ライフサイエンスコーパス: sea level rise

1 oreline accretion rates that outpace current sea level rise.

2 he GS east of 65 degrees W may contribute to sea level rise.

3 t on the stability of the WAIS and resulting sea level rise.

4 itive habitat already threatened by eustatic sea level rise.

5 king increasing water depths consequent upon sea level rise.

6 founds both the detection and attribution of sea level rise.

7 Sheet is the largest land ice contributor to sea level rise.

8 (GICs) contributes about 43% to contemporary sea level rise.

9 changes in net N2 O fluxes caused by future sea level rise.

10 in coastal ecosystems may respond to future sea level rise.

11 historical and future human exploitation and sea level rise.

12 butions of the Greenland ice sheet to global sea level rise.

13 produce uncertainty ranges for 21st century sea level rise.

14 tribution to constrain projections of future sea level rise.

15 reliability of models used to predict global sea level rise.

16 east 25.0 +/- 9.4 millimetres of global-mean sea level rise.

17 plications for increasing the rate of global sea level rise.

18 ort-term observation limits models of future sea level rise.

19 tribution of the West Antarctic Ice Sheet to sea level rise.

20 o project future ice mass loss and resulting sea level rise.

21 rm events with 32% due to projected regional sea level rise.

22 alue for the highest scenario of global mean sea level rise.

23 ing when evaluating the potential effects of sea level rise.

24 nd will become a major future contributor to sea level rise.

25 owdown (rapid increase) in shelf and coastal sea level rise.

26 scenarios, suggesting a strong resilience to sea level rise.

27 to habitat changes caused by 21(st) century sea-level rise.

28 the oceans, leading to thermal expansion and sea-level rise.

29 e mid-Cretaceous, associated with an extreme sea-level rise.

30 re likely than best-case scenarios of slower sea-level rise.

31 urrence of extreme water-level events due to sea-level rise.

32 e against the increased flood risk caused by sea-level rise.

33 s significantly amplifies the risk caused by sea-level rise.

34 le to increases in flooding frequency due to sea-level rise.

35 patial scales needed to mitigate losses from sea-level rise.

36 l forcing such as gradual climate warming or sea-level rise.

37 ctica, presently contributes 5-10% of global sea-level rise.

38 e as 500 years, causing 2.5 to 3.0 meters of sea-level rise.

39 amplify AIS mass loss and accelerate global sea-level rise.

40 eleration of grounded ice flow and increased sea-level rise.

41 as been paid to their impacts on longer-term sea-level rise.

42 will not necessarily alter vulnerability to sea-level rise.

43 y is most valuable if maintained with future sea-level rise.

44 of peat soil development, and resilience to sea-level rise.

45 termination VI and on the duration of MIS 13 sea-level rise.

46 rming, with possible implications for future sea-level rise.

47 and could have contributed 1.4-2 m to global sea-level rise.

48 redicting the contributions of ice sheets to sea-level rise.

49 te changing Holocene climatic conditions and sea-level rise.

50 he Pliocene epoch, causing several metres of sea-level rise.

51 tains the equivalent of 7.4 metres of global sea-level rise.

52 the resilience of communities to storms and sea-level rise.

53 ication is not to minimize the importance of sea-level rise.

54 ecause of land use change, wave erosion, and sea-level rise.

55 gest cryospheric contributor to contemporary sea-level rise.

56 stems that are vulnerable to inundation from sea-level rise.

57 ce equivalent to more than a metre of global sea-level rise.

58 bout 70 per cent of the glacial-interglacial sea-level rise.

59 to have variable, but high, rates of future sea-level rise.

60 commitment (an unstoppable contribution) to sea-level rise.

61 urce of uncertainty in projections of future sea-level rise.

62 ed, providing a possible mechanism for rapid sea-level rise.

63 ided by accelerated global ocean warming and sea-level rise.

64 d by volcanic degassing, global warming, and sea-level rise.

65 ntury alone will cause substantial long-term sea-level rise.

