ライフサイエンスコーパス: volcanic eruption

1 environmental impact of the Thera/Santorini volcanic eruption.

2 e spark flask, simulating a water vapor-rich volcanic eruption.

3 no event occurring in the winter following a volcanic eruption.

4 in reproducing the observed drying after the volcanic eruption.

5 ciated with the recovery from the El Chichon volcanic eruption.

6 tions in subjects and populations exposed to volcanic eruptions.

7 ceed impacts caused by historic droughts and volcanic eruptions.

8 than constant, even in the absence of major volcanic eruptions.

9 ne concentrations, as is evident from recent volcanic eruptions.

10 riggering and mitigating the consequences of volcanic eruptions.

11 trumentation and by including the effects of volcanic eruptions.

12 polymer foams, in glass furnaces, and during volcanic eruptions.

13 sing their potential for future catastrophic volcanic eruptions.

14 n the region's potential for producing major volcanic eruptions.

15 EASM rainfall in response to strong tropical volcanic eruptions.

16 phes from nuclear winter and large magnitude volcanic eruptions.

17 thunderstorms and lightning associated with volcanic eruptions.

18 zation of regional climate impacts following volcanic eruptions.

19 cale to centennial-scale climate response to volcanic eruptions.

20 d crustal recycling or melting and producing volcanic eruptions.

21 n and natural events including wildfires and volcanic eruptions.

22 sions and climate impacts of large explosive volcanic eruptions.

23 s likely produced in only trivial amounts by volcanic eruptions.

24 ce that are forced by orbital variations and volcanic eruptions.

25 s due to sulfate aerosol formation following volcanic eruptions.

26 the recorded signal is indeed influenced by volcanic eruptions.

27 ncrease in cirrus occurrences after ash-rich volcanic eruptions.

28 s fundamental to controlling the dynamics of volcanic eruptions.

29 tiple closely spaced observed and unobserved volcanic eruptions.

30 se red clays indicate a hiatus in successive volcanic eruptions.

31 ent from that of previous well-studied large volcanic eruptions.

32 t of an El Nino by about 98% following major volcanic eruptions.

33 tial flood disasters resulting from tropical volcanic eruptions.

34 racterizing the hydroclimate risks of future volcanic eruptions.

35 (VA) are one of the by-products of explosive volcanic eruptions.

36 for investigating the dynamics and timing of volcanic eruptions.

37 ), which has impacts analogous to those from volcanic eruptions.

38 accumulation in the upper crust before many volcanic eruptions.

39 ttrition is likely to occur in all explosive volcanic eruptions.

40 deposition of ash sourced from high-latitude volcanic eruptions.

41 , reduced solar activity and strong tropical volcanic eruptions.

42 magma chamber dynamics and the triggers for volcanic eruptions.

43 arried out in the aftermath of invasions and volcanic eruptions.

44 ncies to characterize electrical activity in volcanic eruptions.

45 ds subsurface reservoirs that are drained by volcanic eruptions.

46 spheric SO2 emitted from biomass burning and volcanic eruptions.

47 gth and the effusive-explosive transition in volcanic eruptions.

48 w-density pumice clasts generated by silicic volcanic eruptions.

49 Precambrian atmosphere and to document past volcanic eruptions.

50 ing sulfur dioxide associated with the Nabro volcanic eruption (13 June 2011) from the upper troposph

51 After the Campanian Ignimbrite volcanic eruption (40,000 cal BP) and the beginning of H

52 f this finding is that barring another major volcanic eruption, a detectable acceleration is likely t

53 apparatus) that could represent a water-rich volcanic eruption accompanied by lightning.

54 Release of reduced gases in volcanic eruptions accompanied by lightning could have b

55 Explosive volcanic eruptions affect climate, but how climate chang

56 Large volcanic eruptions, although rare events, can influence

57 It was a hydro-volcanic eruption and new magmatic material was not dete

58 Tephra deposits result from explosive volcanic eruption and serve as indirect probes into frag

59 confirm that the combined effects of a major volcanic eruption and severe climatic cooling failed to

60 for example, explosive versus effusive) of a volcanic eruption and thus its hazard potential, but can

61 c transition have been attributed to massive volcanic eruption and/or severe climatic deterioration.

