ライフサイエンスコーパス: flood

1 treamwater composition before and during the flood.

2 were taken as evidence to verify an outburst flood.

3 mers following bankfull, bed-scouring winter floods.

4 abundant in this basin but not consistently flooded.

5 el rise, increasing the frequency of coastal flooding.

6 lower Mississippi River to be vulnerable to flooding.

7 crease the frequency and severity of coastal flooding.

8 ious glacier advance, recession and outburst flooding.

9 quatic plant that is well adapted to partial flooding.

10 ficant even after adjustment for severity of flooding.

11 contributing factors for increased nuisance flooding.

12 on of a whole new secondary root system upon flooding.

13 difficult to evaluate the magnitude of paleo-flooding.

14 al periphery, that respond differentially to flooding.

15 ng the need for mitigation measures prior to flooding.

16 nt temperature, heavy rainfall, drought, and flooding.

17 post-traumatic stress disorder 1 year after flooding.

18 ws sensitivity to interannual variability in flooding.

19 ooded (n=622) to analyse displacement due to flooding.

20 ose flooded, but not displaced, 1 year after flooding.

21 n may attenuate the most negative effects of flooding.

22 ollowing the flood but recovered to near pre-flood abundances by ten months post-flood at both a pris

23 For road flooding, adaptation provided an annual savings of 80-10

24 Major floods adversely affect water quality through surface ru

25 llected 1 year after the flooding event from flood-affected postcodes in five counties in England.

26 Previous studies have shown that flooding affects mental health.

27 This rare flood afforded the opportunity to gain deeper insight in

28 ssess the frequency and location of nuisance flooding along the eastern seaboard of North America.

29 populations established rapidly after first flooding, although colonisation was ongoing throughout t

30 hanges in the frequency of extreme events of flood and drought in recent decades and in the magnitude

31 The study included major flood and drought years, where wetting and drying treatm

32 stion our reconstruction of a large outburst flood and its possible relationship to China's Great Flo

33 This study uses high-resolution flood and loss models to quantify the impacts of coastal

34 be related to ancient accounts of the Great Flood and origins of the Xia dynasty.

35 d its possible relationship to China's Great Flood and the Xia dynasty.

36 However, the historicity of the flood and Xia remain controversial.

37 of ABA metabolism and signaling in roots of flooded and water stressed plants of Carrizo citrange re

38 ltural practices, act as input into weather, flooding and climate models and inform water resource po

39 e oxygen species (ROS) in plant cells during flooding and directly after subsidence, during which the

40 y modulation of future TWS impacts including flooding and drought.

41 avily populated regions to increased coastal flooding and erosion hazards.

42 rous and increasing threats, such as coastal flooding and erosion, saltwater intrusion and wetland de

43 3-14 Public Health England National Study of Flooding and Health, we compared the prevalence of sympt

44 eas will be subject to more frequent extreme flooding and hurricanes.

45 ces of land use and climate change including flooding and increased sediment, nutrient, and chemical

46 eventually experience increased catastrophic flooding and land loss.

47 Rainfall variation, flooding and soil gradients strongly influenced seedling

48 s disorder between participants displaced by flooding and those flooded, but not displaced, 1 year af

49 from diverse environmental stresses such as flooding and vegetative shade.

50 exist, the global scale effects of droughts, floods and extreme temperature on crop production are ye

51 e ultimate cause for Milu dispersal, whereas floods and human disturbance are proximate causes.

52 differences in inflammation, consolidation, flooding, and atelectasis.

53 etagenomic profiles of ARGs before and after flooding, and investigated 23 antibiotics and 14 metals

54 While both types of flooding are likely to increase in the future, only nuis

55 e find that the areas impacted by freshwater flooding are nearly equally divided between coastal and

56 The ecological consequences of flooding are the combined result of species-specific pla

57 A similar correlation between %flooded area and MeHg concentrations was not observed in

58 concentration was positively correlated to %flooded area upstream of the sampling site in the Solimo

59 with polar warming have led to later winter floods around the North Sea and some sectors of the Medi

60 ion, water samples were collected during the flood at 5 locations along the South Platte River and fr

61 near pre-flood abundances by ten months post-flood at both a pristine site and at a site historically

62 limate variability, influence river flow and flooding at the global scale.

63 part to the limited number of high-magnitude floods available for study in the instrumental record.

64 onstitute one of Earth's largest continental flood basalt provinces, whose eruption played a role in

65 n to be stratigraphically tied to a specific flood basalt unit, strengthening the case for volcanic H

66 ophic global environmental change than their flood basalt- and/or dike-dominated counterparts.Althoug

67 -bearing siderite formed in experiments with flood basalt.

