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首页> 外文期刊>Journal of Hydrology >Impact of possible climate and land use changes in the semi arid regions: A case study from North Eastern Brazil
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Impact of possible climate and land use changes in the semi arid regions: A case study from North Eastern Brazil

机译:半干旱地区可能的气候和土地利用变化的影响:以巴西东北部为例

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This paper combines hydrological observations and modelling results of a semi arid catchment in Brazil that could lead to a better understanding of the hydrology of similar catchments in semi-arid regions. The Tapacurá catchment (area 470.5 km~2) in the Northeast of Brazil was selected for this study. The Distributed Catchment Scale Model, DiCaSM, was calibrated and validated for the stream flows of the Tapacurá catchment. The model performance was further tested by comparing simulated and observed scaled soil moisture. The results showed the ability of the model to simulate the stream flow and the scaled soil moisture. The simulated impacts of climate change of low emission (B1) scenarios, on the worst perspective, indicated the possibility of reduction in surface water availability by ?13.90%, ?22.63% and ?32.91% in groundwater recharge and by ?4.98%, ?14.28% and ?20.58% in surface flows for the time spans 2010-2039, 2040-2069, 2070-2099, respectively. This would cause severe impacts on water supply in the region. Changing the land use, for example by reforestation of part of the catchment area which is currently arable land, would lead to a decrease in both groundwater recharge by ?4.2% and stream flow by ?2.7%. Changing land use from vegetables to sugar cane would result in decreasing groundwater recharge by almost ?11%, and increasing stream flow by almost 5%. The combination of possible impacts of climate change and land use requires a proper plan for water resources management and mitigation strategies.
机译:本文结合了巴西半干旱流域的水文观测和模拟结果,可以使人们更好地了解半干旱地区类似流域的水文学。本研究选择了巴西东北部的Tapacurá流域(面积470.5 km〜2)。针对Tapacurá流域的水流,对分布式流域规模模型DiCaSM进行了校准和验证。通过比较模拟和观察到的结垢土壤湿度,进一步测试了模型性能。结果表明该模型能够模拟水流和结垢的土壤水分。从最坏的角度看,低排放(B1)情景对气候变化的模拟影响表明,地下水补给可能使地表水可利用性减少13.90%,22.63%和32.91%,并减少4.988%,在2010-2039年,2040-2069年,2070-2099年的时间里,地表流量分别为14.28%和?20.58%。这将对该地区的供水造成严重影响。改变土地用途,例如通过对部分集水区(目前是耕地)进行重新造林,将导致地下水补给量减少4.2%,溪流减少2.7%。将土地用途从蔬菜改为甘蔗,将导致地下水补给减少近11%,溪流增加近5%。气候变化和土地利用可能产生的影响相结合,需要制定适当的水资源管理和缓解战略计划。

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