ライフサイエンスコーパス: sea level rise

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

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

3 historical and future human exploitation and sea level rise.

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

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

6 tribution to constrain projections of future sea level rise.

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

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

9 elihood of large ice sheet melting and major sea level rise.

10 er S. patens an enhanced ability to tolerate sea level rise.

11 hange drivers modify marsh plant response to sea level rise.

12 nd accounting for 29 +/- 13% of the observed sea level rise.

13 010, contributing 0.41 +/- 0.08 mm yr(-1) to sea level rise.

14 tant contributors to present-day global mean sea level rise.

15 ying physical mechanisms governing the rapid sea level rise.

16 f warming increases with increasing rates of sea level rise.

17 those of the "dust bowl" era and inexorable sea level rise.

18 c carbonate precipitation during postglacial sea level rise.

19 itive habitat already threatened by eustatic sea level rise.

20 acceleration of ice sheet disintegration and sea level rise.

21 king increasing water depths consequent upon sea level rise.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

38 ice-sheet threshold behaviour and associated sea-level rise.

39 ntecedent foundations during glacio-eustatic sea-level rise.

40 ecades, significantly contributing to global sea-level rise.

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

42 on strategies, socioeconomic development and sea-level rise.

43 mpromise habitat stability and resilience to sea-level rise.

44 nes will increase as a result of accelerated sea-level rise.

45 environmental conditions by contributing to sea-level rise.

46 o actively resist the deleterious effects of sea-level rise.

47 ontributing a quarter of the observed global sea-level rise.

48 ncreased drought frequency, and accelerating sea-level rise.

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

50 h erosion takes place even in the absence of sea-level rise.

51 een vertical sediment accretion and relative sea-level rise.

52 which impounds enough ice to yield meters of sea-level rise.

53 20 millimeter year(-1) to the rate of global sea-level rise.

54 ice sheets is a major contributor to global sea-level rise.

55 ts for about ten per cent of observed global sea-level rise.

56 A curves) or, equivalently, the thermosteric sea-level rise.

57 is reason, contribute increasingly to global sea-level rise.

58 accelerate ice-sheet flow and contribute to sea-level rise.

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

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

61 tica, presently contributes 5-10% of global sea-level rise.

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

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

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

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

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

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

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

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

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

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

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

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

74 of the study, atmospheric CO2 increased 18%, sea level rose 20 cm, and growing season temperature var

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

76 For sea level rise, a substantial long-term commitment may b

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

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

79 ore subtle than the impact of warming-driven sea level rise, although the impact of warming increases

80 delay expansion of the area contributing to sea-level rise, although once the pore space is filled i

81 rm global discharge trends as the records of sea level rise and ocean temperature lengthen.

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

83 rees of robustness to changes in the rate of sea level rise and sediment availability, with implicati

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

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

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

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

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

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

90 ated an assessment of their contributions to sea-level rise and the potential release of nutrients to

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

92 ng reef retreated upslope during postglacial sea-level rise and transformed into a barrier reef when

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

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

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

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

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

98 ely on how human impacts interact with rapid sea-level rise, and socio-economic factors that influenc

99 The largest contributions to sea level rise are estimated to come from thermal expans

100 aciers and ice sheet contributions to future sea level rise are uncertain but may equal or exceed sev

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

102 mage and adaptation costs under 21st century sea-level rise are assessed on a global scale taking int

103 Although the impacts of sea-level rise are potentially large, the application an

104 rctic precipitation is not mitigating global sea level rise as expected, despite recent winter warmin

105 hmstorf presented an approach for predicting sea-level rise based on a proposed linear relationship b

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

107 tly, we find that although ocean warming and sea-level rise bring about mainly localized glacier acce

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

109 glaciers is not only contributing to global sea-level rise but also threatening freshwater supplies

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

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

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

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

114 A gain of this magnitude is enough to slow sea-level rise by 0.12 +/- 0.02 millimeters per year.

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

116 t still accelerated conditions lead to total sea-level rise by 2100 of about 0.8 meter.

117 lt may cause 0.1 to 0.25 meter of additional sea-level rise by 2100.

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

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

120 The accompanying sea-level rise can continue for more than several centur

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

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

123 offset a large fraction of ocean warming and sea-level rise caused by anthropogenic influences.

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

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

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

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

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

129 , with the onset of rapid (>1 mm per year of sea-level rise) collapse in the different simulations wi

130 With 20% of the global new-water sea level rise coming from Alaska, partitioning of mass

131 cessary for marshes to keep up with relative sea level rise, competing environmental constraints, and

132 We obtain a value for the global, eustatic sea-level rise contribution of about 3.3 meters, with im

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 that the rate of future melting and related sea-level rise could be faster than widely thought.

136 Whether wetlands continue to survive sea-level rise depends largely on how human impacts inte

137 However, estimates of their contribution to sea level rise disagree.

138 Using two climate models, we project sea level rise due to melting of mountain glaciers and i

139 ects at least comparable to the accelerating sea-level rise due to global warming.

140 Global sea level rise during deglaciation led to a rising regio

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

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

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

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

145 Under similar rates of rapid sea-level rise during the early Holocene epoch most low-

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

147 elds likely contributed 2.2 to 3.4 meters of sea-level rise during the Last Interglaciation.

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

149 location despite changes in sea level (until sea level rises enough to overcome the excess thickness

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

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

152 Global mean sea level rise estimated from satellite altimetry provid

153 7 centuries, a value similar to the rates of sea-level rise estimated for the Caribbean during a comp

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

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

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

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

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

159 e and assess the contribution of glaciers to sea level rise, excluding those in Greenland and Antarct

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

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

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

163 The total contribution to sea level rise from all ice-covered regions is thus 1.48

164 Observed acceleration indicates that sea level rise from Greenland may fall well below propos

165 Climate Change projected the contribution to sea level rise from the Greenland ice sheet to be betwee

166 increase in the ice sheet's contribution to sea-level rise from basal lubrication is projected by al

167 onse, we estimate an upper bound of 45 mm of sea-level rise from Greenland dynamics by 2100.

