PRINCIPLES & FORM
A TUSNAMI WAVE
• The measlant barrier is swung into place when water surges are expected. it has a unique bowed shape which isv incorporated into the final design.
• Tsunami waves occur as a result of seismic activity along subduction zones. The wave extends the full depth of the ocean acting like a typical shallow-water wave. A wave
tens of meters high is produced as the wave interacts with the continental shelf. it is compressed, slows down and builds height.
Steep Slope Less Run-Up
Shallow Slope Long Run-Up
Shoreline
Continental Shelf 150 feet
NATURAL PRINCIPLES-FLOW & DRAG
• Mangroves provide natural tsunami defense. The leaves, branches, trunk and roots all cause DRAG in the water making the wave slow and die down.
POPULATION & NATURAL OCCURRENCES • We looked at the history of where tsunamis tend to happen. The places that have repeatedly been affected are often heavily populated, and have a high projected population growth over the next fifty years. We chose Japan (more specifically Sendai) as our site due to their tsunami history and recent events.
protected area
LIMITED FUNCTIONABILITY:SUPER LEEVES • The super levees in Japan are effective but only to an extent. They can only be placed in certain areas and cannot be built high enough to be 100% failsafe.
sendai
12 Miles
E.T.A.S.
EXPANDABLE TSUNAMI ABSORPTION SYSTEM
3d natural systems design competition 2011