ライフサイエンスコーパス: tide

1 impact because of their ability to form "red tides".

2 ocline with a tidal frequency (i.e. internal tides).

3 where planetary gravity dominates over solar tides).

4 he Infant Development and Environment Study (TIDES).

5 nted a significant source of MeHg during low tide.

6 eristic of a tidal cycle, beginning with low tide.

7 and cool gulf water onto the bank during ebb tide.

8 iberate plantation and seeds floating on the tide.

9 ity compared with the classical AKT(Thr-308)-tide.

10 (m) for MgATP but not on k(cat)/K(m) for FAK-tide.

11 tively higher concentrations observed at low tide.

12 y individuals became much more "bold" at low tide.

13 ffective in elucidating mechanisms caused by tides.

14 ) have been linked to coral reefs during low tides.

15 and submerged due to periodic ebb and flood tides.

16 cculation, background turbidity and internal tides.

17 increased tidal range: spring ebb and flood tides.

18 terococci were elevated during ebb and flood tides.

19 ales-Verrucomicrobia group increased at high tides.

20 he same as the principal lunar and lunisolar tides.

21 -dG and at C8 in all the guanine nucleosides/tides.

22 t concentrations (SSC), over spring and neap tides.

23 thquakes and the occurrence of the strongest tides.

24 erturbers such as passing stars and Galactic tides.

25 min and were generated on both ebb and flood tides.

26 re opposite in sign to those produced by the tides.

27 ith larger measurements observed on outgoing tides.

28 frequencies ranging from 20% to 0.5% of high tides.

29 inary complexes (Kd(ATP) = 0.6 microM and Kd(Tide) = 1 microM).

30 llowed by low affinity binding of Tide (K(d)(Tide)=180 microM), and values of K(m)(ATP)=5-6 microM an

31 and values of K(m)(ATP)=5-6 microM and K(m)(Tide)=4-5 microM were expressed in the active ternary co

32 croM), K(iMgATP) (1.3 +/- 0.2 microM), K(FAK-tide) (5.6 +/- 0.4 microM), and K(iFAK-tide) (6.1 +/- 1.

33 K(FAK-tide) (5.6 +/- 0.4 microM), and K(iFAK-tide) (6.1 +/- 1.1 microM) were obtained.

34 2-->Val) [DNA: C-to-T substitution at nucleo-tide 677 (677C-->T)] in methylenetetrahydrofolate reduct

35 omplex (alphaKd(ATP) = 40 microM and alphaKd(Tide) = 80 microM) from individual transitory binary com

36 raindrops(1-6), river and ocean waves(7,8), tides(9) and others(10-17).

37 dissolved organic matter (DOM) supply at low tide, a synchronous increase in numbers of bacteria and

38 TIDE achieves higher resolution and sensitivity for NMR

39 aused by reflection of semi-diurnal internal tides affects sedimentation patterns and bottom gradient

40 systems that are found in the blooms of red tide algae.

41 Brevetoxins, the toxic components of "red tide" algae, all share one of two robust polycyclic ethe

42 Brown tide algal blooms, caused by the excessive growth of Aur

43 Karenia brevis is the dominant toxic red tide algal species in the Gulf of Mexico.

44 interaction of climate and the timing of low tides along the West Coast of the United States creates

45 Earth's body tide-also known as the solid Earth tide, the displacemen

46 (pre)biological building blocks (nucleosides/tides, amino acids and lipid precursors) under aqueous (

47 ave characteristics, and to a lesser extent, tides, amplify the resulting design heights by an averag

48 of viral replication as seen with nucleoside/tide analogs in other viral infections.

49 nhibitors, including 2'-modified nucleoside/-tide analogs such as PSI-6130, PSI-7977, INX-08189, and

50 T(2)* weIghted DEconvolution or TIDE analyzes individual free induction decays (FIDs) an

51 1821 CE probably resulted in a similar storm tide and a significantly larger storm surge.

52 ansport warm water off the bank during flood tide and cool gulf water onto the bank during ebb tide.

53 enerated by the ocean lunar semidiurnal (M2) tide and demonstrate that magnetic fields of oceanic ori

54 inetic mechanism, for which both E-MgADP-FAK-tide and E-MgATP-P-FAK-tide dead-end complexes form.

