ライフサイエンスコーパス: ascent

1 radient closely follows the line of steepest ascent.

2 od is quickly maximized by cyclic coordinate ascent.

3 nes were carried to the surface during magma ascent.

4 ary and undergo little lateral deflection on ascent.

5 respect to the predictor oracle by gradient ascent.

6 s might be greater during stair descent than ascent.

7 in Pao2 was 1.60 kPa per 1000 m of vertical ascent.

8 on how easily gas and magma decouple during ascent.

9 volatile-driven decompression during conduit ascent.

10 e bioconcentration dynamics following spring ascent.

11 irth weight of approximately 100 g/1000 m of ascent.

12 repeated, energetically costly high-altitude ascents,(10-13) and others fly at some of the fastest sp

13 o dose modification was more frequent in the ASCENT (31%) than in the control arm (15%).

14 erates slab subduction(3), accelerates plume ascent(4) and inhibits chemical mixing(5).

15 tude and achieved even higher levels upon re-ascent, a feature that is positively associated with qui

16 On ascent after a diving exposure, the dissolved gas can ac

17 arch behavior was consistent with a gradient ascent algorithm that utilized directional cues in the p

18 gression revealed decreasing isoleucine with ascent alongside increasing lactate and decreasing gluco

19 aximization principle combined with gradient ascent and block updates.

20 n international perspective, we consider the ascent and decline of the autopsy, the legal frameworks

21 transitions between level walking and stair ascent and descent over a range of stair inclination ang

22 nt (P < 0.001, Cohen's d<-2.77) during stair ascent and descent, and decreased foot progression angle

23 trials involving level-ground walking, ramp ascent and descent, and stair ascent and descent.

24 and without knee osteoarthritis during stair ascent and descent.

25 lace exchange and Ag pop-out as well as step ascent and descent.

26 walking, ramp ascent and descent, and stair ascent and descent.

27 tensity curves showed a significantly slower ascent and diminished maximum intensity in pancreas graf

28 Wilson and Head model kimberlite ascent and eruption by considering the propagation of a

29 measured viscosity values, we simulated the ascent and eruption process of kimberlite magma.

30 Here we present a new model of kimberlite ascent and eruption, emphasizing the extremely unsteady

31 xsolution (here up to ~800 MPa) drives their ascent and explosivity.

32 Other flight modes including vertical ascent and fast forward flight are more mechanically and

33 according to acclimatization status, rate of ascent and individual susceptibility.

34 of noble gases during mantle melting, magma ascent and near-surface degassing.

35 In turn, higher humidity favors large-scale ascent and stronger convection.

36 Bacterial ascent and the cell dynamics of phagocytic cells were as

37 sult of entrainment of ambient mantle during ascent, and also on whether initial plume upwelling is a

38 the landscape able to support high-altitude ascents, and that bats use these locations to reach high

39 First, a reduction in tropical ascent area and an increased frequency of heavy precipit

40 as 17.8 months (95% CI, 16.0 to 19.5) in the ASCENT arm and 20.2 months (95% CI, 18.8 to 23.0) in the

41 erim analysis, more deaths were noted in the ASCENT arm, and the trial was halted.

42 estimate energy expenditure during stairway ascent at speeds chosen by the participants.

43 The ASCENT (Automated Simulations to Characterize Electrical

44 After 66 d at altitude and ascent beyond 6400 m, mitochondrial densities fell by 21

45 ation and the latitude of that circulation's ascent branch.

46 The vertical ascent by prostate cancer cells from the lowlands to the

47 We validated the accuracy of ASCENT calculations, verified usability in beta release,

48 ecreased relative role during the outbreak's ascent compared to non-receipt [OR 0.16 (0.01, 0.84) for

49 One mechanism for degassing during magma ascent, consistent with observations, is the generation

50 The temporal trends analysis showed ascent curves tapering off at approximately weeks 4 to 6

51 Ascent decreased the arterio-central venous concentratio

52 grate wind conditions to guide high-altitude ascents, deftly exploiting vertical wind energy in the n

53 Steepest ascent/descent method and central composite rotatable de

54 on, and ambulation context (transition type, ascent/descent), demonstrating a mathematical modeling a

55 his previously unknown behavior of nocturnal ascents during moonlight nights could be either a respon

56 isation of nanolites impacts magma rheology, ascent dynamics, and eruptive style.

57 agmentation depending on magma degassing and ascent dynamics.

58 ilibrium processes to play a key role on the ascent dynamics.

59 our understanding of such disequilibria and ascent dynamics.

