Calculating Discharge Carrying Capacity of River Tapi - IJERT Psychological Research & Experimental Design, All Teacher Certification Test Prep Courses, Drainage Basins: Definition & Characteristics, Effect of Erosion and Deposition on Landforms, Hillslope Erosion Process: Formation of Rills & Gullies, How a Landform Diagram Describes the Geological Progression of a Landscape, Base Level of a Stream: Definition & Effect on Erosion, Global Temperature Patterns & The Atmosphere, Atmospheric Moisture, Precipitation & Clouds, Origin and Migrations of Humans and Culture, The Impact of Geography on Language & Culture, The Global Distribution & Characteristics of Soil, Ethical and Political Processes of the Environment, Geography of the Caribbean & Central & South America, Geography of Australia & the Pacific Islands, Sociology for Teachers: Professional Development, Gerontology for Teachers: Professional Development, UExcel Introduction to Sociology: Study Guide & Test Prep, General Anthropology for Teachers: Professional Development, Counseling Fundamentals for Teachers: Professional Development, American Government Syllabus Resource & Lesson Plans, Foundations of Education Syllabus Resource & Lesson Plans, 10th Grade English Curriculum Resource & Lesson Plans, Intro to Political Science Syllabus Resource & Lesson Plans, Frankfurt School: Critical Theory & Philosophy, Conscientious Objector: Definition & Status, What is Libertarianism? What are the different methods to calculate discharge of a catchment 1. Most USGS streamgages transmit stage data by satellite to USGS computers where the stage data are used to estimate streamflow using the developed stage-discharge relation (rating). The direct proportionality of stream or river discharge with velocity (V), width (W), and depth (D) indicates the discharge shall increase if all these parameters increase. Calculate the amount of water used for activities. Using a channel width of 10 feet and an average depth of 0.8 feet and the discharge calculation becomes 10 ft x 0.8 ft x 0.9 ft/sec = 7.2 cubic ft/sec (cfs). Splitting a large river into smaller streams often leads to a decreased river or stream discharge. EnergyTransformation is nothing but simply converting onetype of energyinto another form. However, the suspended sounding weights in deeper waters and a wading rod in shallower streams can be respectively used to measure the depth of water. The calculation of the stream discharge is important as it provides an idea about the quality of water and the stream habitats.

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