55 ion PDK1-tide1 substrate versus AKT(Thr-308)-tide and kinase selectivity profiling revealed a novel s

56 tically assess the non-linear interaction of tide and non-tidal residual in order to quantify its con

57 a statistical model that considers predicted tide and projections of SLR.

58 lobal coastal area flooded will be caused by tide and storm events with 32% due to projected regional

59 differed in their responses to variation in tide and temperature, but not over time.

60 n air temperature and relative humidity, and tide and wave actions dilute a fraction of the high sali

61 rate the combined effects of evaporation and tide and waves on subsurface salinity distribution on a

62 average, boldness increased from high to low tide and with increasing temperature but decreased margi

63 hour of day, day of year, minutes from high tide and year.

64 n geophysical fluctuations, such as internal tides and atmospheric-related inertial currents, rather

65 consider the joint effects of non-stationary tides and mean sea level (MSL) at multiple time scales.

66 te enterococci measurements may be biased by tides and other environmental factors, providing a flawe

67 X), the agent infamously associated with red tides and paralytic shellfish poisoning, is described.

68 s demonstrated through the tracking of Earth tides and recording of ground motion corresponding to a

69 lating to wavelengths that are controlled by tides and rotation, we suggest that Titan's moment of in

70 t long wavelengths that are not dominated by tides and rotation.

71 ), most commonly associated with oceanic red tides and shellfish poisoning, is a potent inhibitor of

72 Coastal floods are primarily composed of tides and storm surges due to tropical (TCs) and extra-t

73 gnitude and the relative influence of waves, tides and surge levels), we have performed a computer-ba

74 sent the dissipation of small-scale internal tides and their induced mixing in climate-scale models.

75 rcular orbit is unlikely to be the result of tides and therefore was probably present at formation.

76 ly, individuals that were more responsive to tide (and thus risk) were also more responsive to temper

77 Global curve-fitting analysis of ATP, Tide, and ADP titrations of pre-steady-state burst kinet

78 me on the flanks consistent with an internal tide, and high short-term variability in water temperatu

79 They are emplaced well above high tide, and may include megagravel clasts weighing tens or

80 to combine sea-level projections with wave, tide, and storm surge models to estimate increases in co

81 ains can trap dry weather runoff during high tide, and then release it in a bolus during the falling

82 t budgets, oceanographic forces of waves and tides, and delta morphology has remained poorly quantifi

83 t) dominance, but that most large deltas are tide- and river-dominated.

84 PDK1-catalyzed trans-phosphorylation of PDK1-Tide approximates a Rapid Equilibrium Random Bi Bi syste

85 r velocities caused by semi-diurnal internal tides are high enough to inhibit deposition of fine-grai

86 continuum between wave (about 80 per cent), tide (around 10 per cent) and river (about 10 per cent)

87 coupling with a larger-scale mode-4 internal tide as an explanation for their long-lived character.

88 The resulting "@-tides", as these oligomers have been designated, show a

89 derstorms is associated with the atmospheric tides, as a result of the troposphere-mesosphere-ionosph

90 re, is useful as a quantitative measure of @-tide association and folding processes that involve this

91 supercontinent palaeogeography predicts weak tides because the surrounding ocean is too large to host

92 y; on varying Tide concentrations, ADP and p'Tide behaved as noncompetitive and competitive inhibitor

93 ct and the (T/E)-PDK1-Tide product analog (p'Tide) behaved as competitive and noncompetitive inhibito

94 uria (26/26) suggested MSE onset on a rising tide between 06:30 and 08ratio21 hrs (9 June).

95 K1 called the PDK1-interacting fragment (PIF)tide-binding site, or PIF pocket.

96 ocide hydrogen peroxide (H(2)O(2)) for brown tide bloom control.

97 When applied to brown tide bloom prone natural seawater in a microcosm study,

98 ent effectively removed the developing brown tide bloom, while the rest of phytoplankton assemblage (

99 nction and are associated with periodic "red tide" blooms.

100 ina brevis, an organism associated with 'red tide' blooms in the Gulf of Mexico.