60 2) degassing in the upper crust during magma ascent, followed by further gas-liquid separation at ver

61 -section were greater for stair descent than ascent for both age groups (mostly P = 0.001 to 0006) bu

62 unacclimatized LL and TH during incremental ascent from 1,400 m to 4,300 m in age- and sex-matched g

63 tivity (max acceleration 3.12 g) and a rapid ascent from 126 m at 3.6 m.s(- 1) followed by death and

64 a moth resting in his trekking bag during an ascent from 2,364 to 4,371 m above sea level.

65 a middle-crustal hot zone with episodic melt ascent from an unstable layer at the top of the zone wit

66 After the spring ascent from deep waters, C. hyperboreus approach equilib

67 barotrauma due to lung overexpansion during ascent from depth.

68 Ascent from ground level to the conditions of 7000 to 80

69 increases in hypoxia, simulating the gradual ascent from sea level to an elevation of 6,000 m.

70 troleum fluids dissolved into the sea during ascent from the pared wellhead (1,505 m depth) to the se

71 hly context-specific use of B-strokes during ascents from deep-dives in baseline conditions, during s

72 dence interval [CI], 6.95-23.66; P < 0.001), ascent greater than 400 m/day (aOR, 5.89; 95% CI, 3.78-9

73 ssociated with the ACE genotype in the rapid ascent group (p = 0.01) with a relatively sustained Sa(O

74 he ACE genotype and remained so for the slow ascent group, in whom the fall in Sa(O(2)) with ascent w

75 Rapid ascent (n = 32) and slow ascent groups (n = 40), ascending to approximately 5,000

76 such textures due to fundamentally different ascent histories.

77 ted in Sherpa, compared to lowlanders during ascent; however, PASP was comparable in both groups upon

78 decreased FiO(2)) and hypobaric (HH, 4200 m ascent) hypoxia exposures compared to sea level (normoba

79 , and provide several compelling examples of ASCENT-implemented models.

80 Groups also perform a coordinated silent ascent in an unpredictable direction, covering a mean of

81 Additionally, we show a steeper ascent in calcium signaling as we imposed higher loading

82 Timescales of magma ascent in conduit models are typically assumed to be muc

83 g from initial hypoxia is maintained upon re-ascent in humans or re-exposure to hypoxia in mice and a

84 rebral oxygen delivery was maintained during ascent in lowlanders, it was significantly reduced in th

85 eal that cold pool dynamics reduce mesoscale ascent in the cloud systems, thereby arresting a runaway

86 ort of moist static energy, weakening the NH ascent in the TC formation zones; meanwhile, the increas

87 Changes in the lipid profile with ascent included a decrease in triglycerides (48-50 carbo

88 d narrowing of the convective zone, enhanced ascent, increased high clouds, suppressed low clouds, an

89 aging dives and later in those dives, during ascent, initiate a unique strong gait (B-strokes), hypot

90 oir is in a stable state of efficient bubble ascent into the hydrothermal system on the basis of esti

91 rinary neutrophils acts to prevent bacterial ascent into the kidney.

92 e prevented from forming owing to rapid melt ascent, intrusion and eruption(8,9), so even strong tida

93 This ascent is driven by buoyancy forces, which are enhanced

94 ffective overburden loads (<=11 kPa), stable ascent is followed by dynamic ascent (which has not been

95 therm exhibits an hysteresis loop; a gradual ascent is observed at higher pressures during adsorption

96 ter acclimatization to high altitude upon re-ascent is seen in humans; however, the molecular basis f

97 from Mount Etna's 2001 eruption and a magma ascent model to constrain timescales for crystallization

98 Rapid ascent (n = 32) and slow ascent groups (n = 40), ascendi

99 stry and style of fluid release during magma ascent, notably the behaviour of chlorine, a key metal-t

100 port numerical model was used to explore the ascent of a mature CH(4) bubble toward the seafloor in m

101 ot clear populations of S. aureus Due to the ascent of a phenotyically diverse array of small-colony

102 The ascent of alpha-cyanoacrylamide covalent warheads for th

103 truders throughout, and probably before, the ascent of ants to ecological dominance, with ancient gro

104 forces, such as urine flow, that prevent the ascent of bladder microbes.

105 The recent ascent of covalent drugs has stimulated considerable eff

106 ynthesis, which play a key role in the steep ascent of developing functional materials with unprecede

107 he hypothesis that in these experiments, the ascent of intermediate-fitness compensatory mutants, rat

108 w-water habitats required for the subsequent ascent of macroscopic animals.