68 s between magma and coal during the Siberian flood-basalt eruptions released large amounts of CO2 and

69 As floods become more frequent and severe in the future, gr

70 ely implemented-also offer water filtration, flood buffering, soil health, biodiversity habitat, and

71 otal bulk water ARGs decreased following the flood but recovered to near pre-flood abundances by ten

72 participants displaced by flooding and those flooded, but not displaced, 1 year after flooding.

73 that frequency and severity of droughts and floods can have characteristic effects on the exchange o

74 ence of a residual ABA signaling in roots of flooded Carrizo citrange seedlings.

75 adventitious root development in response to flooding (case study 1), nutrient deficiency (case study

76 The largest source of damages was road flooding caused by increased precipitation followed by d

77 tated routing via storm drains, ditches, and flood channels.

78 the occurrence of ABA signaling in roots of flooded citrus seedlings.

79 ent facility effluent) under normal-flow and flood conditions.

80 rce the role of this ABA receptor under soil-flooding conditions and explain the expression of certai

81 they form a signature readout of prevailing flooding conditions and subsequent adaptive responses.

82 suggesting its better performance under soil flooding conditions.

83 n Typha latifolia L. colonizing a frequently flooded contaminated soil were studied.

84 rs ago an ocean fed by enormous catastrophic floods covered most of the Martian northern lowlands.

85 ed a different induction in response to soil flooding (CsPYL5) or drought (CsPYL8).

86 n a process termed controlled salinity water-flooding (CSW).

87 f new sequencing applications and promise to flood current databases with raw data.

88 s positive and negative relations with total flood damage and damage per unit wealth in 20 and 16 sta

89 Understanding historical changes in flood damage and the underlying mechanisms is critical f

90 In this study, a detailed assessment of flood damage for 1950-1999 is conducted at the state lev

91 Overall, flood damage in 34 out of 48 investigated states can be

92 n important factor contributing to increased flood damage in central US while urbanland exhibits posi

93 A considerable increase in flood damage in CONUS is recorded for the study period w

94 states, highlighting the potential of future flood damage prediction based on climate change and soci

95 In extreme cases, 76% of flood damage variations can be explained in some states,

96 (VIC) model can explain a larger portion of flood damage variations than precipitation in 84% of the

97 and urban area to explore the relations with flood damage.

98 ands in the northeastern USA on (i) regional flood damages by Hurricane Sandy and (ii) local annual f

99 that wetlands avoided $625 Million in direct flood damages during Hurricane Sandy.

100 can be used to reveal the paleohydrology of flood deposits in the stratigraphic record, leading to i

101 Here we quantified the effects of flooding depth and duration on SOM decomposition by expo

102 Extreme precipitation such as the flooding described here may pose significant challenges

103 vivors, who experienced the same coal mining flood disaster.

104 rd, leading to improved mitigation of future flooding disasters.

105 eir brims, a large and monotonic increase in flood discharge is predicted as the canyon was progressi

106 Flood discharges are often estimated by assuming that th

107 o estimate the potential influence of future flood disturbance on geomorphic processes controlling th

108 cale analysis of the main drivers of coastal flooding due to large-scale oceanographic factors.

109 global-scale estimates of increased coastal flooding due to sea-level rise have not considered eleva

110 whether species were increasingly related as flooding duration intensified.

111 acity, thereby elevating the risk of a major flood during subsequent rainstorms.

112 ontinental shelves during ice ages and their flooding during interglacials have been hypothesized to

113 ate reduction, often accompanying (sea)water flooding during secondary oil recovery.

114 evices and used remote sensing data to model flood dynamics during three consecutive winters (2012-20

115 In the 6-12 months preceding a flood, El Nino generates a positive precipitation anomal

116 l rise scenarios we consider, the 1-in-500-y flood event increases from 3.4 m above mean tidal level

117 sland, Australia, before, during and after a flood event.

118 -sectional survey collected 1 year after the flooding event from flood-affected postcodes in five cou

119 An early summer flooding event in a grassland biodiversity experiment in

120 anges associated with flow during the single flooding event.