101 tu secondary microseism generation, post-low-tide bores, storm-induced sediment transport, infragravi

102 Florida red tide brevetoxins are sodium channel neurotoxins produced

103 enhanced vertical mixing, perhaps driven by tides, brings abyssal nutrients to the surface and suppl

104 ltered and unfiltered groundwater during low tide, but were similar to seawater U-Hg(T) concentration

105 icated that enzymatic phosphorylation of FAK-tide by FAK1 was best described by a random bi bi kineti

106 g the US Atlantic coasts the contribution of tides can be significant, with the average contribution

107 step follows formation of the E-MgADP-P-FAK-tide complex.

108 etitive inhibitors, respectively; on varying Tide concentrations, ADP and p'Tide behaved as noncompet

109 st to daily and seasonal changes in wave and tide conditions, which are themselves changing over long

110 Periodic ocean tides continually provide a cyclic load on Earth's surfa

111 Are perturbations to ocean tides correlated with changing sea-level and climate, an

112 Adult relocation using tides could explain mass spawning aggregations that incr

113 ce of mud/seawater inhalation (11/26), local tide cycle, and the relative lack of renal myoglobinuria

114 evation higher than the highest astronomical tide datum - captured the biotic and edaphic marsh-uplan

115 hich both E-MgADP-FAK-tide and E-MgATP-P-FAK-tide dead-end complexes form.

116 GPS)-based measurements of semi-diurnal body tide deformation.

117 on Aureococcus anophagefferens bloom (brown tide) development.

118 Measurements of @-tide dimerization and beta-hairpin folding equilibria no

119 n the maintenance of large blooms of the red-tide dinoflagellate Karenia brevis, which produces poten

120 nown as brevetoxins are produced by the 'red tide' dinoflagellate Karenia brevis.

121 river damming: deltas transitioning towards tide dominance are currently gaining land, probably thro

122 e with reduced riverine influence located on tide-dominated sand islands), across elevation gradients

123 low probabilities (unbounded tails), 82% are tide-dominated, and almost 49% are highly susceptible to

124 ignificant, with the average contribution of tides during the 10 largest events up to 55% in some loc

125 rasota Bay, Florida, before and during a red tide event.

126 incorporating the timing of semidiurnal high tide events throughout the breeding season, including ho

127 We demonstrate the performance of TIDE for magic angle spinning (MAS) [(13)C,(13)C]-DARR N

128 cintillans (Noctiluca) is a cosmopolitan red tide forming heterotrophic dinoflagellate.

129 trogen or phosphorus deficiency in the brown tide-forming alga Aureococcus anophagefferens.

130 er increased approximately 7-fold during low tide (from 0.5 to 3.6 pM).

131 During the winter of 2013-2014, the averaged tide gauge (TG) coastal sea level (CSL) anomaly north of

132 The models are extensively validated against tide gauge data and the impact of uncertainties and assu

133 We achieve this by pooling all of the tide gauge data together through a Bayesian hierarchical

134 Therefore, either the tide gauge estimates are too high, as has been suggested

135 Relative sea level rise at tide gauge Galveston Pier 21, Texas, is the combination

136 sed on a modified Kalman smoother, for using tide gauge observations to estimate the individual sourc

137 to the small number of extreme events in the tide gauge record and are only available at gauged locat

138 Our synthetic tests indicate that when all tide gauge records are used in the analysis, it should b

139 The analysis of long-term tide gauge records identified an extreme sea-level rise

140 However, the brevity of tide gauge records result in significant uncertainties w

141 ng an area-weighting technique for averaging tide gauge records that both incorporates up-to-date obs

142 PS-derived radial motions with Fennoscandian tide gauge records to estimate a regional sea surface ri

143 istics from post-event field survey results, tide gauge records, and eyewitness reports, suggesting o

144 year event) during the entire history of the tide gauge records.

145 e of sea-level rise recorded by the New York tide gauge.

146 Numerical model simulations, combined with tide-gauge and satellite altimetry data, reveal that wav

147 proxy relative sea-level reconstructions and tide-gauge data.

148 and basin scales, which we reconstruct from tide-gauge records.

