ライフサイエンスコーパス: subsidence

1 f dynamical transports of methane and strong subsidence.

2 efore apparently driving present-day surface subsidence.

3 Gulf of Mexico, especially those affected by subsidence.

4 ve of urbanization may be threatened by land subsidence.

5 Middle East, has been suffering from extreme subsidence.

6 tic coast and are particularly vulnerable to subsidence.

7 in at-risk populations of 18% to 61% due to subsidence.

8 attraction toward the ice sheet and crustal subsidence.

9 idents, mainly sea level rise (SLR) and land subsidence.

10 with transient reversals between uplift and subsidence.

11 g the coastline during 2002-2010 due to land subsidence.

12 M(w) 8.6 earthquake and coseismic uplift and subsidence.

13 alysis reveals widespread, spatially varying subsidence.

14 bination of absolute sea level rise and land subsidence.

15 measures to mitigate potential damages from subsidence.

16 must address drivers, not just symptoms, of subsidence.

17 lift and seismicity, and resulted in caldera subsidence.

18 rease by 27% (Irene) to 40% (Matthew) due to subsidence.

19 year globally, and quantifies key drivers of subsidence.

20 alluvial deposits makes the region prone to subsidence.

21 es spatially, particularly due to local land subsidence.

22 only a small fraction of the areas prone to subsidence.

23 eastern rift zone and 2.5 m of caldera-wide subsidence.

24 s street-level and elevated segments to land subsidence.

25 ifers to pollutants and contributing to land subsidence.

26 sh vulnerability by not fully accounting for subsidence.

27 t of groundwater pumping and associated land subsidence.

28 causing correlations in volcanic uplift and subsidence.

29 shifts in the locations and rates of maximum subsidence.

30 e rift zone volcanism and subsequent caldera subsidence.

31 de dryer via pole-ward expanding subtropical subsidence.

32 diments and reductions in human-induced land subsidence.

33 ecades, and is surrounded by a broad zone of subsidence.

34 ports their proposal that mantle flow drives subsidence.

35 Nile Delta) experienced the maximum rates of subsidence (- 11 +/- 0.6, - 8.9 +/- 0.7, and - 6.3 +/- 0

36 ), resulting in seawater intrusion(11), land subsidence(12,13), streamflow depletion(14-16) and wells

37 atering of As-bearing clays (proxied by land subsidence), (2) pH-promoted desorption as well as reduc

38 ave identified anomalously localized surface subsidence above seismically imaged lower mantle upwelli

39 e-injection produces 12 mm yr-1 of long-term subsidence, accompanied by an unprecedented seasonal osc

40 en years post-fire, detected permafrost thaw subsidence across 34% of the burned tundra area studied,

41 for quantifying the magnitude and extent of subsidence affecting the Metro system's widespread infra

42 they highlight both localized rates of high subsidence and a significant spatial variability in subs

43 ination of rising sea levels, ground surface subsidence and anthropogenic sediment trapping, and a su

44 inable in the long-term, and to help reverse subsidence and capture carbon (C) there is an interest i

45 e of organic soils has resulted in vast soil subsidence and contributed to increased atmospheric carb

46 Subsidence and deceleration occurred over the subsequent

47 Long-term land subsidence and depth-resolved sediment texture were comp

48 eothermal field deformation including ground subsidence and earthquakes.

49 circulation response which creates anomalous subsidence and enhances surface solar heating over the A

50 ic carbon (OC) was promoted by high tectonic subsidence and fluvial sediment supply.

51 ock and upwelling can extend the duration of subsidence and focus the subsidence into a narrow region

52 Both isostatic subsidence and frequent storms under the colder climatic

53 es in the Early Miocene was brought about by subsidence and glacial erosion in West Antarctica during

54 global risk of long-span bridges affected by subsidence and landslides.

55 e to multiple adverse impacts including land subsidence and permanent groundwater storage loss.

