积和温度会以牺牲其他土地利用为代价而增加。迁移矩阵表明,在31年的时间里,约59.88%的植被和8.23%的裸地分别变成了人工林。建成区年最高平均气温分别为1986年21.50℃、2001年22.20℃和2017年26.01℃。横跨土地用途的样带剖面图显示,水面/植被周围的地表温度上升缓慢,而在建筑和裸露的土地区域迅速上升。研究发现,1986年至2017年期间,土地覆盖发生了剧烈变化,地表温度相应升高,研究区域的水体和裸地持续减少。总体而言,人口密集地区地表温度的时空分布高于邻近的农村地区,这是城市热岛的证据。土地利用变化对城市地表温度分布的影响可以为规划人员和决策者在评估研究区域的热舒适水平和其他风险因素时提供详细的数据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effect of Land Use Changes on the Urban Surface Temperature in Umuahia Town, Southeast, Nigeria
The land surfaces of hot-humid tropical urban areas are exposed to significant levels of solar radiation. Increased heat gain adds to different land surface temperature profiles in cities, resulting in different thermal discomfort thresholds. Using multi-temporal (1986, 2001, and 2017) landsat data, this study examined the impact of land use change on urban temperature profiles in Umuahia, Nigeria. The findings revealed that over time, built-up regions grow in surface area and temperature at the expense of other land use. The transfer matrix, showed that approximately 59.88 percent of vegetation and 8.23 percent of bareland were respectively changed into built up during the course of 31 years. The highest annual mean temperature in built-up regions was 21.50°C in 1986, 22.20°C in 2001, and 26.01°C in 2017. Transect profiles across the landuses reveals that surface Temperature rises slowly around water/vegetation and quickly over built-up and bare land area. The study observed drastic changes in land cover with a corresponding increase in surface temperature for the period between 1986 and 2017 with consistent decrease in water bodies and bare land in the study area. Overall, the spatio-temporal distribution of surface temperature in densely built up areas was higher than the adjacent rural surroundings, which is evidence of Urban Heat Island. The impact of landuse change on urban surface temperature profiles could provide detailed data to planners and decision makers in evaluating thermal comfort levels and other risk considerations in the study area.
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