109 with the common "complex" diseases, and the ascent of man has been the product of 3.5 billion years

110 affects the thermal evolution of Earth, the ascent of mantle plumes, settling of subducted oceanic l

111 With the ascent of modern neurobiological technology, our underst

112 Here, we propose a new mechanism for the ascent of mushy magma based on microstructural observati

113 sence of these drugs commonly results in the ascent of mutations that ameliorate these costs, rather

114 processes contributing to the emergence and ascent of resistance during treatment and the waning of

115 ve rhyolite eruption indicate that the rapid ascent of rhyolite occurred through dyking and that melt

116 The ongoing ascent of sequencing technologies has enabled researcher

117 rconnected network, culminating in the rapid ascent of the basalt relative to the surrounding solid m

118 avaginal inoculation and confirmed the rapid ascent of the chlamydial organisms from the lower to upp

119 We show that the initial ascent of the meltwater outflow from the ice shelf cavit

120 ikely an influential factor that impeded the ascent of the parent magma and allowed the formation of

121 e classic model of pathogenesis proposes the ascent of UPEC by the urethra and external adherence to

122 The ascent of UTI-causing pathogens to the kidneys results i

123 TP, effectively short-circuiting the slower ascent of water vapor across the cold tropical tropopaus

124 As a test case, the invasive ascents of the Tepui by highly metastatic PC-3 and nonin

125 ext] in the sagittal plane during both stair ascent (P = 0.005, Cohen's d = 1.7) and descent (P = 0.0

126 r solubility in magma reveals that, for many ascent paths, exsolution may be more efficiently achieve

127 nly occurred during the latter stages of the ascent phase and, once initiated, was rapid.

128 diving heart rate minima during the powered ascent phase of feeding lunges followed by a gradual dec

129 The highest speeds occurred during the ascent phase, and the average diving time was 6 min 45 s

130 sure, B-strokes were used during descent and ascent phases of both deep and shallow dives.

131 y outcomes of fast-pace 5- and 10-step stair ascent power.

132 Preventive measures include slow ascent, pre-acclimatization and, in some instances, medi

133 ly a few seconds using an optimised GRadient Ascent Pulse Engineering (GRAPE) implementation, this no

134 This migration included a 3-wk, ~4,100-m ascent punctuated by upward bursts and pauses, resemblin

135 The strong relation between magma ascent rate and disequilibrium crystallization and exsol

136 Their morphology, aspect ratio, inferred ascent rate, and temperature show that they are passivel

137 Ascent rates during these dives were significantly slowe

138 Those timescales constrain magma ascent rates of 40-500 m/h (0.011 to 0.14 m/s) from the

139 earliest erupted tephra, which implies magma ascent rates of about 0.1 and 1 m s(-1).

140 ses (reservoir chambers) with variable magma ascent rates, mostly within 48 hours.

141 ess, about 45 percent of air in the tropical ascent region at 21 kilometers is of mid-latitude origin

142 rkable stabilization due to asymmetry in the ascent region from the (E)-isomer to ITS.

143 rformed with site-specific analytic gradient ascent relying on historical operational data.

144 Predicting a bubble ascent scenario in muddy sediment will further allow est

145 Two bubble ascent scenarios were demonstrated: stable and dynamic.

146 e role of chronic hypoxia independent of the ascent, Sherpa who had not recently descended were also

147 reater depth are probably channelized during ascent, so preventing direct re-equilibration with shall

148 t of season, depth and duration of trawl and ascent speed.

149 Magma ascent, storage, and discharge in the trans-crustal magm

150 the thermal path experienced by magma during ascent strongly controls degassing, vesiculation, magma

151 in the international, multicenter, phase III ASCENT study.Patients were randomly assigned 1:1 to rece

152 taxa is consistent with slower responses in ascent than descent toward carrying capacity.

153 During ascent, the device is evacuated as it equilibrates with

154 During ascent, there were reductions in iron status in both low

155 oling rate, such as would occur during magma ascent through a chondritic crust.

156 effects on sulfur solubility associated with ascent through over-thickened crust.

157 The rate of migration increases with ascent through the intermediate zone (average 2-6.4 micr

158 cumulation of multiple melt fractions during ascent through the overlying crust eliminates geochemica

159 ole in its bladder colonization and eventual ascent through the ureters, against urine flow, to invad

160 the PLM descent time in comparison with its ascent time.

161 oclase reaches equilibrium in 1-2 h, whereas ascent times were <1 h.

162 This approach--documenting magma ascent timescales from the mantle beneath a convergent m

163 We found that following ascent to 4,300 m, LL had significantly lower PCO(2) (P

164 0 m) and following day 8 to 9 of incremental ascent to 4,300 m.

165 y lowlanders before and 4-6 days after rapid ascent to 4300 m.

166 es at low altitude (LA) and following active ascent to 4559 m (HA).

167 ll as on day 2 (MG2) and 4 (MG4) after rapid ascent to 4559 m.

168 with longitudinal sampling at baseline, upon ascent to 5,100 m and descent to sea level.

169 d Sherpa were determined during: (1) a 9-day ascent to 5050 m (20 lowlanders; 12 Sherpa), and (2) fol

170 During ascent to 5050 m, the rise in pulmonary artery systolic

171 lood flow (duplex ultrasound) during a 9 day ascent to 5050 m.

