HAWAII KAI TSUNAMI HAZARD July 2006. SWAN Model for Hawaii Kai Click above for Movie SWAN Model for Hawaii Kai Click above for MovieSWAN Model.

Slides:



Advertisements
Similar presentations
Charles Mader PACON - Paper and PowerPoint
Advertisements

KRAKATOA Hydro- Volcanic Explosion and Tsunami
Prepare For The Worst Hope For The Best. Potential and somewhat probable worst case disasters include: Epidemics Epidemics Terrorism Terrorism Tsunamis.
TSUNAMI HAZARD TO Hawaii from a M9+ Event similar to 2004 Indian Ocean Tsunami SAWG SAWG Hawaii Civil Defense 11/2007.
Around the World in 60 Days March 11 to May 10, 2009 China Airline – Honolulu to Hong Kong – 5546 miles Tahitian Princess – Hong Kong to Dover – 16,009.
Coastal Ecology and Sustainability
Rip Current Statistics Rip Current Formation Types.
1960 Chilean Earthquake By Ola Smith. Basic Info Magnitude: 9.5 Death toll: Injuries: 3000 Damage: 130,000 homes destroyed, 2 million people.
TSUNAMI Provided by G. Wuesthoff.
Kenji HARADA DRS, DPRI, Kyoto Univ.
By Alexandra Busato April is Tsunami Awareness Month!
Evaluation of the effect of the disaster prevention technique using coastal farmlands Kiri H. and H. Tanji National Institute for Rural Engineering National.
Tsunamis!.  A tsunami is a series of ocean waves generated by sudden movement in the sea floor.  In the deep ocean, the tsunami wave may only be a few.
 Currents that run along the western coast of the United States are _________________.  Currents that run along the eastern coast of the United States.
Tsunami. Why did the earthquake cause a tsunami?the earthquake cause tsunami Shallow focus earthquake Large volume of oceanic crust displaced The movement.
2011 Tōhoku Earthquake and Tsunami. MODIS satellite image on 26 FEB, before the tsunami. Scale bar is 10 km.
Tsumani’s By Jessica Scheper
AIM: How do Tsunamis form? DN: What is a tsunami? What type of damage does a tsunami cause? HW: Article.
Tsunamis!!. Tsunami Tsunami – Japanese word that means “harbor wave”
By: Courtney Stryke ♥ 12/20/06 Blue
By: Yazan HAJJAR What is a Tsunami? A Tsunami is a set of huge waves of water that are usually caused by earthquakes or volcanic eruptions. This happens.
Tsunamis Oceans 11. What is a tsunami? Tsunamis are defined as extremely large ocean waves triggered by underwater earthquakes, volcanic activities or.
TSUNAMI.  Aerial view of Japanese Tsunami Aerial view of Japanese Tsunami  Ground level view of Tsunami Ground level view of Tsunami  The Japanese.
Tsunami toll could top 100,000, Red Cross says.
Chapter 8 Waves and Water Dynamics
Natural Hazards and Disasters Chapter 5 Tsunami. Tsunami is a “harbor wave” Waves rise highest where focused in bays or harbors.
OCEAN MOTION Coulter. Most waves form when winds blowing across the water’s surface transmit their energy to the water. Wave-movement of energy through.
Coastal Environmental Geology. Environmental Issues and Coastal Geology Excessive Sedimentation Shoreline Erosion Coastal Subsidence Sea Level Rise Storm.
THE NEXT DESTRUCTIVE TSUNAMI: ITS NOT IF, BUT WHEN.
Tsunamis GEOL 4093 Risk Assessment. Tsunamis Also known as “seismic sea waves” Generating force is not wind, but movement of the sea floor, volcano, landslide,
Tsunamis Oceans 11. What is a tsunami? Tsunamis. are defined as extremely large ocean waves triggered by underwater earthquakes, volcanic activities or.
TSUNAMI BASIC INFO 1.) Tsunami are NOT tidal waves, they have nothing to do with tides 2.) They are caused by “BIG SPLASHES” from… *earthquake motion (Fig.
Tsunami! Tidal waves of destruction CHAPTER 2, CRO #7.
Tsunamis By: Taylor Murphy & Merry Nestor. How do tsunamis occur ? When a tsunami leaves the deep ocean it travels to the shallow water near the inlands.
Hurricane Ike. Natural Hazards and Disasters Chapter 5 Tsunami.
PACIFIC TSUNAMI WARNING CENTER Ewa Beach, Hawaii US Department of Commerce National Weather Service.
Tsunamis. Amateur videos from the 26 December 2004 tsunami in SE Asia What is a tsunami? What can cause a tsunami? Wave basics (three formulas you need.
Super Tsunamis By: Faith Hatchard
Xiaoming Wang and Philip L.-F. Liu Cornell University
Tsunamis.
Sumatra Earthquake & Indian Ocean Tsunami
Mega Tsunami Recently, scientists have realized that the next Mega Tsunami is likely to begin on one of the Canary Islands, off the coast of North Africa,
HAWAII KAI TSUNAMI HAZARD 2 Zone Evacuation Zone October 2015.
2004 Indian Ocean Tsunami Minhae Park Grade 8 Science.
2004 INDIAN OCEAN TSUNAMI (BOXING DAY TSUNAMI) JACK MEEKS NICOLE WHITE ANA HEIMULI ANTONE BURBIDGE.
Oceanography. How much of the Earth’s surface is water?
Weathering and Erosion. MOVING WATER What do we call the movement of water? –Water Cycle (I hope you didn’t forget) How do you think the water cycle causes.
Introduction to Aerial Stereo Photographs
Nama: RETNO Kelas: XII IPS-1 Judul : Explanation Texs.
Tsunami Tsunami – a large destructive wave that is the result of a geologic process such as an earthquake (most likely), volcano, or land slide (both.
Tsunamis By Joe Pappalardo and Matt Voegelin. Definition An unusually large sea wave produced by a seaquake or undersea volcanic eruption.
Hazards: Take Control TSUNAMI By NEMO Saint Lucia.
Tsunami. What is a Tsunami December 26th Tsunami hits the Indian Ocean. December 26th Tsunami hits the Indian Ocean. Indonesia, Sri Lanka,
Tsunami death toll Indonesia94,081 Sri Lanka28,729 India9,067 Thailand4,993 Somalia200 Myanmar90 Maldives80 Malaysia68 Tanzania10 Bangladesh December 26,
Tsunami. The name ‘tsunami’ is Japanese. It means harbor wave. Tsunamis used to be called tidal waves, but they actually have nothing to do with the tides.
Tsunami Tsunami also know as seismic waves, are a series of enormous waves created by an underwater disturbance such as an earthquake, landslide, volcanic.
Weathering & Erosion Chapter 4 Lesson 3 Page 192.
Tsunami.
Landforms.
Tsunami Mathematics.
TSUNAMI DONE BY: Sami Mubarak Khalfan Al-Ma’mary ID:
Japan’s Earthquake &Tsunami 2011
TOPIC 1:TECTONIC PROCESSES AND HAZARDS
Wavees part 2 Tsunami.
The devastating impact of seismic sea waves
amplification of seismic waves: tsunami (seismic sea waves), T&L, Fig
The devastating impact of seismic sea waves
Tsunami.
Presentation transcript:

