ライフサイエンスコーパス: tsunami

1 g rupture that contributed to the subsequent tsunami.

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 of the 2011 Great East Japan Earthquake and Tsunami.

8 ific following the March 2011 earthquake and tsunami.

9 e Fukushima power plant after the March 2011 tsunami.

10 to the 2011 Great East Japan Earthquake and Tsunami.

11 in the Peruvian subduction zone create large tsunamis.

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

13 tant factor in the generation of destructive tsunamis.

14 rvations for early warnings of MCS-generated tsunamis.

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

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

17 ng Simbo fault, potentially amplifying local tsunami amplitude.

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

19 Tsunami and geodetic observations indicate that addition

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

36 Tsunamis caused by slope failures with terminal landslid

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

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

39 0 year stratigraphic sequence of prehistoric tsunami deposits from a coastal cave in Aceh, Indonesia.

40 are paramount to saving lives and minimizing tsunami destruction.

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

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

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

44 bined with satellite imagery to quantify the tsunami effects.

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

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

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

48 limatic regime that occurred after the older tsunami event.

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

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

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

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

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

54 Giant tsunamis, generated by submarine landslides in the Hawai

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

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

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

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

59 exhibited contrasting earthquake rupture and tsunami generation.

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

61 geneous slip distributions for probabilistic tsunami hazard analysis.

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

63 attern and broadly expanding the seismic and tsunami hazard.

64 How can they be efficiently modelled for tsunami hazard?

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

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

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

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

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

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

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

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

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

74 11 Great East Japan Earthquake and resulting tsunami, including how unsustainable urban development e

75 Website following the 2011 tsunami-initiated catastrophe.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

92 curate forecasts of earthquake magnitude and tsunami potential.

93 The tsunamis produced widespread littoral landforms, includi

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

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

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

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

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

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

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

101 nch than expected, increasing earthquake and tsunami size.

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

103 exposure of coastal Sumatran communities to tsunami surges.

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

105 11 East Japan earthquake generated a massive tsunami that launched an extraordinary transoceanic biol

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

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

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

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

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

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

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

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

114 The 2004 tsunami was, independently of previous psychiatric morbi

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

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

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

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

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

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

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

122 0 tonnes, was produced by a 12- to 13-m-high tsunami with a period in the order of 1 h.

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