121 od risk from the full set of all significant flood events associated with U.S. landfalling TCs from 2

122 ain aquifer was high-concentration, overbank flood events in winter that directly recharged groundwat

123 During flood events, AREE anomalies progressively disappeared a

124 We also used a recent series of flooding events in Yalong Bay, southern China, to test t

125 ed surges in parasite prevalence during past flooding events indicate that the ongoing global warming

126 for changes in the frequency and duration of flooding events to result in nonlinear population respon

127 the globe have the potential for very large flooding events with low probabilities (unbounded tails)

128 nities (community coalescence), for example, flooding events, host excretion, and soil tillage [1, 2]

129 has increased the frequency and severity of flooding events, with significant negative impact on agr

130 wind erosion (dust) and rainfall inundation (flood) events.

131 A river flooding example using three insect species (a fast life

132 p in knowledge, we conduct a suite of column flood experiments through silica sand, systematically va

133 We found that species-specific responses to flooding explained most of the variation in occurrence f

134 ilability, whereas in Nepal preparedness for flood extremes should be the policy priority.

135 In contrast, under the assumption that floods filled canyons to their brims, a large and monoto

136 ges are often estimated by assuming that the floods filled the canyons to their brims with water; how

137 d likely impact rural fisher livelihoods and flooded forest biodiversity.

138 ng prevented tree regeneration in frequently flooded forest islands.

139 he world, and predicting increases in future flood frequency.

140 t 49% are highly susceptible to increases in flooding frequency due to sea-level rise.

141 cs, will experience the largest increases in flooding frequency.

142 tal cities vulnerable to SLR are at risk for flooding from multiple drivers (e.g., extreme coastal hi

143 sessment approach that accounts for compound flooding from river flow and coastal water level, and we

144 d forest understory vegetation along a tidal flooding gradient.

145 arthropods living in aqueous or temporarily flooded habitats including water-walking insects or wate

146 , we find that the return period of a 2.25-m flood has decreased from approximately 500 y before 1800

147 nal and sedimentary features associated with flooding have been documented in both modern and past ca

148 Here, we propose a bivariate flood hazard assessment approach that accounts for compo

149 Common flood hazard assessment practices typically account for

150 hat the likelihood of increased or decreased flood hazard during ENSO events is much more complex tha

151 We find that New York City's flood hazard has increased significantly over the past t

152 roach may not appropriately characterize the flood hazard if there are compounding effects.

153 The flood hazard in New York City depends on both storm surg

154 Coastal flood hazard varies in response to changes in storm surg

155 tology to estimate the temporal evolution of flood hazard.

156 asingly common and pose significant outburst flood hazards if the dam is breached.

157 an innovative tool for assessing compounding flood hazards in a warming climate.

158 The 2.25-m flood height is permanently exceeded by 2280-2300 for sc

159 ver, projected sea-level rise causes overall flood heights associated with tropical cyclones in New Y

160 reatly compared with preindustrial or modern flood heights.

161 impact on the magnitude and timing of river floods; however, no consistent large-scale climate chang

162 er quality during the September 2013 extreme flood in the South Platte River, Colorado, USA.

163 Wu et al reported an enormous flood in the upper Yellow River that destroyed the Lajia

164 ms hit the UK leading to record rainfall and flooding in many regions including south east England.

165 ms during the 2013-2014 winter led to record flooding in the UK.

166 n reconnection and the frequency of overbank flooding in winter have the potential to temporarily sto

167 the Pleistocene by the catastrophic Missoula floods in eastern Washington, USA.

168 We analyzed the timing of river floods in Europe over the past five decades, using a pan

169 Record-breaking floods in September 2013 caused massive damage to homes

170 l moisture maxima have led to earlier winter floods in western Europe.

171 nities were more phylogenetically related as flooding increased.

172 zed by features associated with catastrophic flooding indicates final breaching of the Strait by high

173 e and contributed to stream loading, and (3) flood-induced groundwater discharge mobilized soluble co

174 and chromatin-binding proteins (readers) are flooded into the system.

175 uakes reduced channel capacity and increased flood inundation.

176 Crop yield loss due to flooding is a threat to food security.

177 ely to increase in the future, only nuisance flooding is an early indicator of areas that will eventu

178 Flooding is detrimental for nearly all higher plants, in

179 Flooding is expected to increase in frequency and severi

180 tion of fluid shear velocity associated with floods is universal, indicating that self-organization o

181 ts, hypoxia (low oxygen, which occurs during flooding) is directly sensed by the Cys-Arg/N-end rule p

182 inearly over time on the six most frequently flooded islands, while salt marsh herbs and shrubs repla

183 ceptions concerning geologic evidence of the flood, its timing and magnitude, and the complex social-

184 For example, flooding large areas for hydroelectric dams converts mou

185 e RAV specifically increased occurrence when flooding lasted for longer time periods, because large R

186 raps large igneous province, from dominantly flood lavas to sill intrusions.