HAWAII KAI TSUNAMI HAZARD July 2006

SWAN Model for Hawaii Kai Click above for Movie SWAN Model for Hawaii Kai Click above for MovieSWAN Model for Hawaii KaiSWAN Model for Hawaii Kai On CD-ROM in Numerical Modeling of Water Waves – CRC Press (2004) On CD-ROM in Numerical Modeling of Water Waves – CRC Press (2004) A train of 3 meter high, 1500 second tsunami waves. 30 DeChezy Friction. A train of 3 meter high, 1500 second tsunami waves. 30 DeChezy Friction. Modeled 15 years ago. Modeled 15 years ago. Topography of bay from Sea Engineering depth measurements for Ferry Feasibility Study. Topography of bay from Sea Engineering depth measurements for Ferry Feasibility Study. Floods up to 5 meters inside front of bay and a min of 2 meters in back of bay by third wave. Floods up to 5 meters inside front of bay and a min of 2 meters in back of bay by third wave.

Hambantota, Sri Lanka Dr. Hermann Fritz surveyed after December 26, 2004 Indian Ocean Tsunami Dr. Hermann Fritz surveyed after December 26, 2004 Indian Ocean Tsunami Noted that it was similar to Hawaii Kai with reef outside with a channel under a road along the sea shore into a large shallow lake. Noted that it was similar to Hawaii Kai with reef outside with a channel under a road along the sea shore into a large shallow lake.

Hambantota Tsunami Wave arrived a little over 2 hours after earthquake. The first wave was about 1 meter high and the second wave was up to 10 meters high about 10 minutes later. Wave arrived a little over 2 hours after earthquake. The first wave was about 1 meter high and the second wave was up to 10 meters high about 10 minutes later. Houses over 1 kilometer inland were demolished. Houses over 1 kilometer inland were demolished.

Tsunami Effects Little of the town was left standing with no water, electricity or communications. Little of the town was left standing with no water, electricity or communications. One thousand houses along the Hambantota-Tissa road, town-council residences, shops and other buildings destroyed. Many homes located near the Hambantona harbor were completely washed away. One thousand houses along the Hambantota-Tissa road, town-council residences, shops and other buildings destroyed. Many homes located near the Hambantona harbor were completely washed away.

