Questions
SOI-BBS
soi-asia@soi.wide.ad.jp
Tsunami Seminar
Copyright
- Tsunami Trace Measurement and Some Examples in Sri Lanka and Sumatra - Differences of Tsunami Height due to Local Topography -
- Contents (1)
- Contents (2)
- Purposes of tsunami survey
- Selection of survey site(1)
- Selection of survey site(2)
- Selection of survey site(3)
- Selection of survey site(4)
- Survey period(1)
- Survey period(2)
- Survey period(3)
- Survey planning with other survey teams and local experts
- Coordination of survey teams and role of information center
- DPRI's Indian Ocean Tsunami page
- Application of Internet and e-mails
- Japan's area sharing (Trace measurement only)
- Planning and coordination - Example in Sri Lanka -(1)
- Planning and coordination - Example in Sri Lanka -(2)
- Planning and coordination - Example in Sri Lanka -(3)
- Planning and coordination - Example in Sri Lanka -(4)
- Planning and coordination - Example in Sri Lanka -(5)
- Planning and coordination - Example in Sri Lanka -(6)
- Make-up of a survey team
- Preparation and equipment
- Instruments - elevation -
- Instruments - distance or positioning -
- Instruments - distance and elevation -
- Instruments - communication -
- Finding traces
- Finding traces - Water mark on house and building -
- Finding traces - Broken part of structure -
- Finding traces - Vegetation, floating garbage deposition, etc. -
- Runup height and inundation depth
- Effect of local topography - hilly place and low land -(1)
- Effect of local topography - hilly place and low land -(2)
- Hambantota residential area(1)
- Hambantota residential area(2)
- Hambantota residential area(3)
- Hambantota residential area(4)
- Hambantota harbor area(1)
- Hambantota harbor area(2)
- Hambantota harbor area(3)
- Hambantota harbor area(2)
- Hambantota harbor area(3)
- Oncoming tsunami waves in Hambantota area(1)
- Oncoming tsunami waves in Hambantota area(2)
- Geographical character of Hambantota area
- Effect of local topography - exceptional condition -(1)
- Effect of local topography - exceptional condition -(2)
- Lepung - long distance measurement -(1)
- Lepung - long distance measurement -(2)
- Lepung - long distance measurement -(3)
- Lepung - long distance measurement -(4)
- Lepung - long distance measurement -(3)
- Lepung - long distance measurement -(4)
- Lepung - long distance measurement -(5)
- Lepung - long distance measurement -(3)
- Lepung - interview -
- Rhiting - Exceptional tsunami height -(1)
- Rhiting - Exceptional tsunami height -(2)
- Rhiting - Exceptional tsunami height -(3)
- Rhiting - Exceptional tsunami height -(4)
- Rhiting - Exceptional tsunami height -(5)
- Rhiting - Exceptional tsunami height -(6)
- Rhiting - Exceptional tsunami height -(7)
- Rhiting - Exceptional tsunami height -(8)
- Rhiting - Exceptional tsunami height -(9)
- Rhiting - Exceptional tsunami height -(10)
- Rhiting - Exceptional tsunami height -(11)
- Rhiting - Exceptional tsunami height -(12)
- Erosion, sediment movement - Impact to environment -
- Post-survey local meeting - brief report -
- Post-survey data processing - Sea level correction and GPS correction -
- Data sharing and utilization
- Reference
- Q1 from Brawijaya(1)
- Q1 from Brawijaya(2)
- Q2 from Syiah Kuala