Uploaded May 2021 | Updated September 2026, 1 hour ago
[Reupload]
"The tilting flume at the Institute of Hydraulic Engineering and Water Resources Management at RWTH Aachen University shows the differences between subcritical and supercritical flow. Therefore, a hydraulic jump is generated in open channel flow. A hydraulic jump is formed when the depth of flow changes from supercritical to subcritical state."
This is part of the Open Educational Resources Initiative by the Faculty of Civil Engineering of the RWTH Aachen University.
For further information visit: fb3.rwth-aachen.de
This video and intro are licensed under Creative Commons 4.0 International BY the Faculty of Civil Engineering RWTH Aachen University.
For further information visit: creativecommons.org
"Global OER Logo“ CC BY 3.0 Jonathas Mello .
Southern California by Riot
Creative Commons — Attribution 3.0 Unported— CC BY 3.0
creativecommons.org/licenses/by/3.0
Music provided by FreeMusic109 youtube.com/FreeMusic109
[Reupload]
"The tilting flume at the Institute of Hydraulic Engineering and Water Resources Management at RWTH Aachen University shows the differences between subcritical and supercritical flow. Therefore, a hydraulic jump is generated in open channel flow. A hydraulic jump is formed when the depth of flow changes from supercritical to subcritical state."
This is part of the Open Educational Resources Initiative by the Faculty of Civil Engineering of the RWTH Aachen University.
For further information visit: fb3.rwth-aachen.de
This video and intro are licensed under Creative Commons 4.0 International BY the Faculty of Civil Engineering RWTH Aachen University.
For further information visit: creativecommons.org
"Global OER Logo“ CC BY 3.0 Jonathas Mello .
Southern California by Riot
Creative Commons — Attribution 3.0 Unported— CC BY 3.0
creativecommons.org/licenses/by/3.0
Music provided by FreeMusic109 youtube.com/FreeMusic109
