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s of Nine days of experimental data demonstrated that the sys- IUGG in Birmingham, B.,.tem precisely tracks sea-level, when compared to tide-gauge Hino, R., T.Kanazawa, S.Sakai, Y.Tanioka, and K.Suyehiro, Tsunamis data.TheSensor-buoy does not respond to short period wind- from an off-Sanriku and the Papua New Guinea earthquakes observed by ocean bottom tsunami measurement, Programme and Abstracts The Seis- waves compared to the Support-buoy, suggesting that a spar- mological Society of Japan, , Fall Meeting P , in Japanese.type buoy is preferable for detecting long period waves such Kato, T., Y.Terada, M.Kinoshita, H.Isshiki, and A.Yokoyama, GPS as tsunami.FrequencyT.M., G.H.Born, M.E.Parke, and C.Rocken, Precise mean sea- it is feasible to detect a tsunami, because a tsunami has, in level measurements using the Gl
experimental, birmingham, sea-level tide-gauge, tkanazawa, ksuyehiro, sensor-buoy, off-sanriku, earthquakes, measurement programme, programme abstracts, support-buoy, mological, japanesetype, preferable, mkinoshita hisshiki, hisshiki ayokoyama, tsunamifrequency analysis, analysis tsunami-kei, tsunami-kei kaihatsu, japanesekelecy, measurements,
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