尼日利亚联邦首都地区Kubwa土地利用覆盖和地表温度的变化

Y. A. Abbas, O. O. Morenikeji, M. Dalil, C. Ohadugha, H. Musa
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摘要

城市地区内人类活动的增加带来了土地/土地覆盖格局的巨大变化,并对城市生态系统的变化产生了明显的影响,使城市地区变得脆弱。这些转换导致许多微、中尺度气候的出现,比原始气候和周围地区的气候温暖。本文分析了库巴、FCT、阿布贾等城市地表温度变化对植被覆盖损失的影响。该研究使用了1990年、2000年、2010年和2020年的陆地卫星图像来分析土地覆盖变化和地表温度。研究显示,从1990年到2000年,建成区面积增长了166%,2010年增长了80%,2020年平均增长了23%。1990 -2000年间,裸露地表减少了-25%;2010-2020年间,从3028.5公顷进一步减少到1979.6公顷,减少了14%。研究确定1990年库布瓦的地表温度分别为15℃和32.4℃,平均值为23.7℃。库巴2000年最小和最大地表温度分别为25℃和35℃,平均为30℃。2010年最小和最大地表温度分别为25℃和35℃,平均为30℃;2020年最小和最大地表温度分别为25℃和40℃,平均为32.5℃。分析显示,1990年、2000年和2010年的温度变化增加了0.4°C。2010年至2020年期间,由于城市扩张、基础设施发展、人口增长和人为活动,地表温度升高了2°C。该研究建议改善城市绿色基础设施;林业局应开展植树造林工作,以恢复研究区植被覆盖的枯竭。
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Variation in land use cover and surface temperature of Kubwa, Federal Capital Territory, Nigeria
Increasing human activity within the urban area brings massive changes in Land/Land Cover patterns and has an obvious effect of changes to urban ecosystems that make urban areas fragile. These conversions result in the appearance of numerous micro and mesoscale climates, warmer than the original climate and that of surrounding areas. This paper analyzed urban surface temperature variation on vegetal cover loss in Kubwa, FCT, Abuja. The study employed the used Landsat imageries of (1990, 2000, 2010 and 2020) to analyse land cover changes and land surface temperature. The study revealed that built-up area increase from 1990-2000 with 166% and 80% in 2010 and the year 2020 recorded an average of 23%. Bare surface decreased by -25% between (1990 -2000); further decreased from 3028.5 to 1979.6 hectares and -14% between 2010-2020. The study established that the LST value in 1990 Kubwa was 15℃ and 32.4℃ with a mean value of 23.7℃. The minimum and maximum LST of Kubwa in 2000 was 25℃ and 35℃ with mean of 30℃. The trend further continues, in the year 2010, minimum and maximum LST of 25℃ and 35℃ with a mean of 30℃ and in 2020 with a minimum and maximum LST of 25℃ and 40℃ with mean of 32.5℃. The analysis revealed that temperature variation increases between 1990, 2000, and 2010 were 0.4°C. There was 2°C in LST between the 2010 and 2020 due to urban expansion, infrastructure development, population growth and anthropogenic activities. The study recommends improvements of urban green infrastructure; and the FCT administration should embark into afforestation in order to restore the depleted vegetal land cover of the study area.
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