ライフサイエンスコーパス: tsunami

1 icanes), and geophysical (volcanic activity, tsunamis).

2 ion of central Chile triggered a destructive tsunami.

3 es as large as that of the 2004 Indian Ocean tsunami.

4 low slip greatly contributing to the ensuing tsunami.

5 epicenter 7 months before the earthquake and tsunami.

6 , mainly during the first 3 months after the tsunami.

7 ific following the March 2011 earthquake and tsunami.

8 e Fukushima power plant after the March 2011 tsunami.

9 g rupture that contributed to the subsequent tsunami.

10 and Yamada) that were heavily damaged by the tsunami.

11 ced the 2011 Great East Japan Earthquake and Tsunami.

12 the Earth several times, leading to a global tsunami.

13 ern for a worst-case scenario distant-source tsunami.

14 o Dickson Fjord, triggering a 200-meter-high tsunami.

15 ant tsunami events including the 2011 Tohoku Tsunami.

16 its capability to visualize ocean tides and tsunami.

17 sunami and the 1960 Great Chilean Earthquake Tsunami.

18 of the 2011 Great East Japan earthquake and tsunami.

19 Prefecture) was directly in the line of the tsunami.

20 lects back towards high latitudes, causing a tsunami.

21 e aftermath of the 2011 Japan Earthquake and Tsunami.

22 of the 2011 Great East Japan Earthquake and Tsunami.

23 to the 2011 Great East Japan Earthquake and Tsunami.

24 yn-eruptively, then it cannot have generated tsunamis.

25 tant factor in the generation of destructive tsunamis.

26 rvations for early warnings of MCS-generated tsunamis.

27 in the Peruvian subduction zone create large tsunamis.

28 coupling likely contributed to fast-arriving tsunamis.

29 ncluding the impact of giant earthquakes and tsunamis.

30 crustal depths can lead to the generation of tsunamis.

31 failure, potentially leading to destructive tsunamis.

32 tics of meteotsunamis are similar to seismic tsunamis.

33 seismic vibrations and/or the generation of tsunamis.

34 sting a currently neglected source of global tsunamis.

35 s potential source for great earthquakes and tsunamis.

36 onment, most notably leading to catastrophic tsunamis.

37 But do they represent storms or tsunami?

38 the risks associated with strong shaking and tsunamis(1).

39 uake and quickly followed by the devastating Tsunami, a damageable amount of radionuclides had disper

40 In response to the 26 December 2004 tsunami, a survey team of scientists was dispatched to S

41 and inferred from historical earthquake and tsunami accounts.

42 Data are drawn from the Study of the Tsunami Aftermath and Recovery, a population-representat

43 ng Simbo fault, potentially amplifying local tsunami amplitude.

44 The 1787 earthquake, and tsunami and a probable predecessor in 1537, suggest a pl

45 ants, 33 (3.8%) died directly because of the tsunami and an additional 95 people died during the 38-m

46 ption in January 2022 generated catastrophic tsunami and contends for the largest natural explosion i

47 Tsunami and geodetic observations indicate that addition

48 ed with sedimentation by an impact-generated tsunami and in Western Australia is represented by a maj

49 hquake of March 2011 was followed by a major tsunami and nuclear incident.

50 state of understanding of volcanic explosion tsunami and provides a framework for assessment of futur

51 merican Samoa, namely the 2009 South Pacific Tsunami and the 1960 Great Chilean Earthquake Tsunami.

52 A direct correlation between the tsunami and the acoustic-gravity waves' arrival times co

53 s of infections have recently occurred after tsunamis and earthquakes in Indonesia, Kashmir, and Hait

54 to natural variability (such as earthquakes, tsunamis and hurricanes) and climate change (such as flo

55 and to contrast and compare the deposits of tsunamis and storms.

56 Such flank failure can result in devastating tsunamis and threaten not only the immediate vicinity, b

57 patterns, storm events and possibly 'normal' tsunamis, and reached their present height by uplift of

58 Such tsunamis are a major hazard, but forward models of their

59 eing widespread and frequent, these internal tsunamis are at least comparable to winds, and much more

60 is where the world's largest, most damaging tsunamis are generated.