66 hey may be critical for understanding future sea-level rise.

67 s will be seriously endangered as the global sea level rises.

68 deltas(8,10), increased coastal erosion and sea-level rise(11) signal a continuing negative trajecto

69 1-13) the ice sheet accelerates ice flow and sea-level rise(14-16).

70 With expected accelerated sea-level rise(5), however, recent land gains are unlike

71 ts suggest a long duration for the period of sea-level rise (533 +/- 2 through 498 +/- 2 ka) encompas

72 slowdown of the GS west of 70 degrees W and sea level rise acceleration along the U.S.

73 constructions document a continuous but slow sea-level rise after 6.5 ka with an accumulated change i

74 associated with a continued acceleration of sea-level rise along the northeast coast of the United S

75 Sea-level rise, an increase in the frequency and intensi

76 al human impacts (e.g., interactions between sea level rise and anthropogenic land subsidence, which

77 The model also suggests that continued sea level rise and coastal population growth could trigg

78 er 21, Texas, is the combination of absolute sea level rise and land subsidence.

79 because of human-driven disturbances such as sea level rise and oil spills can potentially reduce mar

80 y, exposing links between increased rates of sea level rise and storm flood heights.

81 itical to mid-latitude population centres as sea levels rise and tropical cyclone maximum intensities

82 ases in frequency are more clearly linked to sea-level rise and global warming.

83 Predicted sea-level rise and increased storminess are anticipated

84 maintenance of barrier island resilience to sea-level rise and is used to extend hurricane records b

85 ropogenic greenhouse gas emissions on future sea-level rise and its long-term impacts.

86 34)U/(238)U started to increase before major sea-level rise and overshot the modern value by 3 per mi

87 s of less than 350 years at current rates of sea-level rise and sediment availability.

88 ntrolled by the competition between relative sea-level rise and sediment supply that drives lobe prog

89 hwater reservoir, results directly in global sea-level rise and Southern Ocean freshening.

90 the drivers of differences between published sea-level rise and storm surge projections, and how thes

91 or significant uncertainty in projections of sea-level rise and that large ensembles are a necessary

92 Rates of sea-level rise and the extent of human perturbation of t

93 ng the increasing flood risk associated with sea-level rise and tidal and/or meteorological changes a

94 forests have the capacity to keep pace with sea-level rise and to avoid inundation through vertical

95 Increasing rates of sea-level rise and wave action threaten coastal populati

96 rsistence perennially under current rates of sea-level rise and, for most sites, for over a century w

97 dal Oscillation (PDO) years, as well as with sea-level-rise and surface warming, caused primarily by

98 ons under long-term Native American harvest, sea-level rise, and climate change; provide context for

99 ubsidence, regional water management, global sea-level rise, and climate extremes.

100 regional mid-late Holocene and 20th century sea-level rise, and close to IPCC sea-level rise project

101 intensifying tropical cyclones, accelerating sea-level rise, and increasing coastal flooding.

102 astal wetlands in mitigating climate change, sea-level rise, and salinity increase, soil organic carb

103 s at a rate that matches or exceeds relative sea-level rise, apart from rapidly subsiding Texas and L

104 ce 1972, the largest contributions to global sea level rise are from northwest (4.4 +/- 0.2 mm), sout

105 eleased in contaminated coastal soils due to sea level rise are unknown.

106 Implied rates of sea-level rise are high (up to several meters per centur

107 pping point, potentially leading to rates of sea level rise at least an order of magnitude larger tha

108 Relative sea level rise at tide gauge Galveston Pier 21, Texas, i

109 the Atlantic Ocean warming and thermosteric sea-level rise at low latitudes to midlatitudes emerged

110 ojections with worst-case scenarios of rapid sea-level rise being more likely than best-case scenario

111 ate stability changes controlled by relative sea-level rise, bottom water warming and fluid pathway e

112 ent decomposition of the global and regional sea-level rise budget.