62 aerosols, stratospheric ozone depletion, and volcanic eruptions and a second suite of simulations for

63 rock record-can therefore shed light on past volcanic eruptions and atmospheric conditions.

64 omparison with approaches to criticality for volcanic eruptions and creep failure.

65 limate sensitivity involving the response to volcanic eruptions and Eocene climate change are also de

66 Here, using 145-year records of volcanic eruptions and ISMR, we show that ISMR deficits

67 orecast failure scenarios both in the field (volcanic eruptions and landslides) and in the laboratory

68 g gas-particle flows associated to explosive volcanic eruptions and moving down a volcano's slope, ca

69 placement of granite plutons, huge explosive volcanic eruptions and physical and chemical zoning of c

70 ressures and gas concentrations in explosive volcanic eruptions and provide estimates of eruption mag

71 atmospheric gravity oscillations induced by volcanic eruptions and recorded by pressure sensors can

72 We assess the main external forcings (i.e., volcanic eruptions and solar activity) on NAO variabilit

73 d a statistical connection between explosive volcanic eruptions and subsequent El Nino climate events

74 Understanding interactions between volcanic eruptions and the cryosphere (a.k.a. glaciovolc

75 evaluate the relationship between historical volcanic eruptions and the observed NAO response since t

76 summer cooling in the years following large volcanic eruptions, and exhibits strong warming since th

77 Ground deformation often precedes volcanic eruptions, and results from complex interaction

78 hydrocarbon reserves, magma build-up before volcanic eruptions, and subterranean tunnels.

79 eismicity are well-established precursors to volcanic eruptions, and their interpretation forms the b

80 The impacts of large terrestrial volcanic eruptions are apparent from satellite monitorin

81 Explosive volcanic eruptions are driven by exsolution of H2O-rich

82 Volcanic eruptions are episodic despite being supplied b

83 Most of Earth's volcanic eruptions are hidden beneath the ocean in compl

84 Magmatic intrusions and volcanic eruptions are intimately related phenomena.

85 In addition, the NH volcanic eruptions are more efficient in reducing the NH

86 scales involved in the generation of silicic volcanic eruptions are much longer than originally thoug

87 Large-scale, explosive volcanic eruptions are one of the Earth's most hazardous

88 the Cretaceous, the massive Deccan trap (DT) volcanic eruptions are regarded as the primary driver of

89 Volcanic eruptions are shallow phenomena that represent

90 Terrestrial volcanic eruptions are the consequence of magmas ascendi

91 Explosive volcanic eruptions are the largest non-anthropogenic per

92 Volcanic eruptions are thought to be a key driver of rap

93 Vanguard efforts in forecasting volcanic eruptions are turning to physics-based models,

94 Limitations in using major volcanic eruptions as a constraint on cloud feedbacks ar

95 Our revised timescale more firmly implicates volcanic eruptions as catalysts in the major sixth-centu

96 The volcanic eruption at La Palma started on September 19, 2

97 on the spatial and temporal distribution of volcanic eruptions at various sections of an ultraslow s

98 heric aerosols from large tropical explosive volcanic eruptions backscatter shortwave radiation and r

99 brupt changes in cirrus properties following volcanic eruptions based on satellite measurements.

100 It is difficult to predict hydro-volcanic eruptions because they are local phenomena that

101 l eruption models have provided insight into volcanic eruption behaviour, but most address plinian-ty

102 to the occurrence of several closely spaced volcanic eruptions between 1108 and 1110 CE.

103 sponse.El Nino tends to follow 2 years after volcanic eruptions, but the physical mechanism behind th

104 usion in Earth's crust can lead to hazardous volcanic eruptions, but the physical processes involved

105 t affect eruptive behavior occur during many volcanic eruptions, but typical analytical techniques ar

106 essing of mantle melts and the triggering of volcanic eruptions by supply of magma from greater depth

107 noes, thus improving our ability to forecast volcanic eruptions by using petrology.

