Your SlideShare is downloading. ×
s1180202
s1180202
s1180202
s1180202
s1180202
s1180202
s1180202
s1180202
Upcoming SlideShare
Loading in...5
×

Thanks for flagging this SlideShare!

Oops! An error has occurred.

×
Saving this for later? Get the SlideShare app to save on your phone or tablet. Read anywhere, anytime – even offline.
Text the download link to your phone
Standard text messaging rates apply

s1180202

390

Published on

0 Comments
0 Likes
Statistics
Notes
  • Be the first to comment

  • Be the first to like this

No Downloads
Views
Total Views
390
On Slideshare
0
From Embeds
0
Number of Embeds
0
Actions
Shares
0
Downloads
1
Comments
0
Likes
0
Embeds 0
No embeds

Report content
Flagged as inappropriate Flag as inappropriate
Flag as inappropriate

Select your reason for flagging this presentation as inappropriate.

Cancel
No notes for slide

Transcript

  • 1. System of Tsunami~What is System of Tsunami~ s1180202 Motohito Yoshida
  • 2. Simulation Of TsunamiAround Japan, the severe earthquake might occur in the vicinity of the coast.In that case, the calculation began after the earthquake occurswith the latest computer, and because the tsunami raids aJapanese coast at once after the earthquake occurs, thetsunami warning cannot be announced by the time the tsunamireaches.Then, the fault with the possibility to generate the tsunami is setbeforehand, the numerical simulation of the tsunami is done,and the result is accumulated as a tsunami forecast data base.1. The horizontal position and depth of fault2.Size of fault3.The direction of fault4.Inclination of fault5.Direction and size of slippingIt is necessary to provide it.The direction of the fault has been decided referring to a past earthquake.To deal even if the earthquake of what size occurs in what place, a lot of simulations are done about the horizontal position of the fault, depth, the size of the fault, and the sizeof slipping.About the inclination and the direction of slipping, of the fault, it is a setting that most greatly generates tsunamis, and the inclination assumes 45° to be a purereverse fault .
  • 3. The fault is about 1,500 places to horizontal direction, and it thinks about four kinds, and one fault requests of diastrophism of these in bottom ofthe sea of 6 kinds and magnitudes to depth to and from 0-100km.This is handed over to the tsunami spread calculation.
  • 4. tsunami spread calculationIn general, it can be thought that the bottom of the sea diastrophism that generates the tsunami becomesa ruggedness that the vertical movement of the ocean crust is caused in the surface of the seaimmediately after the occurrence of the earthquake the state as it is because diastrophism is completedbefore it has the extension of tens of kilometers or more, and the tsunami begins to extend.The surface of the sea ruggedness pattern obtained thus is assumed to be an initial source of wave of thetsunami, and the appearance where this is transmitted in every direction is calculated.The computational domain is delimited in detail like the lattice in length and breadth, and as the method ofthe math calculation, time of height and the speed of the tsunami in each lattice is chased and calculatedaccording to the equation of the tsunami spread.It calculates for all faults like this, and the appearance of the temporal variation of the tsunami thatappears in the coast is reproduced.
  • 5. Forecast of height of tsunami in coast There is no height of the tsunami that becomes the standard of the tsunami warning expected in the coast because it uses height in the coast calculated by the simulation as itis. It is because of depths in the vicinity of the coast being thought to be a fall of the repeatable precision of the tsunami in the place where geographical features shallowlybecomes complex, too because the size of the computational grid is made constant. It takes a great amount of time to calculate the whole country, and it is not realistic thoughthere is a method of doing a very detailed make the computational grid detailed in the vicinity of the coast to solve this calculation.Then, height in the coast is presumed by using "Green law" from the height of the tsunami in being the offing combination in no still very inclusion of the error margin.The speed of the tsunami slows if a tsunami offshore (point where depth is deep) comes to the place where depth of the coast is shallow, and the interval between the previouswave and the wave in the back shortens. However, the energy conserved in the person wave must be equal.The wave surface is a coastline and the height of the wave rises as a result to the extent that the interval between the wave and the wave shortens when entering into going sideby side. This is a green law.
  • 6. Making of warning and warning of eachforecast district in JapanThe Meteorological Agency is informing you of height and the attainment expectation time of the tsunami of each tsunami forecast district where the coast in the wholecountry was divided into 66 expected that the tsunami warning and the warning are announced.These tsunami forecast districts are set considering it for the emergency in the related disaster prevention organization such as municipalities when warning and thewarning are announced after the feature of how of a tsunami different according to geographical features to appear is investigated.Here, it explains how the Meteorological Agency is making warning and the warning of the forecast district.In the tsunami warning and the warning of the forecast district, it announces judging "Tsunami", "Tsunami", and "Tsunami advisory" based on the highest in that valueamong the predictive values of the height of the tsunami in two or more points in the forecast district, and unifying the maximum height.What applies a green law to the tsunami simulation calculation result to a point (forecast point) left for being the offing combination from the coast at about 15km basedon the method of above-mentioned "Forecast of the height of the tsunami" and converts it into height in the coast is used for the tsunami height presumption of anindividual point.
  • 7. Attainment time of tsunamito forecast districtThe computational error of the attainment expectation time of the tsunami grows in the vicinity of the coast where depth is shallow.Then, the tsunami attainment time to the forecast district is calculated by adding time that the tsunami spreads from there to the coast at the attainment time in the forecastpoint it is the offing combination of obtaining because of the simulation.Gravitational acceleration is used, and at this time, g and depth are assumed to be h, and the tsunami uses transmitting in the sea at the speed of √gh.How to the forecast district to request the attainment expectation time is as follows. ①  The point where the spread time from the forecast point is equal is connected from the depth data aroundthe forecast point.  ②  The spread chart of the tsunami is made by repeating ①.  ③  The spread time of the tsunami from the forecast point to the coast can be read from the tsunami spreadchart.   ④  The earliest one is made the attainment expectation time to the forecast district about all the forecastpoints in the forecast district for the attainment expectation time to the coast sooner or later.  The attainment expectation time to the tidal observatory is used to announce for the spread time from each tidal observatory to the source of wave of the tsunami.
  • 8. Comparison with past tsunami recodeThe observed value and the predictive value of a past tsunami are compared by using the tsunami forecast data base that does as mentioned above and makes it.When the height of the tsunami of 139 cases where the tsunami has been observed so far was seen, the average of the ratio of the observed value in the tidal observatory andthe predictive value of the data base became about 1.2, and became good on average the observed value when reproducing it.On the other hand, the predictive value to the tsunami forecast district announced by the tsunami warning and the warning is about 1.8 times on the average because itadopts the maximum predictive value in the forecast district (Refer to < height of the tsunami in the forecast district >) compared with the observed value.However, the tsunami can become a tsunami that is bigger than the height of the expectation of the tsunami told by the tsunami warning and the warning according tocircumstances because there is a character that height changes greatly because of local geographical features.Leaving of shelter to the height at once from the coast at once if the tsunami warning is announced if the warning is announced is important.

×