ライフサイエンスコーパス: flooding

1 el rise, increasing the frequency of coastal flooding.

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

3 ws sensitivity to interannual variability in flooding.

4 post-traumatic stress disorder 1 year after flooding.

5 equently lethal condition caused by airspace flooding.

6 er stability or as a result of damage due to flooding.

7 mperatures, and greatest frequency of winter flooding.

8 mmer temperature and the frequency of winter flooding.

9 and adaptation measures in cases of extreme flooding.

10 id development and an increase in storms and flooding.

11 ent of arsenic mobilization during prolonged flooding.

12 of pathogen infection either during or after flooding.

13 eeting other objectives such as reduction of flooding.

14 er into soil and reduce high flow events and flooding.

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

16 nt forage production and could help mitigate flooding.

17 nergistic way at the beginning of the acidic flooding.

18 the complex hydrometeorology associated with flooding.

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

20 and is therefore susceptible to catastrophic flooding.

21 e epoch most likely triggered by postglacial flooding.

22 of neurons demonstrated CMSP without dextran flooding.

23 n may attenuate the most negative effects of flooding.

24 ious glacier advance, recession and outburst flooding.

25 lower Mississippi River to be vulnerable to flooding.

26 quatic plant that is well adapted to partial flooding.

27 ficant even after adjustment for severity of flooding.

28 contributing factors for increased nuisance flooding.

29 crease the frequency and severity of coastal flooding.

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

31 difficult to evaluate the magnitude of paleo-flooding.

32 al periphery, that respond differentially to flooding.

33 ng the need for mitigation measures prior to flooding.

34 ea levels where plants were most stressed by flooding (114% stimulation in the + 10 cm treatment), an

35 the success of so-called low salinity water flooding, a recent enhanced oil recovery technology.

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

37 Previous studies have shown that flooding affects mental health.

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

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

40 eater understanding of the feedbacks between flooding and a river's capacity to transport sediment.

41 ity protect plants from growth inhibition by flooding and anoxia, drought, high salt, the presence of

42 arge absorptive capacity to prevent alveolar flooding and clear edema fluid.

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

44 y models are used to estimate the effects of flooding and crop failures on local population mobility

45 of these options) and tend to focus on sewer flooding and CSO alleviation while compromising on downs

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

47 Thus, the unique behavior of rice toward flooding and drought stresses has required special atten

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

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

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

51 3-14 Public Health England National Study of Flooding and Health, we compared the prevalence of sympt

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

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

54 eventually experience increased catastrophic flooding and land loss.

55 and hurricanes) and climate change (such as flooding and more extreme weather).

56 g exposure is forecasted to double following flooding and over half of the women of childbearing age

57 Rainfall variation, flooding and soil gradients strongly influenced seedling

58 Flooding and splashing of wastewater in sewers periodica

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

60 of SHYG in shoot tissue is triggered by root flooding and treatment with ET, constituting an intrinsi

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

62 bitats are subjected to frequent inundation (flooding) and are characterised by food webs that exhibi

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

64 Under all soil pHs, flooding, and draining conditions, less than 22% of Zn w

65 nes, stock market crashes, insurance claims, flooding, and earthquakes.

66 leads to acute lung injury, patchy alveolar flooding, and hypoxemia.

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

68 ng and weather events, such as storms, flash flooding, and landslides, contribute estrogen to waterwa

69 MeHg producers during the first two years of flooding, and net demethylating systems afterward.

70 e amphitheater-headed canyons by large-scale flooding approximately 46 ka, coeval with formation of B

71 ed factors, including road dust and roadside flooding are contributing to more extensive thermokarst

72 ), coastal dunes that protect the coast from flooding are largely the product of a grass introduced f

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

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

75 Both intense drought and excessive flooding are projected to increase by at least 50% towar

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

77 intensity enhancement (because of the oxygen flooding at 5 x 10(-6) Pa) was much higher with C(60)(+)

78 al Hg in the pore water for up to 5 weeks of flooding at all temperatures.

