River Discharge

dc.creatorUlrich Looser;Climate, Energy and Tenure Division
dc.date2023-04-27T11:40:37Z
dc.date2023-04-27T11:40:37Z
dc.date2009
dc.date2019-05-30T13:54:36.0000000Z
dc.date.accessioned2026-06-27T21:22:16Z
dc.descriptionRiver discharge has a role in driving the climate system, as the freshwater inflow to the world’s oceans may influence oceanic circulation patterns at interannual to decadal time scales. At the same time river discharge serves as an indicator for climatic change and variability as it reflect’s changes in precipitation and evapotranspiration. River discharge, which is expressed as volume per unit time, is the rate at which water flows through a cross-section. The unit used to me asure river discharge is usually m3/s (cubic meters per second, or cumecs). Currently in situ methods are the most costeffective and reliable options for river discharge measurement. Discharge measurements are made at each gauging station to determine the discharge rating for the site. The discharge rating is a relation between stage and discharge influenced by stage, slope, rate of change of stage and other factors. The depth of flow in the cross-section is measured at verti cals using different techniques. As the depth is measured, observations of velocity are obtained at one or more points in the vertical. The measured widths, depths, and velocities permit computation of discharge for each segment of the cross-section. The summation of these segment discharges is the total discharge.
dc.format24
dc.formatapplication/pdf
dc.identifierhttp://www.fao.org/documents/card/en/c/78d4ba09-bd77-54ea-8254-eff22d18af08
dc.identifierhttps://fao-prod.atmire.com/handle/20.500.14283/I1279E
dc.identifierhttp://www.fao.org/3/a-i1279e.pdf
dc.identifier.urihttp://hdl.handle.net/123456789/221178
dc.languageEnglish
dc.rightsFAO
dc.titleRiver Discharge
dc.titleRiver Discharge
dc.titleAssessment of the status of the development of the standards for the Terrestrial Essential Climate Variables
dc.typeBook (stand-alone)

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