108 quently precede large explosive and effusive volcanic eruptions-by as much as weeks to months in the

109 Volcanic eruptions can affect global climate through cha

110 Large tropical volcanic eruptions can affect the climate of many region

111 Early warning systems, activated after volcanic eruptions can alleviate the impacts on aviation

112 Large volcanic eruptions can have major impacts on global clim

113 Volcanic eruptions can impact the mass balance of ice sh

114 Volcanic eruptions can induce peaks in hurricane activit

115 Explosive volcanic eruptions can loft ash, gases, and water into t

116 dence has been accumulating for decades that volcanic eruptions can perturb climate and possibly affe

117 Large volcanic eruptions can remodel the seafloor landscape, d

118 Volcanic eruptions can trigger tsunamis, which may cause

119 ervations of a tsunami from a large emergent volcanic eruption captured with modern instrumentation.

120 Likewise, major volcanic eruptions cause a multiyear period of westward

121 Magma from Plinian volcanic eruptions contains an extraordinarily large num

122 Volcanic eruptions contribute to climate variability, bu

123 limate response to large volcanic eruptions: Volcanic eruptions cool the surface, thus masking the re

124 This suggests that future volcanic eruptions could substantially affect global wat

125 being trapped within olivine crystals before volcanic eruption, did not experience posteruptive degas

126 ere, we use observations to demonstrate that volcanic eruptions disrupt ENSO teleconnections with lan

127 Finally, our analysis suggests that volcanic eruptions do not lead to an overall global redu

128 1477) claimed that large volcanic eruptions do not produce a detectable El Nino r

129 whose onset coincides with clusters of large volcanic eruptions during the nineteenth and twentieth c

130 diverse impacts of one of the most explosive volcanic eruptions ever recorded.

131 , approximately 192-y series of halogen-rich volcanic eruptions exactly at the start of accelerated d

132 Volcanic eruptions exert a considerable influence on glo

133 mplex systems such as the Earth's climate to volcanic eruptions, extreme events or geoengineering.

134 cently suggested that a succession of strong volcanic eruptions forced an abrupt onset of the Little

135 y been developed based on the Holuhraun-2014 volcanic eruption from machine learning with satellite o

136 Future work is needed to confirm that a volcanic eruption from Mt.

137 has been attributed in previous studies to a volcanic eruption from the submarine Kuwae caldera in Va

138 Large explosive volcanic eruptions from island volcanoes deliver vast qu

139 Explosive volcanic eruptions generate pressure disturbances in the

140 ng a close temporal link between large-scale volcanic eruptions, global carbon and mercury cycle pert

141 Superposed epoch analysis indicates that volcanic eruptions had significantly impacted southeaste

142 nt of volcanic ash produced during explosive volcanic eruptions has been found to sediment as aggrega

143 nding physical processes prior to and during volcanic eruptions has improved significantly in recent

144 Our understanding of submarine volcanic eruptions has improved substantially in the pas

145 Large volcanic eruptions have been linked with reductions in I

146 Volcanic eruptions have episodically interfered with hea

147 ale, we showed that over the last 110 years, volcanic eruptions have influenced ASM variations on an

148 rast to the hydrological weakening theory of volcanic eruptions, here we present convergent empirical

149 istorical records evidence a large-magnitude volcanic eruption in 1831 CE.

