Awotwi Alfred, Anornu Geophrey Kwame, Quaye-Ballard Jonathan, Annor Thompson, Forkuo Eric Kwabena
Regional Water and Environmental Sanitation Centre Kumasi (RWESCK)World Bank Africa Centre's of Excellence Project, Department of Civil Engineering, Kwame Nkrumah University of Science and Technology (KNUST), Kumasi, Ghana.
Department of Geomatic Engineering, Kwame Nkrumah University of Science and Technology (KNUST), Kumasi, Ghana.
Heliyon. 2017 Dec 28;3(12):e00477. doi: 10.1016/j.heliyon.2017.e00477. eCollection 2017 Dec.
The Lower Pra River Basin (LPRB), located in the forest zone of southern Ghana has experienced changes due to variability in precipitation and diverse anthropogenic activities. Therefore, to maintain the functions of the ecosystem for water resources management, planning and sustainable development, it is important to differentiate the impacts of precipitation variability and anthropogenic activities on stream flow changes. We investigated the variability in runoff and quantified the contributions of precipitation and anthropogenic activities on runoff at the LPRB. Analysis of the precipitation-runoff for the period 1970-2010 revealed breakpoints in 1986, 2000, 2004 and 2010 in the LPRB. The periods influenced by anthropogenic activities were categorized into three periods 1987-2000, 2001-2004 and 2005-2010, revealing a decrease in runoff during 1987-2000 and an increase in runoff during 2001-2004 and 2005-2010. Assessment of monthly, seasonal and annual runoff depicted a significant increasing trend in the runoff time series during the dry season. Generally, runoff increased at a rate of 9.98 × 10myr, with precipitation variability and human activities contributing 17.4% and 82.3% respectively. The dominant small scale alluvial gold mining activity significantly contributes to the net runoff variability in LPRB.
下普拉河流域(LPRB)位于加纳南部的森林地带,由于降水变化和各种人为活动而发生了改变。因此,为了维持生态系统在水资源管理、规划和可持续发展方面的功能,区分降水变化和人为活动对径流变化的影响非常重要。我们调查了LPRB的径流变化,并量化了降水和人为活动对径流的贡献。对1970 - 2010年期间降水 - 径流的分析揭示了LPRB在1986年、2000年、2004年和2010年出现了断点。受人为活动影响的时期分为三个阶段:1987 - 2000年、2001 - 2004年和2005 - 2010年,结果显示1987 - 2000年径流减少,而2001 - 2004年和2005 - 2010年径流增加。对月、季和年径流的评估表明,旱季径流时间序列呈现出显著的上升趋势。总体而言,径流以9.98×10 立方米/年的速度增加,降水变化和人类活动分别贡献了17.4%和82.3%。主要的小规模冲积金矿开采活动对LPRB的净径流变化有显著贡献。