Tsunamis
DOI: 10.1007/1-4020-3331-1_19
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Hydro-Acoustic Monitoring on the Kamchatka Shelf: A Possibility of Early Location of Oceanic Earthquake and Local Tsunami Warning

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Cited by 3 publications
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“…Additionally, as t-phases experience a reduced degree of geometric spreading (cylindrical, ∼ 1 r , rather than spherical, ∼ 1 r 2 ), they may offer greater sensitivity to more distant or smaller seismic events than would be obtained from the corresponding P or S waves at the same epicentral distance; furthermore, the lower and better-constrained sound speed in water can yield tighter constraints on source location than are possible from signals in the solid Earth alone (Dziak et al 2004). Other potential uses of hydroacoustic phases include early-warning systems for tsunamis (Sasorova et al (2005), ), acoustic thermometry for remote monitoring of long-term changes in ocean temperature (Dushaw et al 1999), detection of glacial and ice-calving events (Chapp et al 2005), as well as monitoring of cetacean populations (e.g. McDonald et al (1995), Dréo et al (2019)) and for illicit nuclear tests in violation of the Comprehensive Nuclear Test Ban Treaty (Mitchell (2002), Okal (2008)).…”
Section: Introductionmentioning
confidence: 99%
“…Additionally, as t-phases experience a reduced degree of geometric spreading (cylindrical, ∼ 1 r , rather than spherical, ∼ 1 r 2 ), they may offer greater sensitivity to more distant or smaller seismic events than would be obtained from the corresponding P or S waves at the same epicentral distance; furthermore, the lower and better-constrained sound speed in water can yield tighter constraints on source location than are possible from signals in the solid Earth alone (Dziak et al 2004). Other potential uses of hydroacoustic phases include early-warning systems for tsunamis (Sasorova et al (2005), ), acoustic thermometry for remote monitoring of long-term changes in ocean temperature (Dushaw et al 1999), detection of glacial and ice-calving events (Chapp et al 2005), as well as monitoring of cetacean populations (e.g. McDonald et al (1995), Dréo et al (2019)) and for illicit nuclear tests in violation of the Comprehensive Nuclear Test Ban Treaty (Mitchell (2002), Okal (2008)).…”
Section: Introductionmentioning
confidence: 99%
“…Additionally, as t-phases experience a reduced degree of geometric spreading (cylindrical, ∼ 1 r , rather than spherical, ∼ 1 r 2 ), they may offer greater sensitivity to more distant or smaller seismic events than would be obtained from the corresponding P or S waves at the same epicentral distance; furthermore, the lower and better-constrained sound speed in water can yield tighter constraints on source location than are possible from signals in the solid Earth alone (Dziak et al 2004). Other potential uses of hydroacoustic phases include early-warning systems for tsunamis (Sasorova et al (2005), ), acoustic thermometry for remote monitoring of long-term changes in ocean temperature (Dushaw et al 1999), detection of glacial and ice-calving events (Chapp et al 2005), as well as monitoring of cetacean populations (e.g. McDonald et al (1995), Dréo et al (2019)) and for illicit nuclear tests in violation of the Comprehensive Nuclear Test Ban Treaty (Mitchell (2002), Okal (2008)).…”
Section: Introductionmentioning
confidence: 99%