{"title":"土地利用、水需求和气候变化对多瑙河流域水资源短缺的未来预测","authors":"B. Bisselink, A. De Roo, J. Bernhard, E. Gelati","doi":"10.2478/jengeo-2018-0010","DOIUrl":null,"url":null,"abstract":"Abstract This paper presents a state-of-the-art integrated model assessment to estimate the impacts of the 2°C global mean temperature increase and the 2061-2090 warming period on water scarcity in the Danube River Basin under the RCP8.5 scenario. The Water Exploitation Index Plus (WEI+) is used to calculate changes in both spatial extent and people exposed to water scarcity due to land use, water demand, population and climate change. Despite model and data uncertainties, the combined effects of projected land use, water demand and climate change show a decrease in the number of people exposed to water scarcity during the 2°C warming period and an increase in the 2061-2090 period in the Danube River Basin. However, the projected population change results in a decrease of exposed people in both warming periods. Regions with population growth, in the northwestern part of the Danube River Basin experience low water scarcity or a decrease in water scarcity. The largest number of people vulnerable to water scarcity within the Danube River Basin are living in the Great Morava, Bulgarian Danube and Romanian Danube. There, the combined effects of land use, water demand and climate change exacerbate already existing water scarce areas during the 2°C warming period and towards the end of the century new water scarce areas are created. Although less critical during the 2°C warming period, adjacent regions such as the Tisza, Middle Danube and Siret-Prut are susceptible to experience similar exposure to water scarcity within the 2061-2090 period. Climate change is the most important driver for the increase in water scarcity in these regions, but the strengthening effect of water demand (energy sector) and dampening effect of land use change (urbanization) does play a role as well. Therefore, while preparing for times of increased pressures on the water supply it would be advisable for several economic sectors to explore and implement water efficiency measures.","PeriodicalId":115431,"journal":{"name":"Journal of Environmental Geography","volume":"44 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2018-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"12","resultStr":"{\"title\":\"Future Projections of Water Scarcity in the Danube River Basin Due to Land Use, Water Demand and Climate Change\",\"authors\":\"B. Bisselink, A. De Roo, J. Bernhard, E. Gelati\",\"doi\":\"10.2478/jengeo-2018-0010\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Abstract This paper presents a state-of-the-art integrated model assessment to estimate the impacts of the 2°C global mean temperature increase and the 2061-2090 warming period on water scarcity in the Danube River Basin under the RCP8.5 scenario. The Water Exploitation Index Plus (WEI+) is used to calculate changes in both spatial extent and people exposed to water scarcity due to land use, water demand, population and climate change. Despite model and data uncertainties, the combined effects of projected land use, water demand and climate change show a decrease in the number of people exposed to water scarcity during the 2°C warming period and an increase in the 2061-2090 period in the Danube River Basin. However, the projected population change results in a decrease of exposed people in both warming periods. Regions with population growth, in the northwestern part of the Danube River Basin experience low water scarcity or a decrease in water scarcity. The largest number of people vulnerable to water scarcity within the Danube River Basin are living in the Great Morava, Bulgarian Danube and Romanian Danube. There, the combined effects of land use, water demand and climate change exacerbate already existing water scarce areas during the 2°C warming period and towards the end of the century new water scarce areas are created. Although less critical during the 2°C warming period, adjacent regions such as the Tisza, Middle Danube and Siret-Prut are susceptible to experience similar exposure to water scarcity within the 2061-2090 period. Climate change is the most important driver for the increase in water scarcity in these regions, but the strengthening effect of water demand (energy sector) and dampening effect of land use change (urbanization) does play a role as well. 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引用次数: 12
摘要
基于RCP8.5情景下全球平均气温上升2°C和2061-2090年增温期对多瑙河流域水资源短缺的影响,建立了当前最先进的综合模型。水资源利用指数(Water Exploitation Index Plus, WEI+)用于计算由于土地利用、水需求、人口和气候变化而导致的水资源短缺的空间程度和暴露人数的变化。尽管模式和数据存在不确定性,但预估的土地利用、水需求和气候变化的综合影响表明,在2°C变暖期间,多瑙河流域面临缺水的人数将减少,而在2061-2090年期间将增加。然而,预测的人口变化导致两个变暖期暴露的人数减少。在人口增长的地区,多瑙河流域西北部缺水程度较低或缺水程度有所下降。多瑙河流域易受缺水影响的人口最多的是生活在大摩拉瓦河、保加利亚多瑙河和罗马尼亚多瑙河的人。在那里,土地利用、水需求和气候变化的综合影响在2°C变暖期间加剧了已经存在的缺水地区,到本世纪末将产生新的缺水地区。虽然在2°C变暖期间不那么严重,但邻近地区,如Tisza,多瑙河中部和Siret-Prut,在2061-2090年期间也容易遭受类似的水资源短缺。气候变化是这些地区水资源短缺加剧的最重要驱动因素,但水需求的强化效应(能源部门)和土地利用变化的抑制效应(城市化)也发挥了作用。因此,在为供水压力增加的时期做准备的同时,几个经济部门探索和实施节水措施是可取的。
Future Projections of Water Scarcity in the Danube River Basin Due to Land Use, Water Demand and Climate Change
Abstract This paper presents a state-of-the-art integrated model assessment to estimate the impacts of the 2°C global mean temperature increase and the 2061-2090 warming period on water scarcity in the Danube River Basin under the RCP8.5 scenario. The Water Exploitation Index Plus (WEI+) is used to calculate changes in both spatial extent and people exposed to water scarcity due to land use, water demand, population and climate change. Despite model and data uncertainties, the combined effects of projected land use, water demand and climate change show a decrease in the number of people exposed to water scarcity during the 2°C warming period and an increase in the 2061-2090 period in the Danube River Basin. However, the projected population change results in a decrease of exposed people in both warming periods. Regions with population growth, in the northwestern part of the Danube River Basin experience low water scarcity or a decrease in water scarcity. The largest number of people vulnerable to water scarcity within the Danube River Basin are living in the Great Morava, Bulgarian Danube and Romanian Danube. There, the combined effects of land use, water demand and climate change exacerbate already existing water scarce areas during the 2°C warming period and towards the end of the century new water scarce areas are created. Although less critical during the 2°C warming period, adjacent regions such as the Tisza, Middle Danube and Siret-Prut are susceptible to experience similar exposure to water scarcity within the 2061-2090 period. Climate change is the most important driver for the increase in water scarcity in these regions, but the strengthening effect of water demand (energy sector) and dampening effect of land use change (urbanization) does play a role as well. Therefore, while preparing for times of increased pressures on the water supply it would be advisable for several economic sectors to explore and implement water efficiency measures.