61 Tsunamis are rare, extreme events and cause significant

62 Overall, meteorological tsunamis are revealed as a new generation mechanism of r

63 Among potential source areas for such tsunamis are submarine landslides and margin collapses o

64 While tsunamis are thought to use less than 15% of the total e

65 We initialize the tsunami as an N wave that propagates to shore and impact

66 y fast travel times and long duration of the tsunami, as well as its global reach, are consistent wit

67 ucation: Residents with a basic knowledge of tsunamis, as well as an understanding of how environment

68 opose an improved depositional mechanism for tsunami backflow based on hyperpycnal currents.

69 iterion to the proxy toolkit for identifying tsunami backwash deposits, namely the basal soft sedimen

70 t the representability of this criterion for tsunami backwash deposits.

71 nd there is no immediate danger of a similar tsunami being generated on this part of the plate bounda

72 afforestation efforts under the Billion Tree Tsunami (BTT) project.

73 ndian Ocean basin has identified prehistoric tsunamis, but the timing and recurrence intervals of suc

74 rming eruptions of island volcanoes generate tsunamis by the interaction of different eruptive phenom

75 It is well known that tsunamis can produce gravity waves that propagate up to

76 Tsunamis can propagate thousands of kilometres across th

77 er potential for the reconstruction of paleo-tsunami catalogs and should be preferentially investigat

78 The devastating 2004 Indian Ocean tsunami caught millions of coastal residents and the sci

79 The tsunami caused at least 437 fatalities, the greatest num

80 Tsunamis caused by slope failures with terminal landslid

81 o debris flows, slumps, slides, and possible tsunamis) caused by gas-hydrate dissociation are of imme

82 ight points and ephemeral regions, until the tsunami causes the birth of new cycle's spots.

83 d rheologies successfully reproduce observed tsunami characteristics from post-event field survey res

84 ion present a major challenge for mitigating tsunami coastal impact.

85 Our models of historical and future tsunamis confirm a substantial exposure of coastal Sumat

86 human and dog skeleton discovered within the tsunami debris are in situ victims related to the Late B

87 Prior modeling of the 1957 tsunami deposit and runup records on eastern Aleutian an

88 rained, short-lived organics from within the tsunami deposit constrain the event to no earlier than 1

89 The youngest tsunami deposit is associated with the 1787 great earthq

90 Minoura et al., Geology 28, 59-62], few tsunami deposits are reported.

91 Many are interpreted as tsunami deposits based simply on clast size and inferenc

92 Two sandy tsunami deposits extend over 1.5 km inland of the coast.

93 0 year stratigraphic sequence of prehistoric tsunami deposits from a coastal cave in Aceh, Indonesia.

94 the age of one of the sand sheets below the tsunami deposits of the great Cascadia earthquake in 170

95 covery of three unprecedented well-preserved tsunami deposits related to repeated flank collapses of

96 Examination of tsunami deposits was used to constrain run-up not exceed

97 are paramount to saving lives and minimizing tsunami destruction.

98 tion hubs and planned deployment of a global tsunami detection network.

99 sorders, and, for children, for parental pre-tsunami disorders.

100 We prove that the common believe that great tsunamis do not occur on the Mexican Pacific coast canno

101 Ice Sheet; or second, emplacement by a mega-tsunami during MIS 11 (ref. 4, 5).

102 r a strengthening of the existing Indonesian Tsunami Early Warning System (InaTEWS), especially in Ja

103 e, and can be immediately transformative for tsunami early warning.

104 he spectrum of fault slip including SSEs and tsunami earthquakes.

105 bined with satellite imagery to quantify the tsunami effects.

106 Measurements made by the team show that the tsunami elevation and runup ranged from 5 to 12 meters.

107 fied a loss-of-function mutation, designated tsunami, encoding a homolog of the Fused kinase.

108 is iceberg calving, which can generate large tsunamis endangering human beings and coastal infrastruc

109 t existing empirical equations for landslide-tsunamis establish estimates of an upper envelope of the

110 in Hawaii as induced by the 2012 Haida Gwaii tsunami event.

