ライフサイエンスコーパス: flooding

1 both the risks and benefits associated with flooding.

2 network percolation under the disturbance of flooding.

3 h inhabits moist sediments that are prone to flooding.

4 el rise, increasing the frequency of coastal flooding.

5 lower Mississippi River to be vulnerable to flooding.

6 crease the frequency and severity of coastal flooding.

7 lenges include rising temperatures and flash flooding.

8 post-traumatic stress disorder 1 year after flooding.

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

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

11 n may attenuate the most negative effects of flooding.

12 ious glacier advance, recession and outburst flooding.

13 quatic plant that is well adapted to partial flooding.

14 ficant even after adjustment for severity of flooding.

15 contributing factors for increased nuisance flooding.

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

17 difficult to evaluate the magnitude of paleo-flooding.

18 al periphery, that respond differentially to flooding.

19 ng the need for mitigation measures prior to flooding.

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

21 ws sensitivity to interannual variability in flooding.

22 equently lethal condition caused by airspace flooding.

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

24 mperatures, and greatest frequency of winter flooding.

25 mmer temperature and the frequency of winter flooding.

26 and adaptation measures in cases of extreme flooding.

27 ating sea-level rise, and increasing coastal flooding.

28 that MIS11 ice loss was coupled with marine flooding.

29 risk and an increased likelihood of fluvial flooding.

30 osure to some extent, and highly tolerant to flooding.

31 and, hence, combined stress by salinity and flooding.

32 otentially mobilize residual oil after water flooding.

33 people live on deltas and their exposure to flooding.

34 extreme water levels can double the odds of flooding.

35 n to mitigate the societal impacts of future flooding.

36 he global scale and responsive to periods of flooding.

37 better understanding of wave-driven nuisance flooding.

38 of which ~73% is caused by surface and river flooding.

39 o 60-fold for toxic equivalency (TEQ) during flooding.

40 rated by three mechanisms: (1) direct marine flooding, (2) storm-drain backflow, and (3) groundwater

41 g a giant tsunami that poured over the coast flooding 500 km alongshore the Mexican Pacific coast and

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

43 and its subsequent mineralization upon back-flooding-a common feature of newly flooded impoundments.

44 While recent increases in flooding across the world have been partly attributed to

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

46 Previous studies have shown that flooding affects mental health.

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

48 fall, and then real-time updates of expected flooding along the typhoon's path.

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

50 rofitability of so-called low salinity water flooding, an enhanced oil recovery methodology.

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

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

53 itnessing a regime shift in tropical cyclone flooding and associated ecosystem impacts.

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

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

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

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

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

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

60 e important coastal processes that determine flooding and erosion.

61 3-14 Public Health England National Study of Flooding and Health, we compared the prevalence of sympt

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

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

64 es and ecosystems from rising seas and storm flooding and influence the stability of barrier islands

65 eventually experience increased catastrophic flooding and land loss.

66 999, causing catastrophic human impacts from flooding and leading to major alterations of water quali

67 effects of global warming, extreme weather, flooding and other consequences of climate change on mic

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

69 also explore the proton path using our water flooding and protein dipole Langevin dipole semimacrosco

70 avulsions in meandering rivers often produce flooding and sediment deposition during channel construc

71 Rainfall variation, flooding and soil gradients strongly influenced seedling

72 Flooding and splashing of wastewater in sewers periodica

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

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

75 We find that Mississippi River flooding and warm season droughts detrimental to agricul

76 ffect against cases during the monsoon, when flooding and water contamination are more likely.

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

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

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

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

81 iotic stresses, including drought, salinity, flooding, and temperature stress.

82 lone hazards: peak sustained wind, rainfall, flooding, and tornadoes.

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

84 change continues to expand, and the risks of flooding are increasing.

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

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

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

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

89 These findings have implications for urban flooding as well as hydroclimatological studies.

90 luding recent increases in precipitation and flooding associated with tropical cyclones.

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

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

93 nce that several areas experience noticeable flooding at tide heights lower than existing flood thres

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

95 River deltas are especially vulnerable to flooding because of their low elevations and densely pop

96 endpoint scenarios, such as the increase in flooding by 2050 or 2100.

97 pulation and 46% of global assets at risk of flooding by 2100.

