Department of Civil Engineering Sciences, Faculty of Engineering and the Built Environment, University of Johannesburg, P. O. Box 524, APK Campus, Auckland Park, Johannesburg, 2006, South Africa.
Department of Water, Atmosphere and Environment, University of Natural Resources and Applied Life Sciences, Vienna, Austria.
Environ Monit Assess. 2019 Apr 13;191(5):278. doi: 10.1007/s10661-019-7439-7.
In this study, the effect of land use-land cover change (LULCC) on surface (direct) runoff was estimated for Lake Basaka catchment using the soil conservation services-curve number model in the geospatial information system (ArcInfo), assisted by remote sensing. The result indicated that Lake Basaka catchment experienced a significant LULCC. About 86% of forest coverage and 46% of grasslands were lost over the study period (1973-2015), which were shifted to open bushy woodlands, farms, lake water and wetlands. The runoff responses were observed to be increasing since 1970s, especially after the inception of large-scale irrigation schemes to the region. The highest increase of surface runoff was observed to occur after mid-1980s, which is in line with the significant LULCC and the corresponding increment of lake level in that period. The reduction in vegetation cover has resulted in an increase of runoff coefficient (r) from 0.07 in the 1960s to about 0.23 in 2000s. The sensitivity analysis result indicated that about 70% of the increase runoff rate in the lake catchment is attributed to LULCC, and the remaining proportion is due to rainfall. However, the effect of extreme rainfall on runoff process could not be underemphasized since it has significant impact especially during extreme events (observed r of 0.33 in 2008). Overall, when predicting the runoff response of the lake catchment, it is importance to take into account possible future LULCC and evolution.
本研究利用地理信息系统(ArcInfo)中的土壤保持服务-曲线数模型,结合遥感技术,估算了湖泊巴萨卡流域土地利用/土地覆被变化(LULCC)对地表(直接)径流量的影响。结果表明,湖泊巴萨卡流域经历了显著的 LULCC。在研究期间(1973-2015 年),约 86%的森林覆盖和 46%的草地消失,转变为开阔的灌木林地、农田、湖泊水和湿地。自 20 世纪 70 年代以来,径流量呈上升趋势,尤其是在该地区开始大规模灌溉计划之后。最高的地表径流量增加发生在 20 世纪 80 年代中期之后,这与当时显著的 LULCC 以及相应的湖泊水位上升相一致。植被覆盖减少导致径流系数(r)从 20 世纪 60 年代的 0.07 增加到 21 世纪 00 年代的约 0.23。敏感性分析结果表明,流域内约 70%的径流量增加归因于 LULCC,其余部分归因于降雨。然而,极端降雨对径流过程的影响不容忽视,因为它在极端事件中(观测到的 2008 年 r 值为 0.33)具有重大影响。总的来说,在预测湖泊流域的径流量响应时,考虑到可能的未来 LULCC 和演变是很重要的。