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

80 hotosynthesis was similar between sites, but flooding at the restored sites inhibited ecosystem respi

81 fluxes were more variable due to occasional flooding at the site, which both stimulated and inhibite

82 We detected no effect of flooding (at 19 sites) on this service.

83 le of natural disasters-earthquakes, El Nino flooding, beach ridge formation, and sand dune incursion

84 mes the inorganic load delivered by overbank flooding before flood protection levees were constructed

85 the ionosphere, an influx on a global scale, flooding between 30 to 43 per cent of the surface of Sat

86 Regular flooding by slightly brackish water was probably control

87 Regardless of this uncertainty, flooding by tropical cyclones will increase as a result

88 In coastal ecosystems, hurricanes and flooding can cause dramatic changes in water quality res

89 tic parameter values, the effect of antibody flooding can indeed take place.

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

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

92 icant levels of microbial SO4(2-) reduction, flooding caused increased Fe(II) and As(III) concentrati

93 ng injury are characterized by heterogeneous flooding/collapse of lung tissue.

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

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

96 CO(2) effect was enhanced under salinity and flooding conditions likely to accompany future SLR.

97 suggesting its better performance under soil flooding conditions.

98 ed before and after 884 h of continuous core flooding confirmed negligible dissolution.

99 l change in the variability and magnitude of flooding could be a major consequence of future global c

100 ure, precipitation, heat waves, drought, and flooding could impact on snail and schistosome populatio

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

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

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

104 n the absence of plants was not sensitive to flooding depth and duration.

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

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

107 muscle protein fractional synthesis rates, a flooding dose (50 mg . kg(-1) ) of l-[ring-(13) C6 ]phen

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 subjected to greater wave-induced run-up and flooding due to sea-level rise than those with deeper re

111 whether species were increasingly related as flooding duration intensified.

112 Therefore, oxygen flooding during C(60)(+) sputtering has a great potentia

113 and abiotic conditions, including history of flooding during Hurricane Sandy 7 months prior to the st

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

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

116 nage and seven were subjected to small-scale flooding during the complete study period (two sites) or

117 from Virginia through Florida record marine flooding during the mid-Pliocene.

118 The human enterprise is flooding Earth's ecosystems with exotic species.

119 hat Ar4000+ bombardment combined with cesium flooding enhances secondary ion signals by a factor of 6

120 ungal communities continue to be affected by flooding, even after relative humidity has returned to b

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

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

123 plants into natural settings that, due to a flooding event, favored I. fulva.

124 anges associated with flow during the single flooding event.

125 -3 months after the historic September, 2013 flooding event.

126 ation occurs in the natural progression of a flooding event.

127 are easily mobilized from riverbanks during flooding events and dispersed within the floodplain or t

128 accurate, and precisely dated record of cave flooding events from the northwest Australian tropics th

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

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

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

132 lakes from these fissures and previous water flooding events were presumed to have evaporated and sub

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

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

135 Global climate change has increased flooding events, which affect both natural vegetation dy

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

137 arrheal disease following heavy rainfall and flooding events.

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

139 technique with an invasive open-system core-flooding experiment and compared the results of the pre-

140 ng was carried out before and after the core-flooding experiment at a spatial voxel resolution of 27

141 cterization and geochemical data from a core-flooding experiment on a sample from the Three Fingers e

142 We present laboratory-scale core flooding experiments designed to measure CO2 endpoint re

143 Soil flooding experiments indicate that near-term changes exp

144 We performed core flooding experiments on Indiana limestone using the poro

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

146 on in cases in which whole-cell electrophile flooding fails to stimulate ARE induction prior to causi

147 iced early in the growing season followed by flooding for remainder of season, similar yields as the

148 The use of cesium flooding for the imaging of cells was also investigated

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

150 t model experiments, however, an increase in flooding frequency was found in more than half of the gr

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

152 Rain and flooding from Hurricane Katrina resulted in widespread g

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

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

155 m(2) to over 12,500 km(2) driven by seasonal flooding from the Mekong River.

156 ving shoreline that is increasingly prone to flooding from tropical cyclones.

157 d forest understory vegetation along a tidal flooding gradient.

