气候变化对卢旺达水资源的影响:以Muvumba流域为例

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Averaging 21.6°C to 22.5°C, increased evaporation heightened water body depletion, impacting Muvumba catchment's water availability, exacerbating drought and scarcity. Projections for 2021-2040 anticipate March at 15.01°C as the coldest month, while July hits 28.7°C. Mean temperature may range from 21°C to 23.3°C, with a projected 0.82°C increase. Notably, annual precipitation peaked in 2020 at 1176.31 mm and hit a low in 2017 with 628.77 mm, emphasizing the water stress issue. It was found that the impacted location was the Mulindi sub-catchment, which is susceptible to floods and soil erosion, with the silt end up as sediments in rivers and streams. Research indicated the prediction of 1033.68mm annual rainfall in 2012-2040. Over 20 years it is predicted the reduction of 18.76 mm of precipitation, the highest annual evaporation rate was 2013, indicated 3.83mm which led to more water lost from water bodies. From2012 to 2021 water quality level was varied between 7.6 pH and 7.35 pH which facilitated the release of toxic substances from sediments into water further impacting water quality. Future water demand and use scenarios show that water stress in Muvumba will gradually increase, river discharges reduced by 2019 and 2020 due to decreased precipitation, LULCCD showed reduction of 17% of forests which lead to high rises of temperature .The average monthly discharge is projected to decrease from June to August (Long dry season) by variation of 4.7 and 7.8%by 2021-2040. Large increase of stream flow is projected to occur in April and May by variation of 13 and 14.7%. The research recommended the upgrading and maintaining existing stations and calibrating meteorological instruments, including weather radar, to give all climate information required for future observing, climate trend detection, climate variability management, afforestation, early warning, and disaster management. 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引用次数: 0

摘要

气候变化深刻地影响着水资源,由于天气模式的改变,影响着人们的福祉、农业、工业和城市发展。这项研究的重点是卢旺达的Muvumba流域,旨在评估气候变化的影响。通过分析全球(World Clim, GCMs, CMIP6)和国家数据集,遥感(SRTM高程数据,DEM)对2012-2021年和预计2021-2040年期间的降水、蒸发和温度变化有了深入的了解。利用地理信息系统、HEC-HMS模型和遥感,水文模型评估了Muvumba流域的河流流量,为有效实施缓解和适应战略提供了信息。分析表明,2012-2021年最低气温(14°C至17°C)和最高年气温(27°C至28.3°C)波动,十年来最高气温上升了0.4°C。平均温度为21.6°C至22.5°C,蒸发增加加剧了水体枯竭,影响了Muvumba流域的水供应,加剧了干旱和短缺。对2021-2040年的预测显示,最冷的月份是3月份的15.01°C,而7月份将达到28.7°C。平均气温可能在21°C至23.3°C之间,预计将增加0.82°C。值得注意的是,年降水量在2020年达到峰值1176.31 mm,在2017年达到低点628.77 mm,凸显了水分胁迫问题。研究发现,受影响的位置为Mulindi小流域,易受洪水和水土流失的影响,泥沙最终成为河流和溪流的沉积物。研究预测2012-2040年年降水量为1033.68mm。预测20 a降水减少18.76 mm,蒸发率最高的是2013年,为3.83mm,导致水体水分流失较多。从2012年到2021年,水质水平在7.6 - 7.35 pH之间变化,促使沉积物中的有毒物质释放到水中,进一步影响水质。未来水资源需求和利用情景表明,Muvumba的水资源压力将逐渐增加,由于降水减少,河流流量在2019年和2020年将减少,LULCCD显示森林减少17%,导致温度升高,预计到2021-2040年,6 - 8月(长旱季)平均月流量将减少4.7%和7.8%。预计4月和5月河流流量将大幅增加,增幅分别为13.7%和14.7%。研究建议升级和维持现有台站,并校正气象仪器,包括气象雷达,以提供未来观测、气候趋势探测、气候变率管理、植树造林、早期预警和灾害管理所需的所有气候信息。关键词:气候变化,水文模拟,温度,降水,蒸发和水资源,卢旺达
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Impact of Climate Change on Water Resources in Rwanda: A Case of Muvumba Catchment
Climate change profoundly impacts water resources, affecting people's well-being, agriculture, industry, and urban development due to altered weather patterns. This study focuses on Rwanda's Muvumba catchment, aiming to assess climate change effects. Analyzing global (World Clim, GCMs, CMIP6) and national data sets, remote sensing (SRTM elevation data, DEM) generated insights on precipitation, evaporation, and temperature changes during 2012-2021 and projected 2021-2040. Employing GIS, HEC-HMS model, and remote sensing, a hydrological model evaluates Muvumba catchment's river discharge, informing effective implementation of mitigation and adaptation strategies. Analysis indicated fluctuating minimum temperatures (14°C to 17°C) and maximum annual temperatures (27°C to 28.3°C) in 2012-2021, with a 0.4°C rise in maximum temperature over the decade. Averaging 21.6°C to 22.5°C, increased evaporation heightened water body depletion, impacting Muvumba catchment's water availability, exacerbating drought and scarcity. Projections for 2021-2040 anticipate March at 15.01°C as the coldest month, while July hits 28.7°C. Mean temperature may range from 21°C to 23.3°C, with a projected 0.82°C increase. Notably, annual precipitation peaked in 2020 at 1176.31 mm and hit a low in 2017 with 628.77 mm, emphasizing the water stress issue. It was found that the impacted location was the Mulindi sub-catchment, which is susceptible to floods and soil erosion, with the silt end up as sediments in rivers and streams. Research indicated the prediction of 1033.68mm annual rainfall in 2012-2040. Over 20 years it is predicted the reduction of 18.76 mm of precipitation, the highest annual evaporation rate was 2013, indicated 3.83mm which led to more water lost from water bodies. From2012 to 2021 water quality level was varied between 7.6 pH and 7.35 pH which facilitated the release of toxic substances from sediments into water further impacting water quality. Future water demand and use scenarios show that water stress in Muvumba will gradually increase, river discharges reduced by 2019 and 2020 due to decreased precipitation, LULCCD showed reduction of 17% of forests which lead to high rises of temperature .The average monthly discharge is projected to decrease from June to August (Long dry season) by variation of 4.7 and 7.8%by 2021-2040. Large increase of stream flow is projected to occur in April and May by variation of 13 and 14.7%. The research recommended the upgrading and maintaining existing stations and calibrating meteorological instruments, including weather radar, to give all climate information required for future observing, climate trend detection, climate variability management, afforestation, early warning, and disaster management. Keyword: Climate change, Hydrological Modeling, Temperature, Precipitation, Evaporation and Water resources, Rwanda
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