98 600,000 people could be impacted by dynamic flooding by 2100; a three-fold increase in exposed popul

99 ected to be a significant change in episodic flooding by the end of the century are identified and fo

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

101 tems and where intense rainfall and seasonal flooding can result in considerable aquatic C export (Si

102 pitation, resulting in localized droughts or flooding, can erode the base of freshwater food webs, wi

103 Tertiary EOR, including surfactant flooding, can potentially mobilize residual oil after wa

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

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

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

107 Erratic rainfall leading to flash flooding causes huge yield losses in lowland rice.

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

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

110 suggesting its better performance under soil flooding conditions.

111 itions, the lateral valleys formed upon back-flooding-corresponding to ~30% of the Santo Antonio rese

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

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

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

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

116 nts conducted in a natural field with 3-5 cm flooding depths, control and pretreated seeds of Ciheran

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

118 Flooding detected with synthetic aperture radar (>91% ac

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

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

121 rojections, we find that the odds of extreme flooding double approximately every 5 years into the fut

122 same sediment cores to evaluate the role of flooding, drought, and environmental degradation in Caho

123 Flooding due to extreme weather threatens crops and ecos

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

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

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

127 whether species were increasingly related as flooding duration intensified.

128 G1 and AG2 QTLs associated with tolerance of flooding during germination, together with seed pre-trea

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

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

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

132 arm and wet climate persisted even after the flooding ended, but its duration cannot be determined by

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

134 arch concentration decreased gradually under flooding especially in the tolerant checks and in AG1 +

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

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

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

138 anges associated with flow during the single flooding event.

139 -3 months after the historic September, 2013 flooding event.

140 construct a fascinating timeline of episodic flooding events (ranging from 3.7 to 3.6 Ga to ca. 2.0 G

141 events and is known historically for cyclic flooding events and, within the last 20 years, for groun

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

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

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

145 h can exacerbate nutrient export problems as flooding events intensify in the future climate.

146 A network of urban roads resilient to flooding events is essential for the provision of public

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

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

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

150 ommonly associated with intense rainfall and flooding events, themselves often driven by large-scale

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

152 arrheal disease following heavy rainfall and flooding events.

153 n and natural systems, predominantly through flooding events.

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

155 Soil flooding experiments indicate that near-term changes exp

156 Microfluidic flooding experiments were conducted to evaluate how alka

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

158 Here a method is developed that identifies flooding extents and infrastructure vulnerabilities that

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

160 rby Quelccaya ice core records indicate lake flooding followed a pronounced wet period beginning ~152

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

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

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

164 So far, estimates of future coastal flooding frequency focus on endpoint scenarios, such as

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

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

167 le control, which allows rice to distinguish flooding from other SUB1A-1-regulated stresses.

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

169 d forest understory vegetation along a tidal flooding gradient.

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

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

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

173 focus on drought, high and low temperature, flooding, herbivore, and pathogen stresses.

174 oncern in agricultural soils especially when flooding (hypoxic conditions) results from over irrigati

175 sing high-resolution historical data of road flooding in Harris County during Hurricane Harvey in 201

176 f increasing economic losses associated with flooding in many parts of the world, including Europe(2)

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

178 temperatures, increased rainfall, and higher flooding in the Chobe region during the rainy season.

179 c rivers (ARs) cause heavy precipitation and flooding in the coastal areas of many mid-latitude conti

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

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

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

183 nities were more phylogenetically related as flooding increased.

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

185 N-degron pathway and mediates adaptation to flooding-induced hypoxia.

186 2+), Mn(2+), Co(2+), or Zn(2+) Consequently, flooding infected cells with either Mn(2+) or Zn(2+) all

187 ndscape factors, namely the coverage of post-flooding, irrigated and rain-fed croplands, had weak pos

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

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

190 Flooding is detrimental for nearly all higher plants, in

191 Flooding is detrimental for plants, primarily because of

192 Flooding is expected to increase in frequency and severi

193 underestimating societal exposure to coastal flooding is greater for smaller SLR scenarios, up to a s

194 Coastal flooding is increasingly common in many areas.

195 Sea-level rise (SLR) induced flooding is often envisioned as solely originating from

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

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

198 y of vulnerable assets and present-day tidal flooding issues.