158 Hence, cesium flooding has also a vast potential for SIMS analyses wit

159 The results indicate that flooding has modest effects on mobility that are most vi

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

161 However, crop failures unrelated to flooding have strong effects on mobility in which househ

162 ies of extreme events, including drought and flooding, have been important drivers of the long-term s

163 ly reduced leaf movement in response to root flooding in aco5 T-DNA insertion mutants.

164 thelial barrier function leading to alveolar flooding in acute lung injury (ALI) are incompletely und

165 hanism that protects the lungs from alveolar flooding in acute lung injury.

166 ities, which may result in increased risk of flooding in coastal areas.

167 curring in 2008 following heavy rainfall and flooding in eastern Uganda.

168 caused >3 feet of rainfall and catastrophic flooding in Houston, TX.

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

170 The magnitude of flooding in New York City by Hurricane Sandy is commonly

171 al fertilizer rates, along with intermittent flooding in paddy rice cropping systems.

172 owing recognition of Quaternary catastrophic flooding in the American northwest, and may imply that s

173 o assess the long-term consequences of CO(2) flooding in the subsurface from decadal observations of

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

175 Multi-centennial length phases of flooding in UK and central Europe correspond with period

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

177 In pots without rice plants, flooding increased both the concentration of dissolved S

178 nities were more phylogenetically related as flooding increased.

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

180 ricane concentrations within 2 months of the flooding induced by these hurricanes.

181 e sequencing and metabolite profiling reveal flooding-induced metabolic reprogramming specific to R.

182 floodplain soils, As may be released during flooding-induced soil anoxia, with the degree of mobiliz

183 environmental rRNA gene sequences currently flooding into databases such as GenBank show that these

184 which is likely to affect the probability of flooding into the future.

185 r identical conditions, but using continuous flooding irrigation was 163 +/- 23 mug kg(-1).

186 when compared to rice grown under continuous flooding irrigation.

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

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

189 Flooding is detrimental for nearly all higher plants, in

190 Flooding is detrimental for plants, primarily because of

191 Flooding is expected to increase in frequency and severi

192 soils and farther from rivers where overland flooding is less likely and downslope flow paths and neg

193 This flooding is thought to structure many of the critical ec

194 of ion bombardment with simultaneous cesium flooding is valid not only for monatomic ion bombardment

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

196 ariability (El Nino southern oscillation and flooding) is quite localized: There is a climate-sensiti

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

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

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

200 Effects for year, location and flooding management were also statistically significant,

201 Shifts in the frequency and magnitude of flooding may be an underappreciated but critical factor

202 However, flooding may increase methane (CH4) emissions.

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

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

205 Widespread flooding occurred across northwest Europe during the win

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

207 Severe flooding occurred in the midwestern United States in 200

208 d the community well to cope with comparable flooding occurring 10 y later.

209 g these findings together with the predicted flooding of 1661 km(2) of wetlands along the NC coast by

210 oodway during the Mississippi and Ohio River Flooding of 2011 as a scientifically unique stress exper

211 ase of colloidal and dissolved Hg induced by flooding of a contaminated riparian soil, we performed l

212 a due to Penicillium species after prolonged flooding of a Thai hospital.

213 mics and solid-phase speciation of As during flooding of an As-contaminated soil.

214 rkeley Pit lake in Butte, Montana, formed by flooding of an open-pit copper mine, is one of the world

215 hydrates during deglaciation and concomitant flooding of continental shelves and interior basins.

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

217 lect the greater inflow from tributaries and flooding of natural wetlands that occurred at this time.

218 dditives produce EEM signatures with notable flooding of peaks P, M(1), M(2), and H, relatively highe

219 te lung injury (ALI) is characterized by the flooding of the alveolar airspaces with protein-rich ede

220 ce levels of pro-inflammatory cytokines, and flooding of the alveolar spaces with protein-rich edema

221 er million years, calibrated to the earliest flooding of the East China Sea shelf (70-140 kya), revea

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

223 marked decrease in (QO2) and the subsequent flooding of the lens core with oxygen.