111 limatic regime that occurred after the older tsunami event.

112 nt magnetic signals generated by a few giant tsunami events including the 2011 Tohoku Tsunami.

113 analyses, we show evidence for two enormous tsunami events possibly triggered by bolide impacts, res

114 considered insufficient for triggering large tsunamis, except through the generation of submarine lan

115 Strong tsunami excitation from slow rupture of shallow subducti

116 of fault slip, ground motion, and associated tsunami excitation.

117 disaster provide detailed information about tsunami exposures and self-reported symptoms of post-tra

118 After the 26 December 2004 earthquake and tsunami, field data on the extent of the inundation in B

119 acted as a low-velocity wave trap, capturing tsunami for more than 1 hour.

120 But this would prevent tsunami formation, for which there is some evidence.

121 and thus we have the first observations of a tsunami from a large emergent volcanic eruption captured

122 Hair samples collected 14 y after the tsunami from a sample of adult participants provide meas

123 fault of the 2011 Tohoku-Oki earthquake and tsunami from boreholes drilled by the Integrated Ocean D

124 ed to establish whether Swedish survivors of tsunamis from the 2004 Sumatra-Andaman earthquake had in

125 h patient register for the 5 years after the tsunami (from Dec 26, 2004, to Jan 31, 2010) and estimat

126 of the 2011 Great East Japan Earthquake and Tsunami (GEJE), we examined the association between chan

127 d at Anak Krakatau on December 22(nd), 2018, tsunamis generated by volcanic flank collapse are incomp

128 Giant tsunamis, generated by submarine landslides in the Hawai

129 Here we report that the tsunami-generated magnetic fields consist of the weak bu

130 th separation and sorting more difficult for tsunami-generated waste as opposed to earthquake-generat

131 In Japan, earthquake and tsunami-generated waste were found to have elevated leve

132 marine slope failures are a likely cause for tsunami generation along the East Coast of the United St

133 e earthquakes has important implications for tsunami generation and for the rheological behavior of t

134 22-0.30 km(3), which is used to initialize a tsunami generation and propagation model with two differ

135 the role of air-water-coupling processes in tsunami generation and propagation.

136 tion zone faults is a primary contributor to tsunami generation by earthquakes.

137 exhibited contrasting earthquake rupture and tsunami generation.

138 w and shallow bays, are prime candidates for tsunami generation.

139 me data stream in future warning systems and tsunami genesis estimation observing both, ground motion

140 erspectives to real-time warning systems for tsunami genesis estimation.

141 es can contribute to the generation of large tsunamis (>1 m), under rather generic conditions.

142 However, the source mechanisms behind the tsunami have been disputed due to difficulties in sampli

143 A recent earthquake and the subsequent tsunami have extensively damaged the Fukushima nuclear p

144 environments in areas repeatedly impacted by tsunamis have a higher potential for the reconstruction

145 nd sediment records of large earthquakes and tsunamis have expanded the temporal data and estimated s

146 Such iceberg-tsunamis have reached amplitudes of 50 m and destroyed h

147 evidence suggest that great earthquakes and tsunamis have whipped the Pacific coast of Mexico in the

148 opportunity for sedimentary archives of past tsunamis, have mostly been omitted.

149 presumed to be a major source of seismic and tsunami hazard along the Mexican subduction zone.

150 geneous slip distributions for probabilistic tsunami hazard analysis.

151 ne faults is recognized as a key concern for tsunami hazard assessment.

152 ent properties influence earthquake rupture, tsunami hazard, and prism development at subducting plat

153 attern and broadly expanding the seismic and tsunami hazard.

154 How can they be efficiently modelled for tsunami hazard?

155 ent numerical models can accurately forecast tsunami hazards from these events.

156 importance of understanding the seismic and tsunami hazards of subduction zones.

157 r-shore slip velocities, and the seismic and tsunami hazards posed by LANF earthquakes.