199 tance significantly, indicating that neither flooding itself, nor seawater sulfate, contributed great

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

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

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

203 lobal population exposed to tropical cyclone flooding live on deltas, with 92% (28 million) in develo

204 microbial communities for bioremediation by flooding local populations with catabolic genes for petr

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

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

207 (extreme heat, fire, drought), hydrological (flooding), meteorological (hurricanes), and geophysical

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

209 tions might currently be exposed to nuisance flooding not identified via standard measures.

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

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

212 re, and vegetation in which both drought and flooding occurred in excess (14-81% precipitation depart

213 colation process in which the probability of flooding of a road segment depends on the degree to whic

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

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

216 ognize valleys, based on the pattern of lava flooding of tesserae margins by adjacent plains volcanis

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

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

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

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

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

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

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

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

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

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

227 Responses to flooding or waterlogging involve ethylene signaling, whi

228 Extreme flooding over southern Louisiana in mid-August of 2016 r

229 ed to obtain projections of episodic coastal flooding over the coming century.

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

231 in the southern circum-Chryse region, their flooding pathways include hundreds of kilometers of chan

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

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

234 ydrographs provide early warning of possible flooding prior to typhoon landfall, and then real-time u

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

236 Flooding reduced seedling emergence of all genotypes, th

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

238 tury will see significant changes to coastal flooding regimes (where present-day, extreme-but-rare ev

239 investigate the continuous shift in coastal flooding regimes by quantifying continuous rates of incr

240 ooded wetlands in California, to alternative flooding regimes that occur during El Nino Southern Osci

241 Plants must manage cell swelling during flooding, rehydration, and pathogen invasion-but little

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

243 ich groundwater inundation and direct marine flooding represent the most and least substantial single

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

245 ocesses that may contribute to variations in flooding resilience.

246 Flooding resistance was not strongly correlated with per

247 g, we identified a subset of loci conferring flooding resistance, but lacking antagonistic effects on

248 lyses for variation in plant performance and flooding response were conducted in cultivated sunflower

249 We observed broad variation in flooding responses among genotypes.

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

251 variability, erosion response and consequent flooding responses.

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

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

254 Soil flooding resulted in rapid formation of inorganic thioar

255 Flooding resulting from the bursting of dams formed by l

256 clude microbial and mold growth secondary to flooding, resulting in displacement of persons and need

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

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

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

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

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

262 Seawater flooding significantly reduced CO(2) assimilation, trans

263 resulting in disruptive heatwaves, droughts, flooding, snowfalls, and cold spells.

264 from the most complete database of European flooding so far-suggest that: increasing autumn and wint

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

266 Analysis of these maps at the end of various flooding stages revealed that the nanofluid invaded into

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

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

269 plays a pivotal role in rice survival under flooding stress, as well as other abiotic stresses.

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

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

272 three gaseous signals for the regulation of flooding survival and identifies key regulatory targets

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

274 or enhanced oil recovery with a microfluidic flooding test, showing a dramatic increase of oil recove

275 Local measures of flooding that are comparable over large areas are diffic

276 Typhoon-related precipitation can produce flooding that is often only predictable a few hours in a

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

278 Flooding the field with non-ionic dextrose eliminates al

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

280 ity can also create conditions favorable for flooding, the enhanced precipitation related to Kelvin w

281 rved deltas, which cannot naturally mitigate flooding through sediment deposition.

282 soil redox conditions change, that is, from flooding to drainage to reflooding, batch incubations an

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

284 ed to reevaluate main sources of SLR induced flooding to promote the development of effective flood m

285 or 24 h also improved traits associated with flooding tolerance.

286 Thus, development of cultivars that are both flooding-tolerant and highly productive should be straig

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

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

289 puted tomography coupled with miniature core-flooding was used to evaluate their ability to enhance o

290 Through assessment of multi-mechanism flooding, we find that approaching decades will likely f

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

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

293 Given that coastal flooding will only worsen, we must reframe this problem

294 zards, tropical cyclone (TC)-induced coastal flooding, will worsen under climate change.

295 By contrast, flooding with distilled water or MgSO(4) did not affect

296 the southwest U.S. experienced severe flash flooding with high magnitude, whereas the Northern Great

297 In-situ saturation data reveals that flooding with only 0.1 wt% of E-CNS in brine resulted in

298 d roots, date palm seedlings were exposed to flooding with seawater and its major constituents under

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.