113 contributed little to late-glacial pulses in sea-level rise but was involved in mid-Holocene rises.

114 ose ecosystems that are highly vulnerable to sea level rise, but they may also be vulnerable to sea l

115 elevation gain that match or exceed that of sea-level rise, but for 69 per cent of our study sites t

116 and groundwater pumping, slowing the rate of sea level rise by 0.71 +/- 0.20 millimeters per year.

117 potential to contribute more than a metre of sea-level rise by 2100 and more than 15 metres by 2500,

118 llimetres and 17 to 74 millimetres to global sea-level rise by 2100 under moderate- and high-emission

119 result in about 1 m of committed global mean sea-level rise by 2300, with the NDC emissions from 2016

120 ves to accrete vertically and keep pace with sea-level rise by growing on their own root remains.

121 many coastal regions, projections of global sea-level rise by the year 2100 (e.g., 0.5-2 meters) are

122 e use island isolation following postglacial sea-level rise, ca. 2.5 ka, to characterize long-term ch

123 However, even gradual sea-level rise can rapidly increase the frequency and se

124 Sea-level rise can threaten the long-term sustainability

125 However, projected sea-level rise causes overall flood heights associated w

126 eal waves will synergistically interact with sea-level rise, causing twice as much land forecast to b

127 In T-I, the major sea-level rise clearly post-dates Heinrich Stadial 1.

128 Sea level rise, coastal land subsidence, and increasing

129 As global climate warms and sea level rises, coastal areas will be subject to more f

130 To avoid submergence during sea-level rise, coastal wetlands build soil surfaces ver

131 lso find that 26 cm (12 cm) of the projected sea-level-rise commitment in 2300 can be attributed to e

132 mate deglaciation can explain the more-rapid sea-level rise compared with the last deglaciation.

133 combine the equilibrium response of the main sea level rise contributions with their last century's o

134 ed that the ice sheet contribution to future sea level rise could have been underestimated in the lat

135 Even in the absence of sea-level rise, deltas are increasingly vulnerable to co

136 Over the past 30 years, despite sea-level rise, deltas globally have experienced a net l

137 pared areas of habitat to areas of predicted sea level rise, development, and protected areas.

138 Sea-level rise due to ice loss in the Northern Hemispher

139 t constrains the WAIS contribution to global sea level rise during interglacials to about 3.3 m above

140 ey in Rome that was deposited in response to sea-level rise during Marine Isotopic Stage (MIS) 13.

141 thousand years ago and was linked with rapid sea-level rise during T-II.

142 Ice Sheet explains the high rates of global sea-level rise during the 1940s, while a sharp increase

143 rrevocably contribute at least 3 m to global sea-level rise during the coming centuries to millennia.

144 Several studies have suggested that sea-level rise during the last interglacial implies retr

145 However, the findings suggest that long-term sea-level rise effects such as tidal inundation and incr

146 Sea level rise elicits short- and long-term changes in c

147 ly low progradation rates such that relative sea-level rise enhances aggradation rates-accelerating a

148 f northeast Greenland that holds a 0.5-meter sea-level rise equivalent, entered a phase of accelerate

149 he potential responses of coastal species to sea-level rise, especially for species that rely on coas

150 Global mean sea level rise estimated from satellite altimetry provid

151 7 centuries, a value similar to the rates of sea-level rise estimated for the Caribbean during a comp

152 e, we map areas of blanket bog vulnerable to sea-level rise, estimating that this equates to ~7.4% of

153 ed in this study to indicate that punctuated sea-level rise events are more common than previously ob

154 preted to be generated by several punctuated sea-level rise events forcing the reefs to shrink and ba

155 erraces are interpreted to record punctuated sea-level rise events over timescales of decades to cent

156 When global sea level rise exceeded the local rate of bank building,

157 cent of our study sites the current rate of sea-level rise exceeded the soil surface elevation gain.

