Technical Description-4Tsunami Observations: | ||||
The following background information on tsunami observations on coastal sea level stations was provided by the ITIC to participants during training courses in 2006 and 2007. It provides a practical illustration of the tsunami science principles.
Relevant Points: a. Tsunami are a series of waves that continue for many hours. b. The 1st wave height may not be the largest. c. The largest wave may not occur at the station closest to the earthquake. d. Tsunami signals arriving at coastal stations are affected by local conditions,such as the e. Tsunami wave periods can vary from minutes (5-10) to one hour. Waveforms for the Tokachi-oki earthquake (M8.0) and tsunami, 26 September 2003 Notes:
Relevant Points: a. The earthquake rupture determines the initial character of the tsunami wave. b. In theory, for a subduction zone thrust earthquake, the thrusting plate moves the ocean c. In reality, seafloor topography between the tsunami source and affected coast will modify
The 1st tsunami wave arrival will be an advancing wave (wall of water) toward China, and a receding wave at Luzon, Philippines. With time, the wave character is changed by seafloor topography. The trailing trough catches up to crest in the north (A), but not in the south (A').
|
The figures on this page were created using Generic Mapping Tools open-source software (GMT; Wessel, P. and W. H. F. Smith, New, improved version of Generic Mapping Tools released, EOS Trans. Amer. Geophys. U., Vol. 79 (47), pp. 579, 1998). |