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Changing hydroclimatic and discharge patterns in the northern Limpopo Basin, Zimbabwe

机译:津巴布韦北部林波波盆地的水文气候和排放方式变化

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摘要

Changing regional and global trends in climate and discharge, such as global warming-related declines in annual rainfall in south-eastern Africa, are likely to have a strong influence on water resource availability, and to increase livelihood risk. It is therefore important to characterise such trends. Information can be obtained by examining and comparing the rainfall and runoff records at different locations within a basin. In this study, trends in various parameters of temperature (4 stations), rainfall (10 stations) and discharge (16 stations) from the northern part of the Limpopo Basin, Zimbabwe, were statistically analysed, using the Spearman rank test, the Mann-Kendall test and the Pettitt test. It was determined that rainfall and discharge in the study area have undergone a notable decline since 1980, both in terms of total annual water resources (declines in annual rainfall, annual unit runoff) and in terms of the temporal availability of water (declines in number of rainy days, increases in dry spells, increases in days without flow). Annual rainfall is negatively correlated to an index of the El Nino - Southern Oscillation phenomenon. The main areas of rising risk are an increasing number of dry spells, which is likely to decrease crop yields, and an increasing probability of annual discharge below the long-term average, which could limit blue-water availability. As rainfall continues to decline, it is likely that a multiplier effect will be felt on discharge. Increasing food shortages are a likely consequence of the impact of this declining water resource availability on rain-fed and irrigated agriculture. Declining water resource availability will also further stress urban water supplies, notably those of Zimbabwe's second-largest city of Bulawayo, which depends to a large extent from these water resources and already experiences chronic water shortages.%WaterNet, PO Box MP600, Mount Pleasant, Harare, Zimbabwe,ICRISAT Bulawayo, Matopos Research Station, PO Box 776 Bulawayo, Zimbabwe;UNESCO-IHE, Westvest 7, PO Box 3015, 2601 DA Delft, The Netherlands,Department of Water Resources, Delft University of Technology, PO Box 5048, 2600 GA Delft, The Netherlands;ICRISAT Bulawayo, Matopos Research Station, PO Box 776 Bulawayo, Zimbabwe;UNESCO-IHE, Westvest 7, PO Box 3015, 2601 DA Delft, The Netherlands,Department of Water Resources, Delft University of Technology, PO Box 5048, 2600 GA Delft, The Netherlands;
机译:气候和流量变化的区域和全球趋势,例如与全球变暖相关的东南非洲年度降雨量下降,可能对水资源的可获得性产生重大影响,并增加生计风险。因此,表征这种趋势很重要。通过检查和比较流域内不同位置的降雨和径流记录可以获得信息。在这项研究中,我们使用Spearman等级检验,Mann-方法对津巴布韦林波波盆地北部的温度(4个站),降雨量(10个站)和流量(16个站)的各种参数的趋势进行了统计分析。 Kendall测试和Pettitt测试。自1980年以来,无论是从年度水资源总量(年度降雨量的下降,年度单位径流量的下降)还是从水资源的可利用时间(数量下降)的角度来看,研究区域的降雨和流量均已出现明显下降。雨天,干旱季节增加,无流量的日子增加)。年降雨量与厄尔尼诺现象-南方涛动现象的指数负相关。风险上升的主要方面是干旱时期的增加,这很可能会降低农作物的产量,而年排放量低于长期平均水平的可能性也在增加,这可能会限制蓝水的供应。随着降雨的持续减少,排放可能会产生乘数效应。水资源短缺对雨养和灌溉农业的影响可能导致粮食短缺加剧。水资源可用性的下降也将进一步给城市供水带来压力,特别是津巴布韦第二大城市布拉瓦约的城市供水,这在很大程度上取决于这些水资源,并且已经经历了长期的水资源短缺。%WaterNet,PO Box MP600,Mount Pleasant,津巴布韦哈拉雷,ICRISAT Bulawayo,马托波斯研究站,PO Box 776 Bulawayo,Zimbabwe; UNESCO-IHE,Westvest 7,PO Box 3015,2601 DA Delft,荷兰,德尔福特理工大学水资源系,PO Box 5048, 2600 GA Delft,荷兰; ICRISAT Bulawayo,Matopos Research Station,PO Box 776 Bulawayo,Zimbabwe; UNESCO-IHE,Westvest 7,PO Box 3015,2601 DA Delft,荷兰,德尔福特工业大学水资源系邮箱5048,2600 GA Delft,荷兰;

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