158 The 10 to 20 cm of sea-level rise expected no later than 2050 will more tha

159 to increase surface elevation in response to sea-level rise, for most services there has been no dire

160 eaf forest at the expense of pine woodland), sea level (rising from -80 m to nearly modern levels), a

161 The contribution to sea-level rise from Antarctica averaged 3.6 +/- 0.5 mm p

162 ng ice-sheet evolution and projecting global sea-level rise from ice-sheet loss.

163 eciphering magnitudes, rates, and sources of sea-level rise from polar ice-sheet loss during past war

164 on of this marine-based sector will increase sea-level rise from the Greenland Ice Sheet for decades

165 eased by approximately 1.24 m (due mainly to sea level rise) from approximately A.D. 850 to the anthr

166 nce of avulsions will change due to relative sea-level rise, hampering the ability to forecast delta

167 The Antarctic contribution to sea level rise has reached ~8 millimeters since 1992.

168 e contribution of the Greenland ice sheet to sea-level rise has accelerated in recent decades.

169 and water storage and their contributions to sea level rise have been absent from Intergovernmental P

170 recasts of increasing global temperature and sea level rise have led to concern about the response of

171 timates of increased coastal flooding due to sea-level rise have not considered elevated water levels

172 uncertainties surrounding present and future sea-level rise have revived the debate around sea-level

173 Recognizing the nature of past sea-level rises (i.e., gradual or stepwise) during degla

174 On top of this quantification, the sea level rise impact over coastal areas has to be super

175 have by default been ignored in broad-scale sea-level rise impact assessments to date.

176 , but it remains a challenge to evidence how sea-level rise impacts aquatic island biogeography, espe

177 Our analyses indicate that sea-level rise in recent decades has widely outpaced mar

178 n temporarily obscure the long-term trend in sea level rise, in addition to modulating the impacts of

179 Global climate change drives sea-level rise, increasing the frequency of coastal floo

180 rld's glaciers and ice sheets contributes to sea level rise, influences ocean circulation, and affect

181 nt impacts of climate change: acidification, sea-level rise, intensification of storms, shifts in spe

182 ntury with projected medium accelerations in sea-level rise (IPCC RCP 6.0).

183 Only the fastest projected accelerations in sea-level rise (IPCC RCP 8.5) led to widespread submerge

184 sea level remains uncertain, but multimeter sea level rise is likely for a mean global temperature i

185 Our results indicate that (a) sea level rise is unlikely to decrease the SOM decay rat

186 Sea-level rise is a global problem, yet to forecast futu

187 Sea-level rise is beginning to cause increased inundatio

188 Global sea-level rise is caused, in part, by more rapid ice dis

189 Regional sea-level rise is characterized by decadal acceleration

190 Thus, sea-level rise is creating conditions within which Sesar

191 Well above average sea-level rise is found regionally near the Philippines

192 s provides insights into physical processes: sea-level rise is often assumed to follow air temperatur

193 Sea-level rise is particularly critical for low-lying ca

194 Sea-level rise may accelerate significantly if marine ic

195 g salt marsh, wetland capacity to respond to sea-level rise may change.

196 evel thresholds increases exponentially with sea-level rise, meaning that fixed amounts of sea-level

197 ) changing tidal regimes in mangroves due to sea level rise might attenuate increases in SOM decay ca

198 has allowed mangroves to persist in areas of sea level rise, might result from changes in root produc

199 In most coastal regions, the amount of sea-level rise occurring over years to decades is signif

200 rary applications of radar altimetry include sea-level rise, ocean circulation, marine gravity, and i

201 The main contributors to sea-level rise (oceans, glaciers, and ice sheets) respon

202 We project anthropogenic sea level rise of 28-56 cm, 37-77 cm, and 57-131 cm in 2

203 We estimate ice loss corresponding to a sea level rise of 8.1 +/- 1.1 millimetres from these thr

204 d in the retreat and growing contribution to sea level rise of PIG and nearby glaciers.

205 he year 2100 would commit an eventual global sea-level rise of 4.3-9.9 m.

