Titlebook: Climate Change and Water Resources in Mediterranean Countries; Climate Change and W Hüseyin G?k?eku?,Youssef Kassem Conference proceedings

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書目名稱Climate Change and Water Resources in Mediterranean Countries影響因子(影響力)




書目名稱Climate Change and Water Resources in Mediterranean Countries影響因子(影響力)學(xué)科排名




書目名稱Climate Change and Water Resources in Mediterranean Countries網(wǎng)絡(luò)公開(kāi)度




書目名稱Climate Change and Water Resources in Mediterranean Countries網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書目名稱Climate Change and Water Resources in Mediterranean Countries被引頻次




書目名稱Climate Change and Water Resources in Mediterranean Countries被引頻次學(xué)科排名




書目名稱Climate Change and Water Resources in Mediterranean Countries年度引用




書目名稱Climate Change and Water Resources in Mediterranean Countries年度引用學(xué)科排名




書目名稱Climate Change and Water Resources in Mediterranean Countries讀者反饋




書目名稱Climate Change and Water Resources in Mediterranean Countries讀者反饋學(xué)科排名

紀(jì)念

Validation of PML-V2 Evapotranspiration Model Over Multi-climatic Regions of Iranels, observations, and global products, for validation purposes. The assessment encompassed three different climate types: hot humid, hot semi-arid, and cold semi-arid, representing the north, west, and northwest regions of Iran, respectively. The results demonstrated that the PML-V2 model exhibited

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Innovative Solutions on Water Management for Islands Under Climate Change innovative nature-based solutions to sustainably manage islands‘ existing water resources under the influence of climate change. Understanding the unique status of the islands and the complex relationship between water resources and climate change is of great importance for the creation and develop

出價(jià)

Evaluation of the Flooding and Drought Analysis Results by Determining the Hydrological Characterists during agricultural activities. In this study, the drainage areas were determined as 547 km.. With the help of precipitation data, the possible flood discharge of Eflani River Basin according to different year return periods was calculated according to DSI Synthetic and Mockus methods and was dete

大看臺(tái)

Modelling Hydrological Drought Characteristics by Copulasate return periods in 10, 20, 50, 100, 200, 500 years, and bivariate return periods considering the T. (and) and T′. (or) cases; Gaussian, Student’s t, Clayton, Gumbel, Frank, Joe, BB1, BB6, BB7 and BB8 copulas are utilized. The best copulas have been analyzed by tail dependence and by goodness of f

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Meteorological Drought Analysis in K?z?l?rmak Basin, Türkiye1, 3, 12 and 24 months. In this study, the occurence of wet . and on the other hand Mild Drought (MD), Moderate Drought (MOD), Severe drought (SD) and extreme drought (ED) have been investigated. Findings have demonstrated that for all stations and in all time scale, Wet and MD have the highest perc

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Daily Rainfall Characteristics in Sudan: Statistical Analysis and Modelingc differentiation, which causes many difficulties in its accurate simulation and prediction. Therefore, Multi-Layer Perceptron Neural Networks (MLPNN) and Multiple Linear Regression (MLR) are used for predicting the annual rainfall in Sudan. To this aim, the minimum temperature (Tmin), maximum tempe

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