Measurement of river discharge / खोलाको गति

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by definition River discharge' is the volume of water flowing through a river channel; measured at any given point in cubic metres per second.
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River hydrology is the study of the dynamic volumes of water within fluvial channels. Each river has a unique hydrologic signature-an outcome of the complex interactions between climate and the surrounding landscape, the geology and geomorphology, and the longitudinal, lateral, and vertical connections between the aquatic and terrestrial interface. Hydrology shapes channel and floodplain morphologies and organizes the physiochemical characteristics of lotic habitats in which riverine organisms are adapted. As such, hydrology is considered the master variable of river ecosystem organization; however, the interactions between discharge and other abiotic properties that shape riverine ecological communities are complex and poses challenges for river managers. To cope with such complexity, many hydrologic statistics were developed to summarize river discharge into meaningful metrics for setting water policy standards and understanding fundamental linkages between hydrology and ecology. Although the field of statistical hydrology was aimed at reducing complexity, hundreds of hydrologic statics are now available to summarize discharge, and this has created its own paradox for researchers and river managers. Further research continues to identify the most important statistics to consolidate complexity and understand hydrologic variation. Although each river is hydrologically unique, river systems display recurrent patterns in hydrology-these stem from shared similarities in climate regimes and landscape attributes. These repeated hydrologic regimes have predisposed rivers to hydrologic classification, where rivers are grouped based on similarities in hydrologic behavior. Hydrologic classifications have not only provided insights into the distinct properties of streamflow regimes, but also providing an organizational unit to manage groups of rivers. The use of hydrologic classifications has increased in recent years for both fundamental explorations of hydrologic diversity as well as applied uses for environmental flows.
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