158 ng variations in population vulnerability to tsunami hazards that integrates (i) geospatial approache

159 tury will influence future maximum nearshore tsunami heights (MNTH) at the Ports of Los Angeles and L

160 ning Java rupture simultaneously, shows that tsunami heights can reach ~ 20 m and ~ 12 m on the south

161 ge-scale laboratory experiments that iceberg-tsunami heights from gravity-dominated mechanisms (B and

162 of an upper envelope of the maximum iceberg-tsunami heights, they fail to capture the physics of mos

163 along the coast of Aceh, Indonesia, when the tsunami hit.

164 vel C-terminal domain that we designated the Tsunami Homology (TH) domain.

165 duction earthquakes produce relatively small tsunamis, however historical records and now geologic ev

166 multibeam bathymetric data, reveal possible tsunami impact on Bimini, the Florida Keys, and northern

167 erthrusting earthquakes produced destructive tsunamis impacting Hawai'i in 1946 and 1957.

168 In the near field, tsunami impacts are strongly controlled by the water-cav

169 A tsunami in 1996, 200 km north of our site, was interpret

170 ore the 2011 Great East Japan Earthquake and Tsunami in a survey of older community-dwelling adults w

171 tly before and after the 2011 earthquake and tsunami in Japan.

172 eactor in Japan following the earthquake and tsunami in March 2011 were found in resident marine anim

173 lower risk of PTSD after the earthquake and tsunami in Tohoku, Japan, on March 11, 2011.

174 Simulating tsunamis in a laboratory setting is important to further

175 ch formed after two landslide-generated mega-tsunamis in an East Greenland fjord.

176 females who were living, at the time of the tsunami, in communities directly damaged by the tsunami,

177 nami, in communities directly damaged by the tsunami, in comparison with similar females living in ot

178 11 Great East Japan Earthquake and resulting tsunami, including how unsustainable urban development e

179 ymptoms persistently for two years after the tsunami, indicating that the negative effects of exposur

180 ining megagravel, cannot be used as de facto tsunami indicators.

181 subjected to tsunami neglect the effects of tsunami-induced vertical loads due to internal buoyancy.

182 Website following the 2011 tsunami-initiated catastrophe.

183 ogether with the short travel time following tsunami initiation present a major challenge for mitigat

184 berg detachment, which in turn excites local tsunamis, internal gravity waves and transient currents

185 led prehistoric Aleutian earthquakes produce tsunami inundation in Hawai'i with the most severe, 14(t

186 rther understand soil instability induced by tsunami inundation processes.

187 The 26(th) December 2004 Indian Ocean Tsunami (IOT) emanated from an Mw 9.2 earthquake that ge

188 The next tsunami is due by 2020, portending the start of intense

189 This tsunami is excited at the equator when magnetic dams, cr

190 unga Tonga-Hunga Ha'apai volcano and ensuing tsunami is the first global volcano-triggered tsunami re

191 The average time period between tsunamis is about 450 years with intervals ranging from

192 racteristics and behavior similar to seismic tsunamis, is poorly understood.

193 ocean floor overestimate the phase speed of tsunamis, leading to arrival time differences exceeding

194 Meteorological-tsunami-like (or meteotsunami-like) periodic oscillation

195 Here, we present evidence that these tsunami-like events were generated by atmospheric mesosc

196 ally designed for exploring the physics of a tsunami-like flow on a soil bed is used to perform exper

197 uge, we are now able to simulate and measure tsunami-like loading with sufficiently high water pressu

198 rium complex, is a contributing aetiology to tsunami lung and central nervous system infections in ne

199 region, with the concomitant risk of another tsunami, makes the need for a tsunami warning system in

200 warning interval between the earthquake and tsunami, many coastal residents lost their lives.

201 fail to capture the physics of most iceberg-tsunami mechanisms.

202 his kind of hybrid approach is the so-called tsunami mitigation park, which combines a designed hills

203 The protective benefit of tsunami mitigation parks is thus comparable to that of a

204 Despite the increasing popularity of tsunami mitigation parks, the protective benefits they p

205 ight not maximize the protective benefits of tsunami mitigation parks.

