Rainfall and potential evapotranspiration patterns and their effects on climatic water balance in the Western Lithoral Hydrological Zone of Nigeria

Ed Ashaolu, K. Iroye
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引用次数: 11

Abstract

This study examined the climatic water balance and aridity in the Western Lithoral hydrological zone of Nigeria. Monthly climatic data from 1976-2015 collected from six Nigeria Metrological Agency (NIMET) stations located in Ikeja, Ibadan, Akure, Abeokuta, Osogbo and Ilorin were used. The climatic variables are rainfall amount, temperature, sunshine hour, relative humidity and wind speed. The FAO Penman-Monteith method was adopted in estimating the potential evapotranspiration (PET). Water balance was determined from PET and rainfall amount. The spatial and temporal pattern of rainfall amount and PET were evaluated using universal kriging interpolation method, Mann-Kendall and regression trend analysis. The results of the Mann-Kendall and regression trend analysis revealed a statistically significant (Z= 2.74, P= 0.005) upward trend in rainfall amount between 1976 and 2015. Similarly, a statistically significant (Z= 4.40, p= 0.001) increasing trend was observed in PET during the same period. Six months of water surplus (May-October) and six months of water deficit (November-April) were identified. Overall, 27 years of water deficit was discovered over the 40 years period. Water balance pattern revealed the highest annual mean water surplus (324.51 mm) in the hinterland of Idanre, Akure, and Owo rather than the coastal city of Ikeja which can be attributed to orographic effect in the hinterland. The study area with a mean Aridity index (AI) of 0.94 can still be regarded as humid environment, although the spatial variability of AI indicates that the northern part is tending towards a dry sub-humid condition (AI= 0.76). This study recommends conservation of water surplus in the wet months for the augmentation of deficit in the dry months; this will not only boost agricultural production, but also alleviate water supply problem in the study area. Keywords. Aridity index, potential evapotranspiration, water balance.
降雨和潜在蒸散模式及其对尼日利亚西部沿海水文带气候水平衡的影响
本研究考察了尼日利亚西部岩性水文区的气候水平衡和干旱状况。使用了从位于Ikeja、Ibadan、Akure、Abeokuta、Osogbo和Ilorin的六个尼日利亚气象局(NIMET)站收集的1976-2015年的月度气候数据。气候变量包括降雨量、温度、日照时数、相对湿度和风速。采用FAO Penman-Monteith方法估算潜在蒸散量(PET)。根据PET和降雨量确定水量平衡。采用通用克里格插值法、Mann-Kendall法和回归趋势分析法对降雨量和PET的时空格局进行了评价。Mann-Kendall和回归趋势分析的结果显示,1976年至2015年间,降雨量呈统计学显著上升趋势(Z=2.74,P=0.005)。类似地,在同一时期,PET中观察到具有统计学意义的(Z=4.40,p=0.001)增加趋势。确定了六个月的水盈余(5月至10月)和六个月水赤字(11月至4月)。总的来说,在40年的时间里,发现了27年的缺水现象。水平衡模式显示,Idanre、Akure和Owo腹地的年平均盈余最高(324.51 mm),而不是沿海城市Ikeja,这可归因于腹地的地形效应。平均干旱指数(AI)为0.94的研究区域仍然可以被视为湿润环境,尽管AI的空间变异性表明北部地区正趋向于干旱-亚湿润条件(AI=0.76)。本研究建议在湿润月份保持水分盈余,以增加干旱月份的缺水;这不仅可以促进农业生产,还可以缓解研究地区的供水问题。关键词。干旱指数、潜在蒸散量、水分平衡。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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