149 contributions on 21st-century ESL changes at tide-gauge sites across the globe using extreme-value st

150 USArray Transportable Array inland and NOAA tide gauges along the coast recorded the pressure anomal

151 ent an analysis of sea level measurements at tide gauges combined with observations of temperature an

152 egory 4 storm, passed directly over six wave-tide gauges deployed by the Naval Research Laboratory on

153 Most direct estimates from tide gauges give 1.5-2.0 mm yr(-1), whereas indirect est

154 Here, we survey 152 tide gauges in the Pacific Ocean and South China Sea and

155 and our use of a common reference datum for tide gauges may explain the lower rates compared with ea

156 shable from minor flood thresholds of nearby tide gauges, we find evidence that several areas experie

157 combine a semi-analytical model of internal tide generation with satellite and in situ measurements

158 count for the bulk (>50%) of global internal tide generation, breaking and mixing.

159 cing at the surface associated with Saturn's tides, geology, and/or surface composition.

160 During low tide, groundwater appeared to transport MMHg to the coas

161 e active; with an increased salinity at high tide, halotolerant clusters III, V, and X were predomina

162 ulations in response to a Karenia brevis red tide harmful algal bloom by examining sound spectrum lev

163 After decades of disappointment, the tide has finally changed due to the success of recent pr

164 Remarkably, the tide has now turned again: the most important calcium tr

165 The tide has recently turned with the availability of suffic

166 tuents, a proxy for the highest astronomical tide (HAT), changes over seasonal and interannual time s

167 Tides have been recognized as a major driving forcing af

168 eral areas experience noticeable flooding at tide heights lower than existing flood thresholds.

169 an energetic viewpoint, small-scale internal tides, hitherto overlooked, account for the bulk (>50%)

170 ed of higher affinity, moth cytochrome c pep-tide I-Ek tetramer-binding cells resulted in substantial

171 ill be exceeded almost every day during peak tide (i.e., daily mean higher high water) before the end

172 nces in tumor immunology have now turned the tide in favor of immunotherapy for the treatment of many

173 ave a comparable role in deep circulation to tides in areas with complex topography.

174 This study demonstrates the importance of tides in regulating the dynamics of dissimilatory nitrat

175 --comparable with levels caused by winds and tides--in the vicinity of large populations of planktoni

176 e we propose that the dissipation of extreme tides increases vertical mixing of sea water, thereby ca

177 he sediment-tidal water interface and at the tide-induced groundwater fluctuating layer.

178 es associated with the solid-earth and ocean tides influence the genesis of tremor much more effectiv

179 stress optimized mangrove development along tide-influenced tropical coastlines.

180 , a function of bed surface depth below high tide, influences the rate of sediment deposition and slo

181 Generated primarily by the wind and the tides, internal waves can travel thousands of kilometres

182 Since TIDE is applicable to all type of homonuclear correlatio

183 sustainable energy such as solar, wind, and tide is attracting ever-increasing attention for sustain

184 roM) was followed by low affinity binding of Tide (K(d)(Tide)=180 microM), and values of K(m)(ATP)=5-

185 sed primarily on long-term SLR with a static tide level, and have not comprehensively accounted for d

186 of enterococci in dry sands at the mean high-tide line was significantly positively related to sand m

187 samples came from sandy beaches at the high tide line, and most seawater samples were taken at the s

188 ntly occupy global land below projected high tide lines for 2100 under low carbon emissions, up from

189 topographic and population data, local high tide lines, and regional long-term sea-level commitment

190 ccupy land less than 10 m above current high tide lines, including 250 M below 1 m.

191 ted by a range of physical processes such as tides, local winds, and surface and internal waves, caus

192 f energy propagation of semidiurnal internal tides may determine the average gradient of continental

193 e mechanism, we propose that extreme oceanic tides may produce changes in sea surface temperature at

194 f one of the moon's semi-diurnal gravimetric tides might have driven the patients' bipolar cycles, by

195 Here we propose a "tide" model to accommodate and interpret current experim

196 idge agrees with the predictions of internal tide models.

197 Earth tides modulate tremor and low-frequency earthquakes (LFE

198 hey are shredded by the strong gravitational tides near the white dwarf core.

199 we fear that there will be a dramatic rising tide of alcohol relapse, admissions for decompensated AL

200 Building on these lessons to turn the tide of biodiversity loss will require bold and innovati

201 protect endangered wildlife against a rising tide of infectious disease?

