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Stage (hydrology)





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Inhydrology, stage is the water level in a riverorstream with respect to a chosen reference height. Stage is important because direct measurements of river discharge are very difficult while water surface elevation measurements are comparatively easy. In order to convert stage into discharge, a rating curve is needed. Hydrologists can use a combination of tracer studies, observations of high water marks, numerical modeling, and/or satelliteoraerial photography.

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  • Retrieved from "https://en.wikipedia.org/w/index.php?title=Stage_(hydrology)&oldid=1217269868"
     



    Last edited on 4 April 2024, at 20:40  





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    This page was last edited on 4 April 2024, at 20:40 (UTC).

    Content is available under CC BY-SA 4.0 unless otherwise noted.



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