ࡱ> '` pbjbjLULU 4z.?.?- H< < < < @ @ @ T <<<8ttT `Fx])])])"_$_$_$_$_$_$_$[bhdH_i@ ]);)"])])])H_< < _(---])< @ "_-])"_--VD J@ Yl 06t%<+:`W&]d_<`WfYe?+vYeLYYYe@ v[H])])-])])])])])H_H_+N])])])`])])])])T T T dT T T T T T < < < < < <   Section 2: Conducting the Field Survey Types of Data Collected Methods (5 pages) Ahmet Yalciner, Fumihiko Imamura, Herman Fritz Satellite, aerial, stereoscopic, and other reconnaissance for overview Specialized field and marine surveys Eyewitness interview for wave timing and character, how damage occurred, warning and evacuation response, etc Collecting photos/videos taken by local people using mobile phone, etc (International Tsunami Survey Teams (ITSTs) are often deployed to conduct rapid post tsunami assessments).The post tsunami field survey starts with the communication between the team members) about the event and the situation at survey site. by satellite, aerial, stereoscopic, and other reconnaissance for overview. The preliminary travel and local transportation plan should also take into the agenda. The preliminary information obtained from local and international authorities and media reports should be evaluated and discussed. The team must be well prepared against difficult conditions at the survey site. The proper equipment and devices must be selected. Each team member must have proper and sufficient medical supplement. The post tsunami surveys are conducted rather dynamic daily survey plans at site and consist of specialized field and marine surveys. (i.e. field measurement of sediment, collection and measurement information about environmental and biophysical system impacts of the tsunami on the terrestrial and marine environment in selected locations.) Eyewitness interviews can be invaluable in helping distinguish actual effects of the events (earthquake tsunami) from pre-event conditions and post-event changes like damage clean-up. Eyewitness interviews, measurement of instruments, or local press reports, the times of arrival and periods of the tsunami waves, their number, tsunami arrival time after earthquake shaking and the total duration of the tsunami. Individual interviews with each eyewitness are recommended in order to cross check the information and distinguish the exaggerated information. The other important type of data is visualized materials such as photos, videos taken by local people before, during and after the event. The methods of post tsunami field surveys consist of different stages. These stages are; Evaluation of the information about the event Communication and establishing the team(s) and team members Travel plan of each team member Preparation of the necessary equipment Meeting at a suitable location near or at the site Organizational meeting(s) between local authorities and team members Obtaining local administrative and logistic support Determining the survey areas and tentative time of visits Obtaining all available local data Equipment check up Survey (s) by the team or by the groups of the team members Daily discussion and organizational meetings by the team members Coordination with local authorities and other teams Daily adjustment of survey plan Daily reports from each survey site Final meeting(s) with local authorities and other teams Reporting There must be the additional information about the photographs, videos and other visual materials such as the coordinates of the location and time. Tsunami wave information (5 pages) Ahmet Yalciner, Fumihiko Imamura, Koshimura Run-up, Inundation, Flow Depth, Wave Height , (flow velocities) Wave arrival times Wave character (size, description of what wave looked like, direction, velocity/current) Tidal data/condition General topics to collect field information are; " tsunami source type, " tectonic and seismic parameters, " earth landslides and submarine slumps, " effects of earth deformation, faulting and folding, " tsunami approach and arrival parameters, " tsunami effects, damage and casualties, " response of the public and authorities, - collection of information on human and community vulnerability and resilience factors, " additional observations, comments and recommendations The necessary data can be collected in post tsunami surveys are two types as i) instrumental and ii) observational. Instrumental data is collected directly by instruments. Observational data is collected indirectly by the help of questionnaires and interviews. Main tsunami parameters at shallow and inundations zone are; the water level before the tsunami direction of the tsunami approach observed wave amplitude near the shore, runup height at land, highest water marks at trees and walls of the structures, arrival time of first and maximum wave, number and amplitude of maximum wave(s), inundation limit at land, depth where shoreline receded, direction of flow and flow depth at land, level of flow velocities, Levels (thickness) and spatial distribution of erosion and deposition. Ground uplifting and/or subsidence (size and shape) Landslides and/or slumps (volume, rate, direction, orientation, type and size of the material if avalable) Human belongings, dead marine species, and/or other natural or artificial objects, or animals caught and/or hanging in the upper branches of trees, are also reliable indicators The brief information about these characteristics is given in the following. Some