TY - GEN A1 - Kühn, Michael A1 - Schöne, Tim T1 - Multivariate regression model from water level and production rate time series for the geothermal reservoir Waiwera (New Zealand) T2 - Energy procedia N2 - Water management tools are necessary to guarantee the preservation of natural resources while ensuring optimum utilization. Linear regression models are a simple and quick solution for creating prognostic capabilities. Multivariate models show higher precision than univariate models. In the case of Waiwera, implementation of individual production rates is more accurate than applying just the total production rate. A maximum of approximately 1,075 m3/day can be pumped to ensure a water level of at least 0.5 m a.s.l. in the monitoring well. The model should be renewed annually to implement new data and current water level trends to keep the quality. KW - geothermal reservoir KW - water management KW - data based model KW - multivariate regression KW - coefficient of determination KW - scenario analysis Y1 - 2017 U6 - https://doi.org/10.1016/j.egypro.2017.08.196 SN - 1876-6102 VL - 125 SP - 571 EP - 579 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - de Araujo, Jose Carlos A1 - Bronstert, Axel T1 - A method to assess hydrological drought in semi-arid environments and its application to the Jaguaribe River basin, Brazil JF - Water International N2 - This manuscript proposes a method to assess hydrological drought in semi-arid environments under high impoundment rate and applies it to the semi-arid Jaguaribe River basin in Brazil. It analyzes droughts (1) in the largest reservoir systems; (2) in the Upper Basin, considering 4744 reservoirs, 800 wells and almost 18,000 cisterns; and (3) in reservoirs of different sizes during multiyear droughts. Results show that the water demand is constrained in the basin; hydrological and meteorological droughts are often out of phase; there is a negative correlation between storage level and drought severity; and the small systems cannot cope with long-term droughts. KW - Reservoirs KW - Brazil KW - multiyear drought KW - water management KW - impoundment rate KW - water demand Y1 - 2016 U6 - https://doi.org/10.1080/02508060.2015.1113077 SN - 0250-8060 SN - 1941-1707 VL - 41 SP - 213 EP - 230 PB - Wiley-Blackwell CY - Abingdon ER - TY - JOUR A1 - Tekken, Vera A1 - Kropp, Jürgen T1 - Climate-Driven or Human-Induced indicating severe water scarcity in the Moulouya River Basin (Morocco) JF - Water N2 - Many agriculture-based economies are increasingly under stress from climate change and socio-economic pressures. The excessive exploitation of natural resources still represents the standard procedure to achieve socio-economic development. In the area of the Moulouya river basin, Morocco, natural water availability represents a key resource for all economic activities. Agriculture represents the most important sector, and frequently occurring water deficits are aggravated by climate change. On the basis of historical trends taken from CRU TS 2.1, this paper analyses the impact of climate change on the per capita water availability under inclusion of population trends. The Climatic Water Balance (CWB) shows a significant decrease for the winter period, causing adverse effects for the main agricultural season. Further, moisture losses due to increasing evapotranspiration rates indicate problems for the annual water budget and groundwater recharge. The per capita blue water availability falls below a minimum threshold of 500 m(3) per year, denoting a high regional vulnerability to increasing water scarcity assuming a no-response scenario. Regional development focusing on the water-intense sectors of agriculture and tourism appears to be at risk. Institutional capacities and policies need to address the problem, and the prompt implementation of innovative water production and efficiency measures is recommended. KW - North Africa KW - Moulouya river basin KW - climate change KW - population growth KW - regional development KW - water availability KW - water management KW - water scarcity Y1 - 2012 U6 - https://doi.org/10.3390/w4040959 SN - 2073-4441 VL - 4 IS - 4 SP - 959 EP - 982 PB - MDPI CY - Basel ER -