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NEES Project Warehouse

Developing and Testing Algorithms for Generating Leading Tsunami Waves
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To compare experiments, please select at most four experiments from the experiment list below.

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  Experiment-1: Phase 1: Calibration
Dates: December 07, 2009 - January 04, 2010
Description:
Facility: Oregon State University, OR, United States


  Experiment-2: Phase 1: Water depth 75cm
Dates: January 19, 2010 - January 20, 2010
Description: Water depth is set at 75 cm. Solitary waves with different nonlinearity and bores are generated.
Facility: Oregon State University, OR, United States


  Experiment-3: Phase 1: Water depth 50cm
Dates: January 21, 2010 - January 21, 2010
Description: Water depth is set at 50 cm, where the transition of the beach slope occurs (1/15 to 1/30). Solitary waves with different nonlinearity and bores are generated.
Facility: Oregon State University, OR, United States


  Experiment-4: Phase 1: Water depth 25cm
Dates: January 22, 2010 - January 22, 2010
Description: Water depth is set at 25 cm with 1/15 beach slope. Solitary waves with different nonlinearity and bores are generated.
Facility: Oregon State University, OR, United States


  Experiment-5: Phase 2: Hh02
Dates: October 11, 2010 - October 13, 2010
Description: This research will use the Large Wave Flume wave maker to test the hypothesis that the leading tsunami wave does not have sufficient time and distance to evolve into a solitary form, therefore challenging the currently used modeling approach for wave...
Facility: Oregon State University, OR, United States


  Experiment-7: Phase 2: Hh015
Dates: October 13, 2010 - October 13, 2010
Description: This research will use the newly installed wave makers with long strokes at the NEES tsunami facility at Oregon State University to test the hypothesis that the leading tsunami wave does not have sufficient time and distance to evolve into a solitary...
Facility: Oregon State University, OR, United States


  Experiment-8: Phase 2: Hh01
Dates: October 13, 2010 - October 14, 2010
Description: This research will use the newly installed wave makers with long strokes at the NEES tsunami facility at Oregon State University to test the hypothesis that the leading tsunami wave does not have sufficient time and distance to evolve into a solitary...
Facility: Oregon State University, OR, United States


  Experiment-9: Phase 2: Hh01374
Dates: October 14, 2010 - October 14, 2010
Description: This research will use the newly installed wave makers with long strokes at the NEES tsunami facility at Oregon State University to test the hypothesis that the leading tsunami wave does not have sufficient time and distance to evolve into a solitary...
Facility: Oregon State University, OR, United States


  Experiment-11: Phase 2: Bore
Dates: October 15, 2010 - October 15, 2010
Description: Bores are generated by moving the wave maker paddle at a constant speed until the paddle reaches the maximum stroke length. Three trials with different speeds are tested with one repeated to check the repeatability. To designate the different cases,...
Facility: Oregon State University, OR, United States


  Experiment-12: Phase 2: LDN
Dates: October 15, 2010 - October 15, 2010
Description: Leading-depression N wave. Paddle trajectories are calculated by solving KdV equation in backward time. Three trials with different H/h ratio, and one more trial to check the repeatability have been carried out.
Facility: Oregon State University, OR, United States


  Experiment-13: Phase 2: Triple
Dates: October 15, 2010 - October 15, 2010
Description: Three solitary waves of equal wave heights (H/h = 0.1) are generated. Three trials with different separation time are carried out.
Facility: Oregon State University, OR, United States
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