150 The Hunga Tonga-Hunga Ha'apai (HTHH) volcanic eruption in January 2022 generated catastrophic

151 ption before that at Chaiten was the largest volcanic eruption in the twentieth century, at Novarupta

152 he world which cover between two and 6 major volcanic eruptions in the 20(th) and late 19(th) century

153 However, identification of stratospheric volcanic eruptions in the geological record and their ca

154 Netherlands and then by using the number of volcanic eruptions in the world.

155 Many volcanic eruptions, including some of the largest, resul

156 Observations following major volcanic eruptions indicate that aerosol enhancements co

157 t of aeolian dust and of ash from occasional volcanic eruptions, indicating that metallurgic producti

158 ere and provides observational evidence of a volcanic eruption injecting material through the stratos

159 if unavoidable natural events such as major volcanic eruptions interact with anthropogenic warming u

160 Similar to aerosol enhancements produced by volcanic eruptions, introducing particles into the strat

161 When volcanic eruptions involve interaction with external wat

162 Tsunami generation during volcanic eruptions is complex and often due to a combina

163 and the formation of elongated structures in volcanic eruptions known as Pele's hair.

164 fore material failure and broadly applied to volcanic eruptions, landslides and other phenomena.

165 been proposed that a decreasing pressure of volcanic eruptions led to the oxygenation of the atmosph

166 sults suggest that warming induced by future volcanic eruptions may further enhance the vulnerability

167 illion years ago suggests that stratospheric volcanic eruptions may have contributed to synergetic en

168 pan-tropical surface cooling caused by large volcanic eruptions may mask El Nino warming at our centr

169 arming, external forcing driven by explosive volcanic eruptions may still cause abrupt cooling.

170 cloudiness) and natural disturbances (e.g., volcanic eruptions) may induce transient reductions in t

171 In this emerging risk landscape, moderate volcanic eruptions might have cascading, catastrophic ef

172 Classical mechanisms of volcanic eruptions mostly involve pressure buildup and m

173 agma bodies plays an important role in where volcanic eruptions occur, but detailed field observation

174 thquakes (magnitudes greater than 3.9) and a volcanic eruption occurred within the approximately 60-k

175 During the sampling campaign, a number of volcanic eruptions occurred in the southern hemisphere f

176 em Model to investigate the impact of strong volcanic eruptions occurring in the tropical Northern (N

177 nts follow in the two springs after the 1991 volcanic eruption of Mt.Pinatubo.

178 ians have previously speculated that a large volcanic eruption of unknown origin was the most likely

179 Suggestions have ranged from volcanic eruptions of liquid water or solid ice to tecto

180 magnitude to Pinatubo and Agung, the largest volcanic eruptions of the 20th century.

181 al Pacific to gauge ENSO's response to large volcanic eruptions of the last millennium.

182 ycles were excited following five Agung-like volcanic eruptions of the last millennium.

183 six Arctic ice cores that one of the largest volcanic eruptions of the past 2,500 y occurred in early

184 lightning is commonly observed in explosive volcanic eruptions of Volcanic Explosivity Index (VEI) >

185 Ptolemaic vulnerability to volcanic eruptions offers a caution for all monsoon-depe

186 understanding of the effect of this unusual volcanic eruption on stratospheric chemistry and provide

187 Large volcanic eruptions on Earth commonly occur with a collap

188 neous province preserves some of the largest volcanic eruptions on Earth, with six units totaling >8,

189 The Hunga Tonga-Hunga Ha'apai (HT-HH) volcanic eruptions on January 13 and 15, 2022, produced

190 Volcanic eruptions on land create hot and fast pyroclast

191 We isolate the impact of volcanic eruptions on multiyear-to-decadal climate predi

192 ity to explore the early impacts of tropical volcanic eruptions on stratospheric composition.

193 The effect of the volcanic eruptions on the ITCZ and hence on TC activity

194 ice cores and can be strongly influenced by volcanic eruptions or anthropogenic emissions.

195 Natural drivers such as large explosive volcanic eruptions or multidecadal cycles in ocean circu

196 an 3sigma variability coinciding with either volcanic eruptions or possible wild fire activity.

197 Volcanic eruptions over the past 320 million years have

198 l hydroclimatic response to all the tropical volcanic eruptions over the past millennium that were la

199 ity across two distinct phenomena: explosive volcanic eruptions (P<0.01) and the recent epoch of glob

200 erved compared with that during the inactive volcanic eruption period (1936-1962).