56 nd-use types can help reduce or reverse soil subsidence and reduce GHG emissions.

57 Following rapid coeruptive subsidence and reduction in stress and background seismi

58 nsgressions relative to long-term changes in subsidence and relief of regional lithology must be cons

59 exacerbate salinisation, compounded by land subsidence and rising sea levels.

60 tion, because of the combined effect of city subsidence and sea-level rise.

61 dred and fifty years due to the ongoing land subsidence and SLR of 3.4 mm/year.

62 iously identified positive feedbacks between subsidence and thaw are self-limiting on decadal time fr

63 thane and forms as a result of stratospheric subsidence and the particularly cool conditions near the

64 Thaw-induced subsidence and the resulting inundation along this progr

65 These results imply that subsidence and thermokarst-associated increases in organ

66 We show how centuries of repeated subsidence and uplift during great-earthquake cycles alo

67 nd previously undocumented hot spots of both subsidence and uplift that can be physically explained i

68 a spatially and temporally varying record of subsidence and uplift that is consistent with models of

69 It is crucial to control surface subsidence and utilize solid wastes for sustainable mini

70 g method with advantages in avoiding surface subsidence and utilizing solid wastes.

71 northern hemisphere, initiating south-polar subsidence and winter polar vortex formation.

72 ost accurate for predicting landslides, land subsidence, and flood hazards in the study area.

73 snow avalanches, landslides, wildfires, land subsidence, and floods using machine learning models tha

74 xiform layer [OPL]/inner nuclear layer [INL] subsidence, and hyporeflective wedge-shaped band).

75 Sea level rise, coastal land subsidence, and increasing water demands will exacerbate

76 cannot fully explain the observed localized subsidence, and its locality implies a strong associatio

77 More seamounts, slower subsidence, and less dense mantle on the western flank s

78 Sea-level rise, subsidence, and reduced fluvial sediment supply are caus

79 tened by rising sea levels, accelerated land subsidence, and reduced sediment supply from contributin

80 ng due to anthropogenic sea-level rise, land subsidence, and reduced sediment supply.

81 ne position that include erosion, permafrost subsidence, and sea-level rise.

82 The observed subsidence anomalies result from the siphoning effect an

83 phological changes caused by sea level rise, subsidence, anthropogenic modifications, and changes to

84 The subsidence appears to be associated with a range of fact

85 esolution observations and models of coastal subsidence are scarce, hindering an accurate vulnerabili

86 itoring prove that roof movement and surface subsidence are well controlled by using the developed me

87 s: Total Hip Arthroplasty, Femoral Component Subsidence, Artificial Intelligence, Deep Learning, Sema

88 This analysis emphasizes subsidence as a RSLR hazard in China that requires a bro

89 ering local-scale signals hidden by regional subsidence as detected by interferometric SAR measuremen

90 h rates reaching 20 cm yr(-1) and cumulative subsidence as much as 155 cm.

91 ption and the qualitative markers of OPL/INL subsidence, as well as a wedge-shaped band.

92 tland exposed to recent rapid RSLR following subsidence associated with pillar collapse in an underly

93 id from surrounding regions, which can cause subsidence at low-rate injection locations.

94 Stratospheric subsidence at the edges of the disturbance produced "bea

95 Subsidence attributed to aquifer-system compaction accom

96 no exception, experiencing about a meter of subsidence between 2015 and 2020.

97 to automatically quantify femoral component subsidence between two serial anteroposterior (AP) hip r

98 yer that thaws each summer-is accelerated by subsidence, but the effect is relatively small.

99 sing algorithm was then developed to measure subsidence by automatically annotating reference points

100 ponents of relative sea-level change (mainly subsidence) can also be locally appreciable.

101 ical land motion (VLM), including uplift and subsidence, can greatly alter relative sea level project

102 re heating that shifts the Hadly circulation subsidence center poleward.

103 ed silicates yielding a load-bearing and low-subsidence composite.