206 om West Antarctica, associated with a global sea-level rise of more than 3 m, or whether the ice loss

207 ea-level rise, meaning that fixed amounts of sea-level rise of only ~1-10 cm in areas with a narrow r

208 For sea-level rise of this magnitude, extensive retreat or c

209 While the effects of sea level rise on salt marshes and mangroves are well st

210 fied in this study demonstrate the effect of sea level rise on spatial and temporal community reassem

211 rienced one of the highest rates of relative sea level rise on the Atlantic coast of the United State

212 odels show that ice-sheet melt will dominate sea-level rise over the coming centuries, but our unders

213 s the potential to contribute up to ~15 m of sea-level rise over the next few centuries.

214 Our uncertainty ranges for total sea level rise overlap with the process-based estimates

215 ncluding how this timing is affected by mean sea-level rise, predicts a reproductive threshold that i

216 ecome one of the main contributors to global sea level rise, predominantly through increased meltwate

217 tal ablation rates) are a key uncertainty in sea level rise projections.

218 ted for in most ice sheet models, to improve sea level rise projections.

219 The sea-level rise projections account for potential partial

220 would be considerable uncertainty in future sea-level rise projections due to imperfectly modeled ic

221 th century sea-level rise, and close to IPCC sea-level rise projections through to 2100.

222 These overestimates are similar to recent sea-level rise projections to 2100 at some locations.

223 bine modeled storm surges with probabilistic sea-level rise projections to assess future coastal inun

224 ombining these growth rates with established sea-level rise projections, we find that the odds of ext

225 maintaining coastline elevations relative to sea level rise, protecting coastal infrastructure from s

226 ting scenario corresponding to an additional sea level rise ranging from 0.5 m to 3 m.

227 We estimate a uniform absolute sea level rise rate of 1.10 mm +/- 0.19/a in the Gulf of

228 ove wetlands were exceeding current relative sea-level rise rates (2.6 mm yr(-1)), with surface eleva

229 nderstanding of hard armoring distributions, sea level rise response plans can be fully informed to d

230 Sea-level rise resulting from the instability of polar c

231 This rate of relative sea level rise results from a combination of land subsid

232 y the interplay between the rate of relative sea-level rise (RRSLR), surface accretion by inorganic s

233 ponse of mangroves to high rates of relative sea level rise (RSLR) is poorly understood.

234 Relative sea level rise (RSLR) largely regulates the CAR.

235 their vulnerability to accelerated relative sea level rise (RSLR).

236 Climate change and associated relative sea-level rise (RSLR) have been proposed to increase the

237 to determine ecosystem response to relative sea-level rise (RSLR) over the Holocene.

238 ome of the world's highest rates of relative sea-level rise (RSLR).

239 which are in turn a function of the rate of sea level rise, sand availability, and stress of the pla

240 For the various sea-level rise scenarios we consider, the 1-in-500-y flo

241 Comparison of land movement with relative sea-level rise showed that this plant community was expe

242 ltas may face even greater risk; if relative sea-level rise significantly outpaces sediment supply, t

243 ributed as much as 85% of the 0.7 m relative sea level rise since 1909, and an additional 1.9 m is pr

244 antly from glaciers-has caused twice as much sea-level rise since 1900 as has thermal expansion.

245 The rate of global-mean sea-level rise since 1900 has varied over time, but the

246 oncile the magnitude of observed global-mean sea-level rise since 1900 with estimates based on the un

247 The acceleration in sea-level rise since the 1970s is caused by the combinat

248 Here we test for the effects of sea level rise (SLR) and its interactions with elevated

249 odynamic modeling to quantify the effects of sea level rise (SLR) and TC climatology change (under RC

250 Coastal inundation due to sea level rise (SLR) is projected to displace hundreds o

251 One of the main consequences of mean sea level rise (SLR) on human settlements is an increase

252 Sea level rise (SLR), a well-documented and urgent aspec

253 es beach loss globally, will accelerate with sea level rise (SLR), causing more beach loss if managem

254 ation and obligate use of beaches subject to sea level rise (SLR).

