more tsunami basics
DESCRIPTION
More Tsunami Basics. Phases of a Tsunami Event: Generation Propagation Shoaling Inundation. Shoaling. Wave steepens and breaks because of decreasing depth:. Forces on a structure: Hydrostatic (pressure) force Buoyant Force Hydrodynamic Force. Forces on a structure: - PowerPoint PPT PresentationTRANSCRIPT
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Catherine Petroff, University of Washington - July 22, 2007UW Educational Outreach – Tsunami Science & Preparedness Program (Su 07)
More Tsunami Basics
Sponsored by NOAA and USAID under the U.S. Indian Ocean Tsunami Warning System Program Page 2
Catherine Petroff, University of Washington - July 22, 2007UW Educational Outreach – Tsunami Science & Preparedness Program (Su 07)
Phases of a Tsunami Event:
•Generation
•Propagation
•Shoaling
•Inundation
Sponsored by NOAA and USAID under the U.S. Indian Ocean Tsunami Warning System Program Page 3
Catherine Petroff, University of Washington - July 22, 2007UW Educational Outreach – Tsunami Science & Preparedness Program (Su 07)
Shoaling
Wave steepens and breaks because of decreasing depth:
Sponsored by NOAA and USAID under the U.S. Indian Ocean Tsunami Warning System Program Page 4
Catherine Petroff, University of Washington - July 22, 2007UW Educational Outreach – Tsunami Science & Preparedness Program (Su 07)
Forces on a structure:
Hydrostatic (pressure) forceBuoyant ForceHydrodynamic Force
Sponsored by NOAA and USAID under the U.S. Indian Ocean Tsunami Warning System Program Page 5
Catherine Petroff, University of Washington - July 22, 2007UW Educational Outreach – Tsunami Science & Preparedness Program (Su 07)
Forces on a structure:
Hydrostatic (pressure) forceBuoyant ForceHydrodynamic ForceSurge ForceImpact ForceBreaking Wave Force
Sponsored by NOAA and USAID under the U.S. Indian Ocean Tsunami Warning System Program Page 6
Catherine Petroff, University of Washington - July 22, 2007UW Educational Outreach – Tsunami Science & Preparedness Program (Su 07)
Here is an example of a broken wave (or bore) hitting a square column in a laboratory:
Sponsored by NOAA and USAID under the U.S. Indian Ocean Tsunami Warning System Program Page 7
Catherine Petroff, University of Washington - July 22, 2007UW Educational Outreach – Tsunami Science & Preparedness Program (Su 07)
Sponsored by NOAA and USAID under the U.S. Indian Ocean Tsunami Warning System Program Page 8
Catherine Petroff, University of Washington - July 22, 2007UW Educational Outreach – Tsunami Science & Preparedness Program (Su 07)
Sponsored by NOAA and USAID under the U.S. Indian Ocean Tsunami Warning System Program Page 9
Catherine Petroff, University of Washington - July 22, 2007UW Educational Outreach – Tsunami Science & Preparedness Program (Su 07)
Hydrodynamic forces on a structure on a structure:Here is what the lateral force looks like on the square column during impact
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Catherine Petroff, University of Washington - July 22, 2007UW Educational Outreach – Tsunami Science & Preparedness Program (Su 07)
For the modelers in the audience, here is the same thing on a computer:
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Catherine Petroff, University of Washington - July 22, 2007UW Educational Outreach – Tsunami Science & Preparedness Program (Su 07)
Sponsored by NOAA and USAID under the U.S. Indian Ocean Tsunami Warning System Program Page 12
Catherine Petroff, University of Washington - July 22, 2007UW Educational Outreach – Tsunami Science & Preparedness Program (Su 07)
Let’s do a brief exercise:
Light wood construction
2x4 studs, light plaster both sides 19psf
Floor wood 4 psf
Roof wood 3 psf
5 meters square
1 psf = 48 Newtons/m2
Velocity?Asafa Powell 100
meters in 9.77s, 2006 Zurich
http://nctr.pmel.noaa.gov/education/science/docs/floatorfall.xls