104 res a broad-scale policy response, utilizing subsidence control combined with coastal adaptation.

105 Realistic subsidence control measures can avoid up to two thirds o

106 ntinued to increase linearly, ground surface subsidence created saturated microsites and suppressed R

107 , including tide gauge records, GPS geodetic subsidence data, and Interferometric Synthetic Aperture

108 jected by 2100, with contributions from land subsidence declining from 30 to 10% over the projection

109 yedoma), accounting for ~50% of the detected subsidence, despite representing only 30% of the fire di

110 However, subsidence does have significant effects on the hydrolog

111 that the Ardabil plain has been facing rapid subsidence due to groundwater pumping and reduced rainfa

112 ) in northwestern Iran, has experienced land subsidence due to intensive groundwater withdrawal and l

113 estimates, and empirical assessments of land subsidence due to permafrost thaw with projections of co

114 ates Atlantic coastline continues to undergo subsidence due to post glacial settlement and ground wat

115 An abrupt slowing of subsidence during the past million years was likely caus

116 ant cells during flooding and directly after subsidence, during which the plant is confronted with hi

117 nce and a significant spatial variability in subsidence, emphasizing the need for further measurement

118 el and significant post-2009 earthquake land subsidence, endangering homes and critical infrastructur

119 ess, with high seismicity, continuing uplift/subsidence episodes with movements of approximately 70 c

120 nd Matthew are simulated considering SLR and subsidence estimates for 2100.

121 Similar abnormal subsidence events in northeastern Asia further show the

122 vidence for repeated late Holocene coseismic subsidence events.

123 gnificant movement of these landslides, with subsidence exceeding 40 mm over seven years.

124 n risks associated with sea-level rise, land subsidence, extreme weather, and public health.

125 Our analysis reveals two distinct subsidence features in the study area with rates exceedi

126 Femoral component subsidence following total hip arthroplasty (THA) is a w

127 ould absorb water, expand, deliquesce, cause subsidence, form crusts, disrupt surfaces, and ultimatel

128 Projections indicate 63 cm of bulk subsidence from 2006 to 2100 in the strong-warming Repre

129 thermochronology, to resolve local tectonic subsidence from global sea level.

130 of global sea-level rise and rapid localized subsidence has not been observed in our Holocene geologi

131 suggest locations where the consequences of subsidence have compromised the train's braking safety d

132 Namibia, combined with estimates of thermal subsidence history, suggest that biological productivity

133 This rise, likely driven by subsidence, implies that evidence for early settlement c

134 we provided a systematic assessment of land subsidence in all of China's major cities from 2015 to 2

135 oximately 23 year data-span to quantify land subsidence in cropland areas.

136 and increasing frequency and extent of land subsidence in Iran's planes.

137 tudy aid in assessing the spatial extents of subsidence in known subsiding areas, and in locating unk

138 ion, with uplift observed in late winter and subsidence in late summer, showing a periodicity of appr

139 ce long-lived coherent structures that cause subsidence in local regions, explaining the low cloudine

140 low-level cooling and anomalous atmospheric subsidence in response to positive vegetation greenness

141 assessment confirms that the main reason for subsidence in the interested area is groundwater over-ex

142 Radar altimetry also reveals time-varying subsidence in the North China Plain consistent with the

143 ls that parts of New Orleans underwent rapid subsidence in the three years before Hurricane Katrina s

144 The subsidence in these two areas are accelerating and follo

145 s have been used to investigate and evaluate subsidence in this region including: Global Positioning

146 Specifically, subsidence increases landscape runoff, which helps maint

147 Subsidence induced by groundwater depletion is a grave p

148 Regional land subsidence influences RSLR, however quantified rates of

149 end the duration of subsidence and focus the subsidence into a narrow region, which we call the lens

150 ates that at least 94% of rapid modern urban subsidence is attributable to anthropogenic activities,