187 authors propose that the abrupt change from flood lavas to sills resulted in the heating of sediment

188 ns tell of the successful control of a Great Flood leading to the establishment of the Xia dynasty an

189 y mature but emerge only when the plant gets flooded, leading to the formation of a whole new seconda

190 canically-induced suppression of Nile summer flooding led to societal unrest in Ptolemaic Egypt (305-

191 nalysis suggests that in many regions, local flood level determinations should consider the joint eff

192 water-level variability, i.e., short-tailed flood-level distributions, located mainly in the Tropics

193 Informative flash flood-like disturbances that eliminate most gastrointest

194 in the media and of warnings, much of the TC flood losses are instead freshwater-driven, often extend

195 estimates a 16% average reduction in annual flood losses by salt marshes with higher reductions at l

196 ges by Hurricane Sandy and (ii) local annual flood losses in Barnegat Bay in Ocean County, New Jersey

197 problem (e.g. spatiotemporal variability in flood magnitude and the relative influence of waves, tid

198 , the nonlinearity between precipitation and flood magnitude motivates the need for estimation of his

199 arge-scale climate change signal in observed flood magnitudes has been identified so far.

200 We also further discuss how this flood may be related to ancient accounts of the Great Fl

201 The frequency and duration of such floods may be more important to population dynamics than

202 ental illnesses studied, and the severity of flooding might be the reason for some, but not all, of t

203 m services include drinking water provision, flood mitigation, habitat provision and carbon sequestra

204 s restricted to individuals whose homes were flooded (n=622) to analyse displacement due to flooding.

205 nd in response to stress conditions, such as flooding, nutrient deprivation, and wounding.

206 t the existence of a clear climate signal in flood observations at the continental scale.

207 Extensive flooding occurred during the winter of 2013-14 in Englan

208 Linking flood occurrence to persistent modes of climate variabil

209 tanding of the climatic controls that govern flood occurrence.

210 Despite the flood of data expected from this technology, the data an

211 Between 1992 and 2014, tidal flooding of forest islands increased by 22%-117%, corres

212 ntary features resulting from the disastrous flooding of the Kinu River, central Japan, in September

213 For small scale "nuisance flooding," often associated with high tides, recent incr

214 urge models to estimate increases in coastal flooding on a continuous global scale.

215 d, a levee in Joso City, causing destructive flooding on the surrounding floodplain.

216 however, suggesting that positive effects of floods on annual algal production were primarily mediate

217 ariability mediates the formation of extreme floods on one of the world's principal commercial waterw

218 it can be difficult to assess the effects of floods on streamwater chemistry because of challenges co

219 ring the main phase of the eruption, but was flooded once the eruption had finished.

220 r one driver at a time (e.g., either fluvial flooding only or ocean flooding only), whereas coastal c

221 (e.g., either fluvial flooding only or ocean flooding only), whereas coastal cities vulnerable to SLR

222 Responses to flooding or waterlogging involve ethylene signaling, whi

223 measure of seasonal predictability of future floods or droughts in a changing climate.

224 This could cause enhanced floods or droughts, stronger soil erosion and nutriment

225 is at odds with the discharges expected for floods originating from glacial lake outbursts.

226 eived a warning more than 12 h in advance of flooding (p=0.04 for depression, p=0.01 for post-traumat

227 Because flooded paddy fields are efficient denitrification biore

228 Quantitation stability of a (68)Ge flood phantom was demonstrated within 0.34%.

229 ylene accumulating to high concentrations in flooded plant organs and by changes in light quality and

230 In roots of flooded plants, restoration of control ABA levels after

231 w that during the acute phase of the 2013-14 floods, potential feeding areas decreased dramatically a

232 Improving flood predictability, preparedness, and response at seas

233 found that salt stress from increased tidal flooding prevented tree regeneration in frequently flood

234 imits and communities continue to develop in flood-prone areas.

235 tropical rivers, rainfall drives a periodic flood pulse fueling fish production and delivering nutri

236 fied variance components of the Mekong River flood pulse that predict yield in one of the largest fre

237 t decades and in the magnitude of the annual flood pulse, a phenomenon that influences virtually all

238 Hydropower will modulate this flood pulse, thereby threatening food security.

239 eld: prolonged low flows followed by a short flood pulse.

240 utaries during distinct phases of the annual flood-pulse.