Loss of Life When the tsunami hit, hundreds of local people were visiting Sunday markets. When the tsunami hit, hundreds of local people were visiting Sunday markets. Two to three thousand people were promenading along Hambantota harbor when the tsunami wave struck. Two to three thousand people were promenading along Hambantota harbor when the tsunami wave struck. The overwhelming majority of these died. The overwhelming majority of these died. Over 4500 died in low-lying coastal strip Over 4500 died in low-lying coastal strip

HAMBANTOTA, SRI LANKA December 26, 2006 Tsunami DEATH ZONE WAS AREA BELOW 10 METERS and LESS THAN 1 KILOMETER FROM SHORE. DEATH ZONE WAS AREA BELOW 10 METERS and LESS THAN 1 KILOMETER FROM SHORE.

Multiple Tsunami Waves Often populated areas along coasts are located in low-lying and flat regions that together with natural and man made obstacles make retreat of the flood caused by first tsunami wave to be slow. Subsequent waves ride over a region already flooded resulting in higher and faster waves. Often populated areas along coasts are located in low-lying and flat regions that together with natural and man made obstacles make retreat of the flood caused by first tsunami wave to be slow. Subsequent waves ride over a region already flooded resulting in higher and faster waves.

Sri Lanka Multiple Tsunami Waves The multiple wave phenomenon was observed throughout the Sri Lanka coast. The multiple wave phenomenon was observed throughout the Sri Lanka coast. It wasnt one wave, it came in great surges, each one deeper than the last and pushing the water that had come in before it in front of it. It wasnt one wave, it came in great surges, each one deeper than the last and pushing the water that had come in before it in front of it.

Sri Lanka Multiple Tsunami Waves Most witnesses described 3 main waves. Most witnesses described 3 main waves. The first knocked them off their feet, the second picked them up and carried them, often up to 50 km/hr, and the third bore them up to 15 meters high or sucked them under. The first knocked them off their feet, the second picked them up and carried them, often up to 50 km/hr, and the third bore them up to 15 meters high or sucked them under.

Fritz Indian Ocean Tsunami Survey Conclusions Evacuate all areas below 15 meters above sea level and within 0.25 mile of shoreline or along rivers. Evacuate all areas below 15 meters above sea level and within 0.25 mile of shoreline or along rivers. Evacuate all areas below 10 meters above sea level and within 1.0 mile of shoreline or along rivers. Evacuate all areas below 10 meters above sea level and within 1.0 mile of shoreline or along rivers. Evacuate all areas below 5 meters above sea level and within 3 miles of shoreline. Evacuate all areas below 5 meters above sea level and within 3 miles of shoreline.

"The Hawaii Kai evacuation zone should include all areas "The Hawaii Kai evacuation zone should include all areas below 5 meters above sea level" below 5 meters above sea level" Consider the 1946 historical observations as recorded in Consider the 1946 historical observations as recorded in United States Tsunamis (page 66) United States Tsunamis (page 66) Waipio Valley - 12 meter run-up amplitude Waipio Valley - 12 meter run-up amplitude Swept 1 mile into valley, pulled away homes and people Swept 1 mile into valley, pulled away homes and people and left only foundations and left only foundations Waikolu Valley, Molokai meter run-up amplitude Waikolu Valley, Molokai meter run-up amplitude Destroyed farms and buildings up entire valley. Destroyed farms and buildings up entire valley. Makapuu Point, Oahu meter run-up amplitude Makapuu Point, Oahu meter run-up amplitude Destroyed the nearby Ranch buildings with 3 waves (Helsley Destroyed the nearby Ranch buildings with 3 waves (Helsley from wave deposits) leaving only foundations. from wave deposits) leaving only foundations. Three wide valleys destroyed by the 1946 tsunami are Three wide valleys destroyed by the 1946 tsunami are historical evidence that Hawaii Kai is at risk. historical evidence that Hawaii Kai is at risk.

HAWAII KAI MINIMUM Evacuation zone should include all area below 5 meters above sea level. MINIMUM Evacuation zone should include all area below 5 meters above sea level. 3 Meter Tsunami Flooding Graphic 3 Meter Tsunami Flooding Graphic MOVIE AVAILABLE ON NMWW DVD MOVIE AVAILABLE ON NMWW DVD

Sandy Beach and Queens Gate 3 meter, 1500 sec Tsunami 3 meter, 1500 sec Tsunami 10 meter, 1500 sec Tsunami 10 meter, 1500 sec Tsunami From Numerical Modeling of Water Waves CD-ROM, CRC Press (2004). From Numerical Modeling of Water Waves CD-ROM, CRC Press (2004). All of Queens Gate up to Hawaii Kai Drive should be in evacuation zone. All of Queens Gate up to Hawaii Kai Drive should be in evacuation zone. MOVIE AVAILABLE ON NMWW DVD MOVIE AVAILABLE ON NMWW DVD

–Queens Gate