202 health partnerships, which have stemmed the tide of infectious diseases in low- and middle-income co

203 tially dedicated exclusively to stemming the tide of infectious epidemics.

204 In this era of systems biology, the tide of information derived from "omic" technologies (ge

205 Stemming the tide of invasions requires understanding why some specie

206 latform for beginning to confront the rising tide of non-communicable diseases.

207 se past gains are threatened with the rising tide of obesity and diabetes.

208 An incoming tide of research is now beginning to challenge this as y

209 effectiveness is now threatened by a rising tide of resistance.

210 We anticipate our work may turn the tide of the dogmatic view of CHOP and cause a reinvestig

211 own been shown to be sufficient to stem the tide of the epidemic.

212 he power of research in children to turn the tide of the growing burden of non-communicable, chronic,

213 Here we report a red tide of the phototrophic ciliate Mesodinium rubrum locat

214 ention and management strategies to stem the tide of this disease and its cost.

215 gent and immediate action to stem the global tide of tobacco-related death and suffering and to impro

216 ction of RFL cells showed slowly propagating tides of cGMP spreading across the cell in response to d

217 the discovery of ubiquitous, strong diurnal tides of dust in the Southern Hemisphere of Mars.

218 We argue that red tides of M. rubrum are more likely to occur under the th

219 to develop novel therapies that may turn the tide on the continuing struggle to find effective cures

220 ombination prevention strategies to turn the tide on the HIV pandemic.

221 -wetland complexes located above the head-of-tide on the western shore of Chesapeake Bay.

222 e fiddler crab Afruca tangeri forages at low tide on tropical and semi-tropical mudflats, under brigh

223 en cycling microorganisms, but the effect of tides on dissimilatory nitrate reduction, including deni

224 hern Gulf coast, the average contribution of tides over the largest 10 events is generally below 25%.

225 We propose that tides played a catalytic role in liberating iceberg arma

226 ed on fingerprinting elements suggested that tides played a major role in forming particulate matter

227 rients increased the biomass and evenness of tide pool macrophytes where consumer abundance and nutri

228 In this study, we used tide pool microcosms to demonstrate that the effects of

229 trations, the ADP product and the (T/E)-PDK1-Tide product analog (p'Tide) behaved as competitive and

230 hat excessive Cu and Ni likely promote brown tides, provides evidence for trace metal linkages in alg

231 th with the Moon and Sun at times of extreme tide raising forces.

232 isance flooding," often associated with high tides, recent increases in frequency are more clearly li

233 Tide records going back to the 19th century show no meas

234 At low tide, representative of higher DOM and increased prey bu

235 Here we use a high-resolution, eddy- and tide-resolving numerical ocean model to simulate mangrov

236 We use it to measure the Earth tides, revealing the long-term stability of our instrume

237 ETV differs from the other nucleoside/tide reverse transcriptase inhibitors approved for HBV t

238 hosphorylation of a model peptide substrate (Tide, RRRLSSLRA).

239 d culturable enterococci populations in high-tide sands.

240 At Hong Kong, the increase in tides significantly amplifies the risk caused by sea-lev

241 s revealed distinct shifts such that, at low tide, significantly higher phylotype abundances were obs

242 -terminal amino acids within an 8-residue, @-tide-stabilized [in which @ denotes the 1,2-dihydro-3(6H

243 multiple drivers (e.g., extreme coastal high tide, storm surge, and river flow).

244 Global models of tide, storm surge, and wave setup are used to obtain pro

245 ion when incorporated in an oligopeptide ("@-tide") strand.

246 Daily tide stresses were previously thought to be insufficient

247 orrelations between smaller events and daily tide stresses.

248 ped using a biotinylated version of the PDK1-tide substrate containing the activation loop of AKT fus

249 Our results suggest that internal tides, substrate heterogeneity and oceanographic interfa

250 d 1 mol of tightly bound heme per mol of pep tide subunit.

251 In the deep ocean, tides supply much of the mechanical energy required to s

252 controlled by comparable contributions from tides, surface winds and passing eddies.