168 e ice sheet, suggesting that the majority of sea-level rise from Greenland dynamics during the past d

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

170 Sea-level rise from melting of polar ice sheets is one o

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

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

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

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

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

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

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

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

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

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

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

182 imate models and show that ocean warming and sea-level rise in the twentieth century were substantial

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

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

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

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

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

188 ble debate remains as to whether the rate of sea level rise is currently increasing and, if so, by ho

189 Climate change-associated sea level rise is expected to cause saltwater intrusion

190 10 m), the millennial average rate of global sea level rise is very likely to have exceeded 5.6 m kyr

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

192 This estimate of committed sea-level rise is a minimum because it ignores mass loss

193 Future sea-level rise is an important issue related to the cont

194 Sea-level rise is beginning to cause increased inundatio

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

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

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

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

199 , rapid ice-marginal changes contributing to sea-level rise may indicate greater ice-sheet sensitivit

200 retion rates everywhere equal to the rate of sea-level rise, meaning water depths and biological prod

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

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

203 48 +/- 36 km3 yr(-1), equivalent to a global sea level rise of 0.5 +/- 0.1 mm yr(-1).

204 1A), the largest of these events, produced a sea level rise of 14-18 metres over 350 years.

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

206 e lower limit to irreversible global average sea level rise of at least 0.4-1.0 m if 21st century CO(

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

208 a modest contribution to the present rate of sea-level rise of 3.0 millimeters per year.

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

210 We find that a total sea-level rise of about 2 meters by 2100 could occur und

211 As a consequence we are committed to a sea-level rise of approximately 2.3 m degrees C(-1) with

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

213 we infer a likely (68% confidence) long-term sea-level rise of more than 9 m above the present.

214 ontributed only 5.4 +/- 2.1 metres to global sea level rise, of which 0.66 +/- 0.07 metres were relea

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

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

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

218 namics in response to gradual phenomena like sea-level rise or tidal forces, but is less well-suited

219 in sediment supply, rather than in relative sea-level rise or wind regime, explains the different cr

220 An increase in the rate of sea-level rise, or a reduction in sediment supply, cause

221 ch agrees well with independent estimates of sea level rise originating from land ice loss and other

222 o domes gets lower, producing nine metres of sea level rise over 500 years.

223 GICs, contributed 1.06 +/- 0.19 mm yr(-1) to sea level rise over the same time period.

224 ng and posed a fourfold larger exposure than sea-level rise over multi-decadal time scales.

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

226 Although sea-level rise over the last century has been dominated

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

228 approximately 0.4 mm of equivalent eustatic sea level rise per year, respectively.

229 ivalent to 0.4 +/- 0.2 millimeters of global sea-level rise per year.

230 of outlet dynamics and glacier geometry for sea-level rise predictions.

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

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

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

234 loss sources in Alaska is needed to improve sea level rise projections.

235 remains the primary source of uncertainty in sea level rise projections.

236 The sea-level rise projections account for potential partial

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

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

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

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

241 aximum 'natural' (pre-anthropogenic forcing) sea-level rise rates below 2 m per century following per

242 We also find that maximum sea-level rise rates were attained within 2 kyr of the o

243 Finally, rates of sea-level rise reached at least 1.2 m per century during

244 e ice dynamics and the subsequent impacts on sea-level rise realistically.

245 ands have long been considered vulnerable to sea-level rise, recent work has identified fascinating f

246 upon seasonal and annual ice flow, and thus sea level rise, remains unclear.

247 Accurate prediction of global sea-level rise requires that we understand the cause of

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

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

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

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

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

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

254 Previous sea level rise (SLR) assessments have excluded the poten

255 +/- 18 Gt y(-1), equivalent to 0.68 mm y(-1) sea level rise (SLR) for 2003-2009.

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

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

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

259 dal wetlands experiencing increased rates of sea-level rise (SLR) must increase rates of soil elevati

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

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

262 , likely committing us to > 9 m of long-term sea-level rise (SLR).

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

264 tarctic changes thus cannot be attributed to sea-level rise, strengthening earlier interpretations th

265 Large sea-level rise, such as the approximately 100-meter rise

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

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

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

269 currently accounts for virtually all of the sea-level rise that is not attributable to ocean warming

270 For sea level rise, the CC commitment is 10 centimeters per

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

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

273 of future ice-sheet contributions to global sea-level rise, the incorporation of dynamic thinning in

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

275 able uncertainty in the prediction of future sea-level rise, this approach does not meaningfully cont

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 f this correction, we estimate that eustatic sea level rose to approximately 6-13 m above the present

282 glaciological conditions required for large sea-level rise to occur by 2100 and conclude that increa

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

284 area, leaving their overall contribution to sea level rise unclear.

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

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

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

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

289 Sea level rise will change inundation regimes in salt ma

290 In similar geologic situations, rapid modern sea level rise will initiate this process globally, and

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

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

293 ther north, the contribution of Greenland to sea-level rise will continue to increase.

294 elt water that would otherwise contribute to sea-level rise will fill existing pore space of the perc

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

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

297 ually in 2100 under 25-123 cm of global mean sea-level rise, with expected annual losses of 0.3-9.3%

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

299 ere fixed today, global-mean temperature and sea level rise would continue due to oceanic thermal ine

300 Predicted sea level rise would increase the vulnerability of low l