206 real-time tsunami MOST (Method of Splitting Tsunami) model produced by the NOAA Center for Tsunami R

207 Earthquake and tsunami modeling combined with local probabilistic RSLR

208 To assess the expected inundation hazard, tsunami modeling was conducted based on several scenario

209 y, we present comparisons with the real-time tsunami MOST (Method of Splitting Tsunami) model produce

210 Following recent tsunamis, most studies have focused on the onshore depos

211 by the 2011 Great East Japan Earthquake and Tsunami (n = 4,857).

212 uakes (n = 868) affected most species, while tsunamis (n = 272), and volcanoes (n = 171) affected con

213 For particularly destructive hazards like tsunamis, natural elements like vegetation are often com

214 present the first geologic evidence of great tsunamis near the trench of a subduction zone previously

215 ing the fragility of structures subjected to tsunami neglect the effects of tsunami-induced vertical

216 detailed analysis of seismic, geodetic, and tsunami observations of the aftershock that the event im

217 les into continuous real-time earthquake and tsunami observatories.

218 el physical mechanism, namely, that a "solar tsunami" occurring in the Sun's interior shear-fluid lay

219 The great Sumatra-Andaman earthquake and tsunami of 2004 was a dramatic reminder of the importanc

220 ically and soon to stave off the approaching tsunami of AD.

221 The Tohoku earthquake and tsunami of March 11, 2011, resulted in unprecedented rad

222 ivation-induced deaminase, which unleashes a tsunami of mutations in the immunoglobulin loci.

223 Nuclear Plant, damaged by an earthquake and tsunami on March 11, 2011 released large amounts of (131

224 uclear plants affected by the earthquake and tsunami on March 11, 2011 shows that three variables wer

225 We conclude that, on early Mars, tsunamis played a major role in generating and resurfaci

226 curate forecasts of earthquake magnitude and tsunami potential.

227 Dynein water waves resembling tsunami produce nearly optimal energy transport over 1,5

228 The tsunamis produced widespread littoral landforms, includi

229 s a novel tool for the prediction of extreme tsunami-producing near-trench slip.

230 c accumulations, were the main mechanisms of tsunami production.

231 This tsunami propagates poleward at a speed of ~300 m/s until

232 Our computations of tsunami propagation and inundation yield model flow dept

233 nt of the geomagnetic main field parallel to tsunami propagation direction.

234 d hazard ratios (HRs), then adjusted for pre-tsunami psychiatric disorders, and, for children, for pa

235 sunami is the first global volcano-triggered tsunami recorded by modern, worldwide dense instrumentat

236 nformation dissemination for earthquakes and tsunamis require a rapid characterisation of the fault p

237 unami) model produced by the NOAA Center for Tsunami Research and we observe variations in TEC that c

238 he Minoan town of Malia (Crete) shows that a tsunami resulting from the Bronze Age Santorini eruption

239 A tsunami results when an earthquake on the ocean floor cr

240 Improving earthquake and tsunami risk assessment requires understanding the mater

241 ose an unknown submarine landslide-generated tsunami risk to Southern Hemisphere populations and infr

242 ays all of the physical characteristics of a tsunami runup, the timing (<1 hour postimpact) is instea

243 y record of the backwash from two historical tsunamis sampled in a sheltered bay in American Samoa, n

244 ts were identified and compared to the known tsunami sandsheets.

245 lobes formed in association with the younger tsunami, showing that their emplacement took place follo

246 Numerical tsunami simulations indicate that only the combination o

247 greatest number from a volcanically-induced tsunami since the catastrophic explosive eruption of Kra

248 nch than expected, increasing earthquake and tsunami size.

249 nals, and are an efficient and unpredictable tsunami source.

250 Simulations show that the tsunami stabilized into a 7-meter-high long-duration sei

251 rd demonstrates that at least 11 prehistoric tsunamis struck the Aceh coast between 7,400 and 2,900 y

252 exposure of coastal Sumatran communities to tsunami surges.