of the parameters are also shown in the Figure  SHAPE \* MERGEFORMAT  Figure: Cross sectional view of tsunami at shallow and inundation zone The water level before the tsunami The water surface elevation above still water level in a particular region before the generation of tsunami The water level at the time of survey The water surface elevation above still water level in a particular region before the generation of tsunami Short description of the survey area. The coordinates and elevations of some control points at the survey area should be measured in order to verify the data from satellite image Direction of the tsunami approach The direction from which tsunami approaches to the shore Observed wave amplitude near the shore, The tsunami wave amplitude is the vertical distance from the still-water level to the water surface either below or above. Runup height at land, The height of the water onshore observed above a reference sea level usually at the horizontal inundation limit. Highest water marks at trees and walls of the structures, The water marks on trees and wall of the structures in tsunami inundation zone showing the maximum water surface elevation. Lines of landward limit of sea grass, debris, sediment, or oating garbage deposition, horizontal boundaries between vegetation killed or damaged by saltwater and surviving vegetation (discoloration after a few weeks is a good indicator), amounts of bark stripped from trees, and levels of seaweed or debris caught in screens or other structures, are also good indicators Arrival time of first and maximum wave, Arrival time of first and maximum wave of the tsunami at a particular location during tsunami propagation and inundation Amplitude of maximum wave, The amplitude of tsunami wave with the highest water surface elevation during a tsunami event at the specified depth. Maximum water level at inundation zone Maximum water level is the difference between the elevation of the highest local water mark and the elevation of the shoreline at the time of tsunami attack (i.e., corrected for the difference in shoreline elevation between the time of measurement and the time of tsunami attack). Inundation limit at land, The inland limit of wetting measured horizontally from the edge of the coast defined by mean sea level. Depth where shoreline receded, The water depth where the maximum tsunami withdrawal occurs (the drawdown limit) Direction of flow and flow depth at land, Direction of water flow towards the shoreline during tsunami inundation Flow depth at land is the vertical distance between the slope of land and the water surface in inundation zone. Level of flow velocities, The level of flow velocities during tsunami can be estimated from the evidences of flow direction and/or flow strength. The estimated flow dept and magnitude of the drag and inertia forces which dragged the objects can give information about the level and strength of the flow during tsunami. Flow direction can be inferred from geometrical orientation patterns of debris accumulation or from the direction of tree falls. Levels (thickness) and spatial distribution of erosion and deposition (sudden erosion, transport, and deposition of sediments (volume, type, and rate) The levels of erosion and scour during the drawdown stage of the tsunami where the soil strength is reduced by the reduction of the effective stresses. The characteristics of the sediment in the sea and at land, its grain size and density at erosion deposition areas must be measured. The information (if any) about the flow velocities at erosion and scour areas should also be collected and reported. Ground uplifting and/or subsidence (size and shape), Landslides and/or slumps (volume, rate, direction, orientation, type and size of the material) Human belongings, dead marine species, and/or other natural or artificial objects, or animals caught and/or hanging in the upper branches of trees, are also reliable indicators. (Note that some plants (i.e. palm trees) die if salt water touches its leaves at top) In order to clarify these tsunami parameters and related tsunami effects the following parameters will also be needed in assessment studies at later stages, time earthquake felt by the local people at site, ground and vegetation characteristics, location, dimensions and types of marine and land structures. The followings are additional data should be collected at site according to their availability. Morphological Information The reflection from the other coastline (if any) and underwater abnormalities which may affect tsunami directivity and energy focusing at site should be investigated. The cross section of the coastal slope should be measured or estimated properly Geological Information Locations of the extent of possible coastal uplift or subsidence areas and their influence in the tsunami runup Seismological Information During the survey, at remote areas, aftershock data from portable seismographs can be obtained. Ecological Information Ecosystems and biodiversity The recent technologies and equipments are necessary in data collection during the field survey for the quality of the data. All equipments and methods should also be indicated in the survey report. A summary table (sample is given in Table 1) should be prepared in detail. 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