151 Land subsidence is impacting large populations in coastal Asi

152 y 50 cm to approximately 180 cm by 2100 when subsidence is included compared to about 160 cm when it

153 We find that land subsidence is ubiquitous throughout the region with rate

154 athes of the Alaska North Slope suggest that subsidence is unlikely to lead to abrupt thaw over large

155 ed by ELM disruption (kappa = 0.58), OPL/INL subsidence (kappa = 0.46), and a hyporeflective wedge-sh

156 tionary wave propagation, leading to greater subsidence, less precipitation, and higher temperatures

157 The developed model predicts global land subsidence magnitude at high spatial resolution (~2 km),

158 s controlling elevation (sediment accretion, subsidence), mangrove replacement of salt marsh, with or

159 Here we present a new subsidence map for the city, generated from space-based

160 However, caldera subsidence may also proceed silently by magma withdrawal

161 show that the ongoing uplift and peripheral subsidence may result from a large mid-crustal diapir fe

162 processing package and its accuracy for land subsidence measurements at different scales needs furthe

163 luating its efficiency and accuracy for land subsidence measurements by comparing its measurements wi

164 Algorithm and manual subsidence measurements by two independent orthopedic su

165 Comparison of the subsidence measurements of the Ardabil plain using the L

166 learning tool needs no user input to perform subsidence measurements.

167 ame) system revealed a slow (heave) and fast subsidence mode and an unstable oscillatory mode, a moda

168 abilized system with a slow (heave) and fast subsidence mode, and a stable oscillatory mode.

169 coverage, and can provide long-term temporal subsidence monitoring capability.

170 Erosion and subsidence moved the shoreline of Banda Aceh inland up t

171 nerable to flooding and often exacerbated by subsidence (negative vertical land motion; VLM).

172 uptive magma withdrawal resulted in 8.5 m of subsidence, net uplift of the inner-caldera on a trapdoo

173 Roughly 73% of the mapped subsidence occurs over cropland and urban areas, highlig

174 uption, the instrument also measured gradual subsidence of 1.4 metres over the next several days, ref

175 We find broad subsidence of 1.6 mm/year, consistent with glacial isost

176 e rates reach 18 cm yr(-1) with a cumulative subsidence of 206 cm, which potentially could adversely

177 tes that this weakness could be explained by subsidence of a metre or more since their construction.

178 infected mice during a key period after the subsidence of acute malaria symptoms, but during which m

179 ed in phosphine gas, probably resulting from subsidence of air into the troposphere.

180 st the New Hebrides arc, lead to progressive subsidence of Ambrym's caldera and concurrent draining o

181 G2A subset were witnessed within 3 months of subsidence of chronic GVHD.

182 Our results illustrate the maintenance and subsidence of different IAVs within swine farrow-to-wean

183 d continental margin thereby contributing to subsidence of flanking sedimentary basins.

184 l measures in hospital plumbing aligned with subsidence of hospital A-associated cases; and d) wgMLST

185 The subsidence of liver damage in G133E virus-infected birds

186 ble mechanisms to explain the appearance and subsidence of Lyme neuritis are discussed.

187 ctic tundra fires may induce widespread thaw subsidence of permafrost terrain in the first seven year

188 reserved retinal architecture (Pattern 1), a subsidence of retinal layers internal to the EZ into the

189 influence of gravity, display predominantly subsidence of the basin side (fault hanging wall), with

190 The buffered meltwater causes a subsidence of the bedrock close to GNSS stations of at m

191 t with subduction-driven dynamic topographic subsidence of the continental interior.

192 OCT features unique in these areas included: subsidence of the outer plexiform layer (OPL) and inner

193 external limiting membrane (ELM) disruption, subsidence of the outer plexiform layer and inner nuclea

194 r (InSAR) technique to measure the long-term subsidence of the plain.

195 s, in a warm-wet climate, before the thermal subsidence of the RGR to its modern-day bathymetric dept

196 However, subsidence of the substrate shows a nonlinear increase w

197 atancy in the shallow fault zone that causes subsidence of the surface.