253 ulation-representative longitudinal study of tsunami survivors who were living along the coast of Ace

254 The first event generated a tsunami that caused more than 283,000 deaths.

255 nity to study a major volcanically-generated tsunami that caused widespread loss of life and signific

256 11 East Japan earthquake generated a massive tsunami that launched an extraordinary transoceanic biol

257 This contributed to the destructive tsunami that occurred during the Tohoku-Oki event and to

258 The earthquake and the subsequent tsunami that occurred offshore of Japan resulted in an i

259 7 great earthquake, M 8.6, producing a giant tsunami that poured over the coast flooding 500 km along

260 verely damaged by the earthquake and ensuing tsunami that struck off the northern coast of the island

261 eological site was hit by a series of strong tsunamis that caused damage and erosion, leaving behind

262 orld are threatened by local (or near-field) tsunamis that could inundate low-lying areas in a matter

263 nitude earthquakes to produce distant-source tsunamis that exceed historically observed MNTH.

264 atra-Andaman earthquake in Indonesia and its tsunami, the possibility of a triggered earthquake on th

265 trate that glacier calving triggers internal tsunamis, the breaking of which drives vigorous mixing.

266 tween a single row of hills with an incoming tsunami to identify the mechanisms through which the par

267 k the oldest, highest-magnitude investigated tsunami to the following rapid abandonment of the island

268 some likely originating from the 2011 Tohoku tsunami, to examine the relationship between rafting com

269 find perturbation periods consistent with a tsunami typical deep ocean period.

270 on of coastal hazards such as distant-source tsunamis under future relative sea-level rise (RSLR) is

271 The sediment marks of centuries old-tsunamis validate historical records and indicate that l

272 isk of another tsunami, makes the need for a tsunami warning system in the Indian Ocean all the more

273 analytical models, to demonstrate that this tsunami was driven by a constantly moving source in whic

274 The 2004 tsunami was, independently of previous psychiatric morbi

275 obability of exceedance of maximum estimated tsunami wave heights along the Japanese coast.

276 er, in general, the slip models derived from tsunami wave modeling and seismological data are poorly

277 00-m asteroid, resulting in a train of large tsunami waves and the potential release of substantial q

278 he first direct observation of both internal tsunami waves and turbidity current reflection.

279 n Washington that are directly threatened by tsunami waves associated with a Cascadia subduction zone

280 tially attributed to the arrival of multiple tsunami waves generated by a major landslide in Strombol

281 Modeling of tsunami waves generated by subaerial landslides is impor

282 for the aftershock, it generated much larger tsunami waves than the mainshock.

283 along the Sumatran Megathrust and generated tsunami waves up to 30 m high.

284 The collective faulting produced tsunami waves with localized regions of about 12 metres

285 ing land, along with driven and conventional tsunami waves.

286 upon impact with the brine pool, similar to tsunami waves.

287 EC that correlate in time and space with the tsunami waves.

288 ajor natural disaster, the 2004 Indian Ocean tsunami, we provide causal evidence of its imprint on ha

289 ing the 2011 Great East Japan Earthquake and Tsunami were compared.

290 ion patterns of the 26 December 2004 Sumatra tsunami were primarily determined by the orientation and

291 than a more piecemeal process, generating a tsunami which reached nearby coastlines within ~30 minut

292 lian Lombardy region was hit by an "epidemic tsunami" which was, at that point in time, one of the wo

293 e interval between impact and arrival of the tsunami, which on the basis of seismic velocities and hi

294 he water-cavity source whereas the far-field tsunami, which was unusually persistent, can be largely

295 isasters such as hurricanes, oil spills, and tsunamis, which may lead to increased populations of har

296 erous geological phenomena, able to generate tsunamis whose effects can propagate far from the source

297 0 tonnes, was produced by a 12- to 13-m-high tsunami with a period in the order of 1 h.

298 southwest of the volcano, which generated a tsunami with runups of up to 13 m on the adjacent coasts

299 arable to that of a small wall, at least for tsunamis with amplitudes that are comparable to the hill

300 Observations of a single tsunami, with no subsequent waves, are consistent with o

301 ere, we present numerical simulations of the tsunami, with state-of the-art numerical models, based o

302 mant period of over 2,000 years, to multiple tsunamis within the span of a century.