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Landcover Change, Land Surface Temperature, Surface Albedo and Topography in the Plateau Region of North-Central Nigeria

机译:尼日利亚中北部高原地区的土地覆盖变化,地表温度,地表反照率和地形

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This study assessed the change in some environmental parameters in the Plateau region of North-Central Nigeria (Barakinladi, Jos, and Kafachan environs) using the nexus of landcover change, land surface temperature, surface albedo, and topography. The study employed both remote sensing and statistical techniques for the period between 1986 and 2014 to analyze the dynamics between and within these environmental variables. In Barakinladi, the built up landcover change is highest (increasing from 39.53% to 47.59% between 1986 and 2014); LST ranges from 19.09 °C to 38.59 °C in 1986 and from 22.68 °C and 41.68 °C in 2014; and the albedo ranges between 0.014 and 0.154 in 1986 and 0.017 and 0.248 in 2014. In Jos, the built-up landcover occupied 34.26% in 1986 and 36.67% in 2014; LST values range between 20.83 °C and 41.33 °C in 1986 and between 21.61 °C and 42.64 °C in 2014; and the albedo ranges between 0.003 and 0.211 in 1986 and 0.15 and 0.237 in 2014. In Kafachan area, the built up landcover occupied 32.95% in 1986 and 39.01% in 2014. Urbanization and agricultural activities, including animal grazing, were responsible for the gradual loss in vegetation and increasing average LST and albedo. The results also revealed that changing landcover and topography have a relationship with surface albedo and land surface temperature, thereby impacting significantly on ecosystem services delivered by the natural system.
机译:这项研究利用土地覆盖变化,土地表面温度,地表反照率和地形的关系评估了尼日利亚中北部高原地区(Barakinladi,Jos和Kafachan周围地区)某些环境参数的变化。该研究在1986年至2014年期间采用了遥感技术和统计技术,以分析这些环境变量之间及其内部的动态。在巴拉金拉迪(Barakinladi),已建成的土地覆被变化最高(从1986年至2014年从39.53%增加到47.59%); 1986年的LST范围为19.09°C至38.59°C,2014年的范围为22.68°C和41.68°C;乔斯的积聚土地覆盖率分别为1986年的34.26%和2014年的36.67%; 1986年的0.014至0.154和2014年的0.017至0.248。 1986年的LST值介于20.83°C至41.33°C之间,2014年的LST值介于21.61°C与42.64°C之间;地表反照率在1986年的0.003至0.211和2014年的0.15至0.237之间。在Kafachan地区,已建成的土地覆盖率分别占1986年的32.95%和2014年的39.01%。城市化和农业活动(包括动物放牧)是造成这种情况的主要原因。植被损失和平均LST和反照率增加。结果还表明,变化的土地覆盖和地形与地表反照率和地表温度有关,从而对自然系统提供的生态系统服务产生重大影响。

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