224 Cessation of the outbreak coincided with flooding of the mine.

225 e of carbon, possibly with contribution from flooding of the Siberian continental shelf during meltwa

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

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

228 we sought to determine the impact of extreme flooding on ARG reservoirs in river water and sediment.

229 landers sent to investigate sites of ancient flooding on Mars have predominantly found lava at the su

230 changes in northern ecosystems and reservoir flooding on methylmercury production and bioaccumulation

231 beneficial effect of cesium implantation or flooding on the enhancement of negative secondary ion yi

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

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

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

235 8 to 305.4 Mm(3), which indicates that water flooding operations may use up to 167.0 Mm(3) per year.

236 d injection program wells, and used in water flooding operations.

237 -alveolar vessels but did not cause alveolar flooding or blood gas abnormalities.

238 in of plains on Mercury, whether by volcanic flooding or impact ejecta ponding, has been controversia

239 Responses to flooding or waterlogging involve ethylene signaling, whi

240 ving in homes that had been damaged by rain, flooding, or both.

241 of perception in the rapid stream of images flooding our eyes.

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

243 Sensory flooding, particularly during auditory stimulation, is a

244 ine and acidified paddy soils, under various flooding periods and draining conditions, by employing s

245 though the soils were subjected to different flooding periods and draining conditions.

246 s that were inundated only during paddy rice flooding periods.

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

248 with (14)C-lableled TCE and used a multistep flooding procedure that quantified the mass of (14)C-TCE

249 The method of network flooding proves to be a useful, practical approach towar

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

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

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

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

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

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

256 We observed that extreme flooding resulted in an increase of approximately 30% in

257 Flooding resulting from the bursting of dams formed by l

258 issues: persistent groundwater overdraft and flooding risks.

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

260 ed 200-250 km downstream from the dam during flooding season campaigns may reflect the greater inflow

261 obal sea level predicted to rise and coastal flooding set to become more frequent and intense, high-r

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

263 events (e.g., drought- and heat-stress, and flooding), should also be considered in future predictio

264 Small-scale flooding showed no or moderate changes in MeHg yield, ma

265 By contrast, R. palustris uses the early flooding signal ethylene to increase survival by regulat

266 ethylene that makes it an early and reliable flooding signal.

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

268 end, we have performed a molecular dynamics "flooding" simulation on a membrane-bound structural mode

269 decomposition rates are inversely related to flooding, SOM decomposition in the absence of plants was

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

271 nules and other mRNPs that accumulate during flooding stress responses.

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

273 ed traits allowing them to survive prolonged flooding, such as species of the genus Rorippa, close re

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

275 Flooding survival strategies have been studied in Oryza

276 lly expressed ERF-VII genes enable effective flooding survival strategies in rice, the constitutive a

277 dentify mechanisms that mediate the distinct flooding survival strategies of two related wild dicot s

278 hese results provide molecular resolution of flooding survival strategies of two species occupying di

279 nserved primarily across genotypes, although flooding susceptibility-associated and genotype-specific

280 We have conducted a core flooding test with a quartzarenite plug of Lower Cretace

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

282 ng this knowledge into medical therapies are flooding the field as well.

283 Flooding the intercellular air spaces of leaves with wat

284 iation led to a rising regional water table, flooding the oxidized soils surrounding Tulane.

285 esis that alternate wetting and drying (AWD--flooding the soil and then allowing to dry down before b

286 he sill of the Bosphorus Strait was reached, flooding the vast northwestern BS shelf and deeply affec

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

288 d flood layers in order to extend records of flooding to the city beyond the instrumental dataset.

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

290 Reporting of wastewater disposal and water flooding volumes could be used to further develop state-

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

292 Although the flooding was deemed a 'wake-up call' to the impacts of c

293 In rosette plants, root flooding (waterlogging) triggers rapid upward (hyponasti

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

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

296 This paper introduces the theory of network flooding, which aims to address the problem of network m

297 e contents, Cd may remain labile during soil flooding, which enhances the risk for Cd transfer into r

298 how potential for reducing the likelihood of flooding, whilst providing food production under conditi

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

300 the levels recorded at the end of the third flooding year.