198 antial diminution of this resource and rapid subsidence of the valley floor.

199 res when we account for post-glacial crustal subsidence of these sites over the course of the anomalo

200 c routes, but economic factors have led to a subsidence of this effort, which places society on the p

201 storage and release accompanying growth and subsidence of tropical peatlands are affected by climate

202 s showing similar subsidence rates and total subsidence of up to 27 cm since 1988.

203 nsive groundwater extraction is causing land subsidence of up to 3 cm/y as measured using satellite-b

204 ose to the rupture area that had experienced subsidence of up to about 4 centimetres during the earth

205 nner nuclear layer and outer plexiform layer subsidence, or a hyporeflective wedge-shaped band, as a

206 nner nuclear layer and outer plexiform layer subsidence, or a hyporeflective wedge-shaped band, as a

207 iated with ENSO events may lead to a reduced subsidence over the Indian region, thus favoring normal

208 ing, favoring low cloud reduction (Radiation-Subsidence Pathway).

209 ence weakening and low cloudiness (Stability-Subsidence Pathway).

210 rture Radar data, which reveals differential subsidence patterns and the creation of subsurface void

211 t shallow LANF rupture, modulating coseismic subsidence patterns, near-shore slip velocities, and the

212 41% of the observed changes in RSLR and that subsidence poses a major threat to Cartagena's preservat

213 e is already undermined, as evidenced by (i) subsidence problems and (ii) altering aquifers' intercon

214 Throughout 2010-2011, strengthening subsidence produced a mesospheric hot-spot and caused ex

215 007 to 2020 to create high-resolution map of subsidence rate at mm-level accuracy for different land

216 Here, we show that subsidence rate exceeding 3 mm per year affects most coa

217 The maximum subsidence rate in central Taiwan is 8 cm yr(-1).

218 This paper seeks to determine the subsidence rate in urban areas of Mashhad in recent year

219 At least 60% of the total subsidence rate occurs within the uppermost 5-10 m, whic

220 This alarming rate of SLR, coupled with a subsidence rate of more than 2.2 mm/yr, poses a signific

221 The maximum subsidence rate was 45 mm/yr, measured at the southeaste

222 With a low subsidence rate, the rubble-mound-submerged breakwaters

223 ific storage in special cases to predict the subsidence rate.

224 .6 cm/year and maximum vertical deformation (subsidence) rate about 19.1 cm/year which could have irr

225 a, New-Damietta, Kafr El-Sheikh had moderate subsidence rates (- 3.2 +/- 0.6, - 2.4 +/- 0.7, - 4.2 +/

226 sient 3D aquifer simulations showing similar subsidence rates and total subsidence of up to 27 cm sin

227 In 2050, assuming these subsidence rates continue, land area, population and ass

228 The geodetic subsidence rates found would imply a further additional

229 Subsidence rates from TOPEX/POSEIDON, JASON-1, ENVISAT,

230 Land subsidence rates in Mexico City reach 500 mm/year, causi

231 chers have been interested in measuring land subsidence rates in the Mashhad valley by InSAR techniqu

232 The western paleo-valley experienced faster subsidence rates in the period 1995-2007, whereas the ea

233 We find peat surface subsidence rates in the rewetted restoration area and ad

234 We estimate subsidence rates of 3.53 mm/a during 1909-1937, 6.08 mm/

235 ata for the 2014-2020 period show cumulative subsidence rates of up to 72.3 mm.

236 to anthropogenic activities, with localized subsidence rates often exceeding GMSL rise.

237 GPS subsidence rates range between - 5.71 2.18 and - 2.85 0.

238 Near Hanford, California, subsidence rates reach 18 cm yr(-1) with a cumulative su

239 Non-uniform dynamic subsidence rates since 50 Ma likely lowered relief in th

240 d human settlement and has since experienced subsidence rates that are among the highest in the world

241 ously analyse trends and patterns in SLR and subsidence rates using a wealth of data from 1993 to 202

242 ta and Damietta) experienced the majority of subsidence rates, (2) the cities of Damietta, Mansoura a

243 ation change, vertical accretion and shallow subsidence rates.