241 Mississippi River floods rank among the costliest climate-related disaster

242 Frequencies of tidal flooding, rates of tree mortality, and understory compos

243 When floods ravage Asian monsoon regions in summer, megadroug

244 als as putative selective agents during post-flood recovery.

245 Soil flooding reduces root abscisic acid (ABA) levels in citr

246 ptember 2013, grasses were unaffected by the flood regardless of plant diversity, and legumes were se

247 Flood-related damages represent a large portion of these

248 , because there are indications that, before flooding, relative head size did not differ between futu

249 However, the majority of past flooding research has focused on individual model specie

250 Germany, provided the opportunity to assess flooding responses of 60 grassland species in monocultur

251 ion and land use history and determined that flooding restoration could promote greater C accumulatio

252 Flooding resulting from the bursting of dams formed by l

253 e increases with increasing pore-water Si in flooded rice paddy soils.

254 architecture of the secondary root system in flooded rice plants is controlled not only by altered ga

255 to amplify or mitigate against the increased flood risk caused by sea-level rise.

256 (SLR) on human settlements is an increase in flood risk due to an increase in the intensity and frequ

257 he potential future changes in TC freshwater flood risk due to changing climate pattern and urbanizat

258 omprehensive assessment of the TC freshwater flood risk from the full set of all significant flood ev

259 ding to distinct patterns of aggradation and flood risk in the densely populated, low-relief Ganga Pl

260 e this actuality, knowledge of TC freshwater flood risk is still limited.

261 Findings have important implications for flood risk management, insurance and resilience.

262 ability to near- and long-term forecasts of flood risk.

263 f better rain-data management, urban pluvial flood-risk management and forecasting, drinking water an

264 The impact of reduced ABA levels in flooded roots on CsPYL5 expression along with its higher

265 When plants encounter soil water logging or flooding, roots are the first organs to be confronted wi

266 ties between forested areas and periodically flooded savannas and grasslands.

267 nd experiments suggested that bed-mobilizing floods scour away overwintering grazers, releasing algae

268 ring the snow-free, snow-covered, and spring-flood seasons.

269 e frequent and severe in the future, growing flood-sensitive plants in higher-diversity communities a

270 ecline of coral reefs, coastal defences from flooding, shifting fish stocks and the emergence of new

271 hways, in interaction with the other gaseous flooding signals.

272 rease mid- and late-21st-century mean annual flood size by 17% and 28%, respectively.

273 Increased flood size could alter stream habitats used by Pacific s

274 lained by predicted increases in mean annual flood size.

275 e of geomorphic channel responses to altered flood size.

276 In a flood-specific deployment, passive sampler TWA concentra

277 tween darkness and low-oxygen constraints of flooding stress and demonstrates that early transcriptom

278 ent, pervasive, and reliable signal of early flooding stress, most likely in tight interaction with t

279 evated (p < 0.01) in samples associated with flooding surfaces, yet the temporal trends of parasite p

280 Our results have implications for flood susceptibility, forecasting and mitigation, includ

281 am versus downstream before and after severe flooding that occurred in Kasese District, Western Regio

282 species might be most affected, however, by floods that exceed a critical threshold.

283 In many gravel-bedded rivers, floods that fill the channel banks create just enough sh

284 Without Rac1, residual milk and cell corpses flood the ductal network, causing gross dilation, chroni

285 e central in the acute-phase response, which floods the circulation with defensive proteins during di

286 eratures have led to earlier spring snowmelt floods throughout northeastern Europe; delayed winter st

287 tions, and found clear patterns of change in flood timing.

288 reactive transport, from low salinity water flooding to fracking brine leakage.

289 can provide timely warnings of the impending floods to downstream residents.

290 ir distribution, extent, volume, interannual flood variability and disturbance levels.

291 Here we show a suppression of Nile summer flooding via the radiative and dynamical impacts of expl

292 ideas of a more gradual extinction involving flood volcanism or climatic changes.

293 INTERPRETATION: Displacement after flooding was associated with higher reported symptoms of

294 e samples after twenty pore volumes of brine flooding.We found a wide range of contact angles with va

295 species were less negatively affected by the flood when grown in higher-diversity plots in July 2013.

296 For catastrophic coastal flooding, when wind-driven storm surge inundates large a

297 IPCC's 1.5 degrees C target, risks of flash floods will exacerbate on top of the current incapabilit

298 the Thames river valley there was widespread flooding, with clean-up costs of over pound1 billion.

299 of maximum growing season GPP in subsequent flood years by 15% compared to control plots.

300 her than air temperature, and higher FCH4 in flooded years was thus equally due to increased methane