JDFEM.com |
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Juan de Fuca Emergency Management South coast of Vancouver Island BC, Canada |
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| Tsunamis -- Juan de Fuca Strait | |||
Worried about a tsunami?
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"The BIG ONE"
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"The LITTLE ONE"
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You just felt 3-4 minutes of shaking This is the Mag 9 super quake |
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| Quickly check for serious injuries.
Do not use phones. Leave them for emergency people Do not expect much help from 911, police, fire, ambulance, BC Hydro, and so on for days |
Go to the Tsunami Warning Center which is the original source where the media and emergency programs are getting their information. |
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If you live near the water Know the following before the quake because afterwards the Internet may not work. |
Know DEFINITION |
WARNING Advisory Watch |
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15 minutes in Tofino 30 minutes in Port Renfrew 1 hour in Sooke 1 hour 15 minutes in Victoria |
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| The tsunami will be fairly small , probably less than a meter The tsunami will not affect you unless you are in a HIGH RISK AREA close to the water such as camping or living near the water |
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Make sure you are a safe height above the water -- See official zones |
Do NOT go to the beach to watch You may get hurt, and you will be a nuisance to emergency operations and the police handling evacuations and road blocks. |
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Stay away from the water for 1-2 days |
Follow the progress of the small tsunami as it hits our coast and enters Juan de Fuca Strait. There is a 15 minute time lag, |
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Computer simulations These can show you beforehand what to expect |
A small tsunami at HIGH tide can drown people camping on the beach The picture shows the Japan tsunami hit first around low tide, ' but continued as the tide rose. |
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| See hint about Insurance | |||
JDFEM.com -- Juan de Fuca Emergency Management resource pages -- TSUNAMIS
Computer Simulations |
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| Institute of Ocean Sciences tsunami website Every image is one minute apart --- 12 Hours = total sequence. Use "Animation" buttons to view action. Use "Next" and "Back" buttons for tight control |
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Notice how few minutes it takes for the red tsunami to reach the outer coast, and the many reflections (meaning multiple peaks) The red zone at the start is water lifted by the locked zone as the continental shelf lunges ~20 meters forward in about 15 seconds It also gives an idea of the "epicenter" or moving locked zone, which is 1000 km long and 50-80 km wide. |
2Notice the length of a tsunami wave (the red patches), and how it bounces off one coast then another. A bay may not have a tsunami for several hours, then in a few minutes the water rises very high, surprising people (watch in the simulations when a bay suddenly turns red). The energy is absorbed bouncing around the gulf islands, so little gets to Vancouver. |
3CFB navy ships in Esquimalt Harbour have barely an hour after the shaking to get out in deep water before the tsunami hits, with very fast currents (the black lines in the simulations) This shows how a Seiche (saysh) wave begins to surge in and out of the harbour, like sloshng water in a shallow pan. It will be like a high tide to a low tide and back to high tide in less than 30 minutes, with over 20 knot currents. All small boats and docks will be damaged or destroyed. Navy ships may act like battering rams against their docks already weakened by the earthquake. |
4Victoria Harbour will get the first tsunami in about 1 hour and 15 minutes, then many other high surges because of Seiche waves like Esquimalt. However the surges will be broken up into separate resonances because of the narrow places. Many docks and boats will also be damaged by the fast surging action, including Fisherman's wharf. Signs should warn all boaters and tourists to stay away from the docks and floating homes for 24 hours or more. |
JDFEM.com -- Juan de Fuca Emergency Management resource pages -- TSUNAMIS
When will it hit? |
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| The following images are from the computer simulation done in 2004 of a Cascadia Mega-quake by
Josef Cherniawsky and others at the
Insititute
of Ocean Sciences for the Coast Guard.
This will give an approximate time of arrival after the mega-quake for planning purposes. Smaller tsunamis with smaller wavelengths will travel slower. |
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30 minutesafter START of shaking. Neah Bay -- water beginning to rise Most of JdF Strait -- water receding < 1 meter |
Size of earthquake area --the contnental shelf surging west and up to create the tsunami |
45 minutes This is where the tsunami would be when first seen on Neah Bay real-time Internet because of the 15 minute data upload delay. Port Renfrew -- water more than 1 meter and rising fast |
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1 hourPort Renfrew - water still peaking Sooke -- Water rising and surging around Whiffen Spit |
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1 hour 15 min Port Renfrew -- water rushing out Sooke -- peaking Esquimalt, Victoria -- water flowing in after receding Port Angeles -- rising fast |
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1 hour 30 min Port Renfrew -- water rushing in, 2nd peak coming Sooke -- after peak, water high, beginning to flow out. Esquimalt, Victoria-- peaking height but still rushing into harbours. Boats and docks a mess. Port Angeles -- peaking and piling high into harbour |
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1 hour 45 min Port Renfrew -- 2nd peak rushing in. Sooke -- water low and rushing out Esquimalt, Victoria-- beginning to recede All harbours and bays -- tsunami sets up resonances in each harbour and bay, with peak timing and heights quite variable, often ~20 minutes peak-to-peak, and repeats for several days. Water can rush in suddenly for at least next 48 hours. |
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JDFEM.com -- Juan de Fuca Emergency Management resource pages -- TSUNAMIS
JDFEM.com -- Juan de Fuca Emergency Management resource pages -- TSUNAMIS
How big will the tsunami be where you live? |
| Wave height represents the best consensus of scientific estimates of wave height at this time. 2x the wave height gives the expected maximum "runup" or height of destruction. 3x the wave height gives the expected "safety" level where people can be evacuated to, and they can stand safely watching the destruction. Planning level allows for subsidence.(see diagram below) However, observations of real tsunamis show the runup can vary greatly depending upon topography.Click on the picture at right to see how runup varies on the two sides of the valley in Japan, and the varying height on the right. The variable and unpredictable runup suggests it's good to have an extra margin of safety. |
| Official heights for planning -- pdf PLANNING FOR HIGHER SAFETY MARGINS IS CHEAP INSURANCE |
JDFEM.com -- Juan de Fuca Emergency Management resource pages -- TSUNAMIS
When is it safe to visit the shore? |
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A single wave through water spreads into a "wave train"---> and also reflects off the shores, and refracts (bends) around shallow water The Japan 2011 tsunami that DID arrive... Despite the ridicule of many people, and the media saying it was a false alarm, the Japan tsunami was a very real.