201 During the active volcanic eruption periods (1901-1935 and 1963-1993), sig

202 We found that during active volcanic eruption periods, which correspond to a negativ

203 Silicic volcanic eruptions pose considerable hazards, yet the pr

204 Following large explosive volcanic eruptions precipitation decreases over much of

205 in order to remove the residual signal from volcanic eruptions present in the OMI data.

206 ly <50 s, providing insight into the overall volcanic eruption process.

207 Large volcanic eruptions produce sulfur dioxide, which in turn

208 Explosive volcanic eruptions produce vast quantities of silicate a

209 Volcanic eruptions provide tests of human and natural sy

210 ient perturbation of global climate by large volcanic eruptions provides a unique opportunity to retr

211 Seismic data recorded before volcanic eruptions provides important clues for forecast

212 rastic and sudden ozone reduction from major volcanic eruptions, regional nuclear conflicts, or long-

213 Volcanic eruptions release a large amount of sulphur dio

214 ietal importance, the volumes of large-scale volcanic eruptions remain poorly constrained.

215 High quality records of stratospheric volcanic eruptions, required to model past climate varia

216 Any future volcanic eruption(s) is a serious concern for scientists

217 famine (half of all disaster victims) and by volcanic eruptions show significant associations with th

218 elta(17)O anomaly of sulfate for the largest volcanic eruptions, showing a further change in atmosphe

219 Toba eruption ~74,000 y ago was the largest volcanic eruption since the start of the Pleistocene and

220 g increasingly recognised in the products of volcanic eruptions, spanning a range of magma compositio

221 Moreover, tropical volcanic eruptions strengthen El Nino and weaken La Nina

222 Transitions in eruptive style during volcanic eruptions strongly depend on how easily gas and

223 4)He ratio detectors aimed at earthquake and volcanic eruption studies, and monitoring of nuclear sit

224 th's mantle affects the dynamics of melting, volcanic eruption style and the evolution of Earth's atm

225 ern and western SPG further suggest that the volcanic eruption supplied (micro)nutrients potentially

226 on product (PHYDA), we find that these large volcanic eruptions tended to produce dry conditions over

227 Polar ice core records attest to a colossal volcanic eruption that took place ca. A.D. 1257 or 1258,

228 ithosphere developed as a result of frequent volcanic eruptions that advected surface materials downw

229 ocks represents times and regions of violent volcanic eruptions that ejected large volumes of sulphur

230 5,100 y BP) by sustained Icelandic volcanic eruptions that forced a centennial-scale 1.0 de

231 large debris flows were triggered following volcanic eruptions that produced several cubic kilometer

232 ands after the largest historically observed volcanic eruption: that of Mt Tambora in 1815.

233 o-Pacific warm pool dry more quickly after a volcanic eruption, the background moisture distribution

234 after moderate and large (VEI > 3) tropical volcanic eruptions; this is not the case for extra-tropi

235 , we show evidence of cirrus modification by volcanic eruptions through ice nucleation on VA, reveale

236 ic SST cooling in response to large tropical volcanic eruptions through thermodynamic and El Nino-Sou

237 Volcanic eruptions transfer huge amounts of gas to the a

238 The reconstruction also suggests that volcanic eruptions trigger El Nino-like PWC weakening, s

239 After volcanic eruptions triggered population displacements in

240 We simulate explosive volcanic eruptions using the Laboratoire de Meteorologie

241 ed the fundamental climate response to large volcanic eruptions: Volcanic eruptions cool the surface,

242 climate-model simulations of the 2011 Nabro volcanic eruption, we show that eruption induced an El N

243 Silicic calderas form during explosive volcanic eruptions when magma withdrawal triggers collap

244 re in the form of volcanic dust by explosive volcanic eruptions, which were invoked by others to expl

245 These arose in the aftermath of two major volcanic eruptions, with each cooling transition being f

246 cold summers that often occurred after large volcanic eruptions, with Laki in 1783 and Tambora in 181

247 In terms of air pollution, such a volcanic eruption would therefore be a severe health haz