water evaluation and planning
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2022 ◽  
pp. 1944-1964
Author(s):  
Abdelkrim Ben Salem ◽  
Souad Ben Salem ◽  
Mohammed Khebiza Yacoubi ◽  
Mohammed Messouli

Water ecosystem service is the most important element that supports Tafilalet agro-ecosystems. In this region, drought frequency is increasing, which complicate the management groundwater reserves. The ephemeral flows of the rivers force people to use groundwater to meet the population demand. Consequently, water resource management is of significant importance the sustainability of this area. Water evaluation and planning (WEAP) is useful management software used to evaluate and trace the trend of water demand. This model was applied in case of Ziz basin in order to simulate and analyze the situation of water under different scenarios. The results show an increasing of demand for water irrigation and with introducing modern irrigation scenario. However, a decreasing trend in reservoir storage volume and groundwater storage was projected in Tafilalet.


Author(s):  
Rindramampionona Fanambinantsoa Ankasitrahana Randriamifidison ◽  
Daniel Rakotoarisoa ◽  
Tsaralaza Jorlin Tsiavahananahary ◽  
Tantely Rakotovao ◽  
Lily Arson Rene de Rolland

Abstract. Les démarches de cette recherche ont été fondées au départ sur le fait que les ressources en eau diminuent avec le changement climatique, alors que les besoins de la population augmentent incéssament. Elle concerne la Commune urbaine d'Ambositra et la Commune rurale d'Ambositra, traversées par la rivière Isaha . Dans cette optique, cet article a pour objectif d'analyser le rapport entre les ressources et les besoins en eau pour diverses utilisateurs tenant compte des variabilités climatiques dans la zone. Pour ce faire, des variables d'entrée ont été utilisés pour modéliser de l'utilisation des ressources en eau par le biais du logiciel WEAP (Water Evaluation and Planning System), précédé par un traitement cartographique pour la délimitation de la zone par le logiciel QGIS. Les données sur la précipitation sont obtenues avec la médiane des valeurs issues des modèles climatiques du scenario RCP4.5. Les principaux résultats de cette étude concernent à la fois l'utilisation de l'eau à des fins agricoles et pour un usage urbain. Et les stratégies proposées concernent tous les acteurs de tous les niveaux, des utilisateurs à l'Etat central. Nous avons évoqué l'urgence de la concrétisation des recommandations émanant de cette étude vue les réalités actuelles ainsi que la prévision issue de la modélisation.


2021 ◽  
Vol 21 (1) ◽  
Author(s):  
Claudia Medina

El embalse Milluni Grande depende principalmente de la precipitación, siendo vulnerable ante periodos de sequía, de forma que puede afectar a la seguridad hídrica de las ciudades de La Paz y El Alto. Por lo tanto, el presente estudio busca determinar la variación de la cantidad de agua disponible en el embalse bajo el set de escenarios de cambio climático establecidos en el quinto informe del Panel Intergubernamental sobre el Cambio Climático (IPCC) para el periodo 2022-2090. El área de estudio se limitó a la microcuenca Milluni, tomando el embalse Milluni Grande como punto de desemboque. La modelación hidrológica se realizó mediante la herramienta Water Evaluation and Planning System (WEAP) utilizando el ensamble de datos diarios de precipitación y temperatura generado a través de la herramienta Gridded Meteorological Ensemble Tool (GMET). Se incorporaron los escenarios de cambio climático empleando el Modelo 1 del Sistema Terrestre de Noruega NorESM1-M, reduciendo su escala mediante el método no paramétrico de vecinos más cercanos (knn-bootstrap). Se obtuvieron las siguientes tendencias para el periodo y área de estudio: incremento general de temperatura, incremento de precipitación en época seca y reducción de precipitación en época húmeda, lo cual puede generar situaciones de sequía. Por otra parte, el caudal de entrada al embalse Milluni Grande tiene tendencia a variar de forma directamente proporcional a la precipitación, mientras que su volumen tiene tendencia a reducirse. Asimismo, puede existir un déficit en la cobertura de los requerimientos de los sitios de demanda, llegando a valores mínimos de 45% para el sistema de distribución Achachicala y 27% para el sistema Meseta. Todos los resultados son acentuados en el escenario pesimista RCP 8.5.


2021 ◽  
Vol 22 (1) ◽  
pp. 30-39
Author(s):  
Miroslav Kandera ◽  
Roman Výleta ◽  
Anna Liová ◽  
Zuzana Danáčová ◽  
ľubica Lovasová

Author(s):  
S. S. Pravin ◽  
C. Gajendran ◽  
T. Divya

Abstract Renewable groundwater and surface water supplies are insufficient for the existing urban population all over the world as water demand is increasing rapidly. Usage per capita in urban areas transcends 160 liters per day. Climate change is projected to increase water demand even more. Sources of surface water obtained by stormwater runoff can be well used to fulfill this requirement. The main objective of this work is to assess the water supply and demand in the dry condition in the Coimbatore region, Tamil Nadu, India, and to use the Water Evaluation and Planning method to create a model for supply and demand in the future. There are more than three dozen of surface water bodies in and around the metropolitan center. Most sources are heavily encroached upon. By linking stormwater runoff from its respective elevation to the accessible surface water bodies, an additional water supply source can be obtained. By using the Water Evaluation and Planning framework as a guide, models were developed to determine potential needs, compare demand and supply, water usage, lack of water use, and population coverage. The enhanced stormwater drainage system for Coimbatore city was also designed in such a way that the corporation's various roads were connected to the major water bodies. The domestic water demand in the future is predicted to be around 27 Million Cubic Feet(MCFT). Meanwhile, the possible amount of stormwater collection in the selected water bodies is predicted to be 50 Million Cubic Meter (MCM) to 320MCM. Thus, the study concluded that 100% of urban domestic water demand can be met if the urban stormwater is utilized by harvesting and storing in surface water bodies.