255 erm tide gauge records identified an extreme sea-level rise (SLR) event during 2009-10.

256 Sea-level rise (SLR) induced flooding is often envisione

257 Climate change associated sea-level rise (SLR) is expected to have profound impact

258 rd of ice sheet contributions to global mean sea-level rise (SLR) since the Fifth Assessment Report (

259 Forecasted accelerations in sea-level rise (SLR) will shift the position of these cr

260 ffects of tides, surges, waves, and relative sea-level rise (SLR), neglecting non-linear feedbacks be

261 urrent projections of climate change induced sea-level rise (SLR), thus posing a threat to reef funct

262 has added less than one millimetre to global sea-level rise so far, this contribution will grow subst

263 Our results indicate that a sudden sea level rise (SSLR) event-driven column stratification

264 Our results demonstrate the threat of sea level rise stands to impact arsenic release from con

265 ulnerable to morphological changes caused by sea level rise, subsidence, anthropogenic modifications,

266 Sea-level rise, subsidence, and reduced fluvial sediment

267 forecast to be flooded for a given value of sea-level rise than currently predicted by current model

268 ater wave-induced run-up and flooding due to sea-level rise than those with deeper reef crests farthe

269 ropogenic carbon emissions lock in long-term sea-level rise that greatly exceeds projections for this

270 from Antarctica is important in determining sea level rise, the fate of Antarctic sea ice and its ef

271 Due to the effect of sea level rise, the return period of Hurricane Sandy's f

272 Predictions for sea-level rise this century due to melt from Antarctica

273 Most estimates of global mean sea-level rise this century fall below 2 m.

274 s the ice surface, predict a metre of global sea-level rise this century in response to atmospheric w

275 ions of these MICI projections over-estimate sea-level rise this century; because the MICI hypothesis

276 se, in addition to modulating the impacts of sea level rise through natural periodic undulation in re

277 t short-lived greenhouse gases contribute to sea-level rise through thermal expansion (TSLR) over muc

278 t reef capacity to track IPCC projections of sea-level rise, thus limiting the natural breakwater cap

279 To thrive in a time of rapid sea-level rise, tidal marshes will need to migrate upslo

280 current altimeter products show the rate of sea level rise to have decreased from the first to secon

281 ptions, our estimates limit maximum Pliocene sea-level rise to less than 25 metres and provide new co

282 es large areas, the relative contribution of sea-level rise to the frequency of these events is diffi

283 hat coastal and neritic fauna benefit during sea-level rise (transgression), whereas sea-level retrea

284 far the largest potential source for global sea-level rise under future warming conditions(1).

285 tribution that large ice sheets will make to sea-level rise under such warming scenarios is difficult

286 Here we identify the committed global mean sea-level rise until 2300 from historical emissions sinc

287 eate accurate projections of future relative sea level rise upon which to base planning efforts.

288 s to estimate the land component of relative sea level rise using interferometric synthetic aperture

289 well mangroves and salt marshes accommodate sea-level rise, we conducted a manipulative field experi

290 sand years ago, ka) was the last time global sea level rose well above the present level.

291 d surface meltwater trigger faster ice flow, sea level rise will accelerate.

292 Sea level rise will change inundation regimes in salt ma

293 The rate of sea level rise will keep increasing with continued globa

294 Sea-level rise will affect coastal species worldwide, bu

295 Assuming no feedbacks, accelerating global sea-level rise will eventually surpass current sediment

296 indicate that the ongoing global warming and sea-level rise will lead to significant intensification

297 Sea-level rise will radically redefine the coastline of

298 Here we demonstrate that sea-level rise will result in larger waves and higher wa

299 r coastal wetlands generally focus solely on sea-level rise without considering the effects of other

300 te to seabed elevation and therefore buffers sea-level rise, without undermining their role as CO(2)