253 oreover, depth and frictional changes affect tide, surge, and wave characteristics, altering the rela

254 pically consider the superimposed effects of tides, surges, waves, and relative sea-level rise (SLR),

255 we describe the synthesis of a variety of @-tide-templated hairpins and the NMR and CD characterizat

256 ophagefferens populations from a dense brown tide that occurred in Long Island, NY, in 2009 were assa

257 The regenerative process may tide the loss of overall beta-cell function, but it also

258 th's body tide-also known as the solid Earth tide, the displacement of the solid Earth's surface caus

259 itude of the moon's semi-diurnal gravimetric tides: the 14.8-day spring-neap cycle, the 13.7-day decl

260 All of these devices can observe the Earth tides: the elastic deformation of the Earth's crust as a

261 Going against the current tide, this paper argues that there is indeed a systemati

262 Dust tides-tidal transport of dust in this way-rapidly transp

263 1(deltaPH)-catalyzed phosphorylation of PDK1-Tide (Tide), which contains an extended "PIF" sequence C

264 d during the peak spawning period after high tide to produce a linear relationship.

265 se in microplastics abundance from the flood tide to the ebb tide was found, and a weak positive rela

266 The cascade from tides to turbulence has been hypothesized to serve as a

267 Given these major elements in the tides-to-turbulence cascade, an energy budget approaches

268 plitude and steepness as internal waves from tide-topography interactions observed elsewhere, and is

269 ed frequently in the absence of any apparent tide-topography interactions.

270 Among those effects, thermal tides transport the angular momentum, which maintains th

271 Tides transport warm water off the bank during flood tid

272 roundwater discharge to the ocean during low tide transported mercury offshore.

273 ics abundance from the flood tide to the ebb tide was found, and a weak positive relationship with SS

274 Inundation by spring tides was the primary rewetting mechanism that sustained

275 2+) concentrations lower than those in brown tide waters enhance A. anophagefferens growth, but Zn se

276 d Ni(2+) concentrations, e.g. those of brown tide waters in the northeastern US, greatly stimulated A

277 lobal sea level and sedimentation, including tide, wave and fluvial processes.

278 an normal ocean-level fluctuations caused by tides, waves, and storm surge.

279 ses such as river and groundwater discharge, tides, waves, and storms.

280 exposure by integrating the effects of SLR, tides, waves, storms, and coastal change (i.e. beach ero

281 times larger than those associated with the tides, we argue that tremor occurs on very weak faults.

282 iable currents driven by buoyancy, wind, and tides, we predict high spatial and temporal variability

283 hen release it in a bolus during the falling tide when drainpipe outlets are exposed; (3) nearshore t

284 Those which were relatively bold at high tide (when predation risk is greater) were similarly bol

285 earthquakes occur preferentially during low tide, when normal faulting earthquakes should be inhibit

286 risk is greater) were similarly bold at low tide, whereas shy individuals became much more "bold" at

287 e substrate (Ac-RRRRRRSETDDYAEIID-NH(2), FAK-tide) which corresponds to the sequence of an autophosph

288 aPH)-catalyzed phosphorylation of PDK1-Tide (Tide), which contains an extended "PIF" sequence C-termi

289 ng the climatic influence of the lunar nodal tide, which has been detected with its modern 18.6-yr pe

290 analyze the LFE response to the fortnightly tide, which modulates the amplitude of the daily tidal s

291 They usually result from barotropic tides, which flow over bottom topography, causing densit

292 vent viscosity had no effect on k(cat)/K(FAK-tide), while k(cat) and k(cat)/K(MgATP) were both decrea

293 eration of internal waves, known as internal tides, whose fate-the relative importance of their local

294 the redistribution of sediments by waves and tides will be critical for successfully predicting human

295 owing to constant changes in river inflows, tides, wind, and water height, all of which combine to a

296 e of 1 mM [gamma-(18)O(4)]ATP and 1.5 mM FAK-tide with a progressive time course which was commensura

297 ater (3.3-5.2 pM) decreased during a falling tide, with groundwater U-Hg(T) concentrations typically

298 ate is highest during the waxing fortnightly tide, with LFEs most strongly promoted when the daily st

299 Here we show that ocean tides within the Labrador Sea were exceptionally large o

300 stward-propagating migrating diurnal thermal tide, zonally distributed dust fronts slosh back and for