2021 ◽  
Vol 779 (1) ◽  
pp. 012104
Author(s):  
Isam M. Abdulhameed ◽  
Sadeq O. Sulaiman ◽  
Abu Baker A. Najm

2021 ◽  
Vol 11 (5) ◽  
Author(s):  
Sara Seddiki ◽  
El Amine Cherif

AbstractBechar city is located in arid climate of the Algerian Sahara, with an average annual rainfall of about 72 mm. There are two sources to ensure the water supply of the town of Bechar; the first comes from a watershed made up of eight non-renewable boreholes, and the second comes from the Djorf Torba dam, located about 45 km to the west. The pressure on water demand in the highland region depends on many factors, namely: demographic, social, climatic and economic. This study is based on the application of a water evaluation and planning computer tool on the city of Bechar. Which allows us to analyze the supply–demand balance in the water and assess the impact of different scenarios on the study area for manage the water resource and the projected water demand for the different sectors (drinking water, industrial water and agriculture) until 2060.


2021 ◽  
Vol 6 (1) ◽  
pp. 55
Author(s):  
Ariska Mia Christiwarda Sihombing ◽  
Indarto Indarto ◽  
Sri Wahyuningsih

Mayang Watersheds frequently hit by floods during the rainy season and drought during the dry season. This study aims to assess the water balance by calculating water resource availability and water demand in the Mayang watershed. The Water Evaluation and Planning (WEAP) model was used as the primary tool for the analysis. The supply of water comes only from precipitation. Demand was calculated based on the water demand for irrigation, domestic, urban, industrial, and livestock uses. The unit of time to calculate the water balance is ten days. It means that each month is divided into three-time steps. Analysis of the WEAP is based on the water demand from 2002 to 2019. The results showed that from 3rd December to 1st May, the Mayang river and its tributaries could supply all demand sites up to 100%. However, unmet demand occurs from 2nd May to 2nd December. The highest first unmet demand occurred in October, with 0.67 million m3. The management of water resources, especially in terms of distribution during the rainy season and dry season, must be considered. Keywords: Water balance; Water supply; Water demand; Mayang; Watershed; WEAP Copyright (c) 2021 Geosfera Indonesia and Department of Geography Education, University of Jember This work is licensed under a Creative Commons Attribution-Share A like 4.0 International License


2021 ◽  
Vol 2 (136) ◽  
pp. 469-496
Author(s):  
Amir Nima Mohammed Al- Zobaei ◽  
Kasim Ahmed Remal Al-Dulaimi

تناولت الدراسة الموارد المائية في ناحية اليوسفية وسبل ادارتها، والتي تعد من اهم النواحي الزراعية في محافظة بغداد ضمن قضاء المحمودية، تقع فلكياً بين دائرتي عرض (00= 3- 33 o– 00= 12- 33o) شمالاً، وبين خطي طول (00= 0- 44 o– 00= 18- 44 o) شرقاً، بمساحة تصل الى (425) كم2. لقد ركزت الدراسة على مشكلة في غاية الأهمية تواجهها الناحية الا وهي (سوء ادارة الموارد المائية) وما يرتبط بها من ظواهر الهدر والتلوث، والتي تعد من اهم المخاطر الداخلية التي تهدد الامن المائي للمواطن، حيث بينت الدراسة سبل إدارة المياه على المستوى المحلي. وتوصلت الدراسة الى وجود مشكلات بشرية اثرت في إدارة الموارد المائية في المنطقة، كان أهمها سوء إدارة المنظومة المائية والزيادة الكبيرة في اعداد السكان والتلوث وتجاوزات بحيرات الأسماك البالغ عددها (418) بحيرة وبمساحة مائية تقدر بحوالي (1524.5) دونم وباستهلاك مائي سنوي يبلغ حوالي (370960) م3/سنة، ومضخات المياه غير المرخصة التي يصل استهلاكها المائي السنوي الى (2226500) م3/سنة، واستخدام نظام الري التقليدي (السيحي) الذي يؤدي الى ضياع (50) % من المياه، كذلك الهدر والاسراف غير المبرر من قبل السكان. كما تم إدخال نظام تخطيط وتقييم المياه Water Evaluation And Planning system (WEAP) حيز التنفيذ كون هذا النظام اتى بثماره في الدول التي عملت به، اذ تم من خلاله تقدير كمية الاحتياجات المائية بهدف تغطيتها وتوفيرها لضمان التنمية المستدامة وإدارة المياه في المنطقة، فتبين من خلاله ان المنطقة بحاجة الى توفير حوالي (242.13) مليون م3/سنة من المياه في عام 2020، ليرتفع في عام 2025 الى حوالي (348.04) مليون م3/سنة، ثم الى (454.05) مليون م3/سنة في عام 2030.


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