Western Canada (List) Vertical lines represent 3 hours each Tofino = + / - about 0.6 m max, or 1 foot up and down from normal for more many hours
Vertical lines represent 3 hours each Victoria = + / - about 0.3 m max, or ~6" up and down from normal, for more many hours...
American tide gauge sites from NOAA Notice how many highs and lows there are, and large tsunamis may come hours after the first! Vertical lines represent 12 hours each NEAH BAY (opposite Port Renfrew)
Vertical lines represent 12 hours each PORT ANGELES (opposite Sooke) |
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JDFEM.com -- Juan de Fuca Emergency Management resource pages -- Radiation
JDFEM.com -- Juan de Fuca Emergency Management resource pages -- TSUNAMIS
Definitions are important to avoid over-reaction |
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| Watch -- A distant quake produced a tsunami that might be a problem in a few hours Advisory -- A distant quake produced a tsunami that will affect our area but scientists are still monitoring how important it will be. Warning -- A distant quake produced a tsunami that is coming in a few hours, so start evacuating low areas, and turn on the sirens. A small tsunami, expecially at high tide, can drown people around beaches, and sweep them away. |
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Tsunami Watch - is issued to alert emergency management
officials and the public of an event
which
may later impact the watch area. The
watch
area may be upgraded to a warning or
advisory
- or canceled - based on updated information
and analysis. Therefore, emergency
management
officials and the public should prepare to take action. Watches are normally issued based on seismic
information without confirmation that
a destructive
tsunami is underway.A typical WATCH email from the Alaska Centre. "A TSUNAMI WATCH MEANS... ALL COASTAL RESIDENTS IN THE WATCH AREA SHOULD PREPARE FOR POSSIBLE EVACUATION. A TSUNAMI WATCH IS ISSUED TO AREAS WHICH WILL NOT BE IMMEDIATELY IMPACTED BY THE TSUNAMI. " |
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![]() . A typical ADVISORY email from the Alaska Centre. "A TSUNAMI ADVISORY MEANS THAT A TSUNAMI CAPABLE OF PRODUCING STRONG CURRENTS OR WAVES DANGEROUS TO PERSONS IN OR VERY NEAR THE WATER IS EXPECTED. SIGNIFICANT WIDESPREAD INUNDATION IS NOT EXPECTED FOR AREAS UNDER AN ADVISORY. CURRENTS MAY BE HAZARDOUS TO SWIMMERS... BOATS... AND COASTAL STRUCTURES AND MAY CONTINUE FOR SEVERAL HOURS AFTER THE INITIAL WAVE ARRIVAL." |
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![]() This was a WARNING email for Japan sent from the Alaska Centre. "A TSUNAMI WARNING MEANS... ALL COASTAL RESIDENTS IN THE WARNING AREA WHO ARE NEAR THE BEACH OR IN LOW-LYING REGIONS SHOULD MOVE IMMEDIATELY INLAND TO HIGHER GROUND AND AWAY FROM ALL HARBORS AND INLETS INCLUDING THOSE SHELTERED DIRECTLY FROM THE SEA. THOSE FEELING THE EARTH SHAKE... SEEING UNUSUAL WAVE ACTION... OR THE WATER LEVEL RISING OR RECEDING MAY HAVE ONLY A FEW MINUTES BEFORE THE TSUNAMI ARRIVAL AND SHOULD MOVE IMMEDIATELY. HOMES AND SMALL BUILDINGS ARE NOT DESIGNED TO WITHSTAND TSUNAMI IMPACTS. DO NOT STAY IN THESE STRUCTURES. ALL RESIDENTS WITHIN THE WARNED AREA SHOULD BE ALERT FOR INSTRUCTIONS BROADCAST FROM THEIR LOCAL CIVIL AUTHORITIES. A TSUNAMI HAS BEEN RECORDED." |