244 s introducing uncertainties in the resulting subsidence rates.

245 mate, nutrient inputs, sediment delivery and subsidence rates.

246 er fault over the past ~610 ka and an uplift/subsidence ratio of 1:1.1-2.4.

247 ks arising from local human activities, land subsidence, regional water management, global sea-level

248 d, while both the equatorial and subtropical subsidence regions have become drier and less cloudy.

249 had operated for less than 10 years, brought subsidence-related structural damage to the attention of

250 coal body to the backfill body, with surface subsidence remaining within acceptable limits for buildi

251 ng of ice-rich permafrost ground causes land subsidence, resulting in development of distinctive land

252 nfer that the observed pattern of uplift and subsidence results from variations in the movement of mo

253 7 mm/year, respectively), (4) the Nile Delta subsidence seems to be dominated by anthropogenic reason

254 ch the overlying lithosphere, inducing broad subsidence that can be reversed when the upwelling reach

255 aphic and meteorological effects and/or land subsidence that cause relative sea level to rise faster

256 these impacts may be exacerbated by coastal subsidence-the sinking of coastal land areas(4)-a factor

257 ered by a feedback between ice melt-back and subsidence to O(10(10)) W, which is similar to observed

258 Ocean--driven by convection to the west and subsidence to the east--known as the Walker circulation.

259 rgo long-range transport and descend through subsidence to the lower troposphere, in which they can s

260 The third region, Dwarka shows a shift from subsidence to uplift during the years which can be attri

261 formations indicates that mild pre-eruptive subsidence took place in the Wallowa Mountains, followed

262 islands above the rupture and a 1-meter-deep subsidence trough farther from the trench.

263 undwater stress, aquifer depletion, and land subsidence using remote sensing and model-based datasets

264 Our results reveal that high subsidence velocity gradients occur over sharp transitio

265 In a 50 km(2) area, thaw subsidence was detected across 15% of the land area in r

266 orne LiDAR dataset show that additional thaw subsidence was detected in < 1% of the study area, indic

267 Subsidence was greatest in severely burned, ice-rich upl

268 he Heber Geothermal Field (HGF), decade-long subsidence was occurring despite injection of heat-deple

269 In fast-subsiding areas, regional subsidence (wavelength ~ 1,000's m) can be dominantly hi

270 Due to subsidence, we propose that these islands and monuments

271 ncorporating the influence of earthquakes on subsidence, we provide a more nuanced understanding of t

272 s tropospheric stability, which also reduces subsidence weakening and low cloudiness (Stability-Subsi

273 which increases longwave cooling and reduces subsidence weakening, favoring low cloud reduction (Radi

274 Sedimentation and subsidence were hence in pace, with subtle facies change

275 etween sea level rise and anthropogenic land subsidence, which are forcing Indonesia to relocate its

276 evel rise results from a combination of land subsidence, which has long been known to be present in t

277 d magma systems exhibit cycles of uplift and subsidence, while comparatively hot plumbing systems exp

278 pact that sea-level rise and permafrost thaw subsidence will have on permafrost shorelines-have recei

279 geotechnical numerical modeling showed land subsidence with an average annual rate of 38 mm between

280 Compounding these hazards is subsidence, with one-third of the study area currently l

281 Sequential interferograms indicate that subsidence within the caldera migrated from one resurgen

282 t not accounting for spatially variable land subsidence within the cities may lead to inaccurate proj

283 onstrained age is between those of coseismic subsidence Y and W events in southern Washington, which

284 deslip oscillatory motion from a first order subsidence yaw behavior.

285 in this way, after corrections for tectonic subsidence, yield cyclic relative sea-level (RSL) variat