Titlebook: Hydrology in a Changing World; Challenges in Modeli Shailesh Kumar Singh,C.T. Dhanya Book 2019 Springer Nature Switzerland AG 2019 Challeng

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Urban Hydrology in a Changing World,land-cover will increase the demand for water resources in these areas. Climate change is also expected to increase the risk of drought in many countries, which will further exacerbate this demand. Before the combined impacts of urbanisation and climate change become evident, the need for accurate i

Friction

Uncertainty in Calibration of Variable Infiltration Capacity Model,gement in order to back the decision makers and hydrologists. It has been recognized that the current and future water challenges vary from the impacts of economic and population growth, floods, droughts or the melting of the glaciers. Hence, there is the need of the hour to adopt efficient hydrolog

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fixed-joint

,Land–Atmosphere Interactions in Indian Monsoon at Sub-seasonal to Seasonal Scale,ife in the Indian subcontinent. The summer monsoon in Indian subcontinent exhibits a wide range of temporal variability that is often viewed as a manifestation of disturbances originated as a result of coupled ocean–land–atmosphere interactions. Although the large-scale processes through the Sea Sur

ostrish

Assessment of Climate Change Impacts on IDF Curves in Qatar Using Ensemble Climate Modeling Approac climate change on IDF relationship in Qatar. The relationship between current (2010–2039), intermediate future (2040–2069) and the far future (2070–2100) IDF curves is examined. An unbiased selection of suitable Coupled Model Inter-comparison Project?Phase 5 (CMIP5) model scenarios provides the bas

圓桶

River Water Temperature Modelling Under Climate Change Using Support Vector Regression,eveloped to study the stream temperatures based on the heat advection, transportation and equilibrium temperature concepts, which necessitates basic river hydro-meteorology, geometry, effluents and other vegetative data. In contrast, several data-driven models were developed, which are based on the

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