172 pa, Kathmandu; 1400 m) and following gradual ascent to 5050 m.

173 flow in Sherpa compared to lowlanders across ascent to altitude (P = 0.046).

174 As inspired oxygen availability falls with ascent to altitude, some individuals develop high-altitu

175 at Sherpa have lower brain blood flow during ascent to and acclimatization at high altitude compared

176 arterial blood from 10 climbers during their ascent to and descent from the summit of Mount Everest.

177 found that BF signal content increased with ascent to EBC in both SH and LL.

178 198 human participants before and during an ascent to Everest Base Camp (5,300 m).

179 Subacute exposure (19 d after initiating ascent to Everest base camp, 5300 m) was not associated

180 The path to translation, like the ascent to Everest, is certainly littered with corpses.

181 uffer less negative cerebral side effects of ascent to extreme altitude, yet little is known as to wh

182 nosine levels are rapidly induced by initial ascent to high altitude and achieved even higher levels

183 During ascent to high altitude and pulmonary edema, the alveola

184 Ascent to high altitude is associated with a fall in the

185 Ascent to high altitude is associated with adjustments i

186 ness and high-altitude pulmonary oedema upon ascent to high altitude, and PFO presence is associated

187 ) and stroke volume (SV) were decreased upon ascent to high altitude, but were comparable to sea leve

188 n is altered in lowlanders during either (1) ascent to high altitude, or (2) following partial acclim

189 e to hypoxic conditions, for example, due to ascent to high altitude, stroke, or traumatic brain inju

190 vestigate changes of intraocular pressure on ascent to high altitude.

191 the pulmonary and cerebral vasculature upon ascent to high altitude.

192 y and flexibility during hypoxic exposure on ascent to high altitude.

193 g exposure to hypobaric hypoxia on a gradual ascent to Mount Everest Base Camp (5,300 m).

194 Finally, we apply mirror ascent to optimize the design so as to achieve more desi

195 Rather, it uses gradient ascent to stochastically explore intermediate feature ma

196 Magma ascent to such low pressure is expected to drive volatil

197 ers, and shapes the output of the DCN in its ascent to the inferior colliculi.

198 rtial melting in the mantle followed by melt ascent to the surface and gas exsolution.

199 mixing and mobilization of coal and basalt, ascent to the surface, explosive combustion, and the atm

200 years; 510 men [65.6%]) reporting 115 group ascents to altitudes between 1524 m and 8730 m were incl

201 full moon, they conducted regular nocturnal ascents to altitudes up to >4,000 m (mean 2,000 m).

202 dus phase is triggered by their transcrustal ascent towards the Earth's surface.

203 ns mostly involve pressure buildup and magma ascent towards the surface(1).

204 ASCENT treatment was associated with shorter survival th

205 The pivotal phase III ASCENT trial demonstrated improved survival outcomes ass

206 ied, exploratory biomarker analysis from the ASCENT trial evaluates the association between tumor Tro

207 ding the TROPiCS-02 primary analysis and the ASCENT trial).

208 vity, gas and melt remain coupled during the ascent up to the last hundred meters of the conduit.

209 s experienced a 30 mg% alcohol prime (10 min ascent) using the Computerized Alcohol Infusion System.

210 imated by mean field Monte-Carlo co-ordinate ascent variational inference (CAVI-MC) and easily scales

211 mobility (0.1-0.4 g cm(3) Pa(-1) s(-1)) and ascent velocity (1.5-6.0 m yr(-1)) are presented to supp

212 effects of atmospheric moisture and vertical ascent velocity) at a global scale in both historical an

213 Magma ascent velocity, decompression rate, and cumulative magm

214 etermine age-specific differences during the ascent versus descent of an influenza season by influenz

215 hey attribute to troposphere to stratosphere ascent via the Asian monsoon.

216 erence of femoral neck strains between stair ascent vs. descent, young vs. older populations was comp

217 ent group, in whom the fall in Sa(O(2)) with ascent was genotype independent.

218 ions insinuate that shearing of magma during ascent was limited.

219 L) and Tibetan highlanders (TH; Sherpa) with ascent was previously unknown.

220 However, Sa(O(2)) with ascent was significantly associated with the ACE genotyp

221 [13.6] years; 185 men [60.7%]) reporting 29 ascents were included in the IPD analysis.

222 1 kPa), stable ascent is followed by dynamic ascent (which has not been previously demonstrated to th

223 and positive knee power generation in stair ascent, which are fundamental biomechanical functions of

224 eutrophils are critical to control bacterial ascent, which is in line with previous studies suggestin

225 e overburden loads induce only stable bubble ascent, which stops at the gas horizon frequently observ

226 ASCENT will enable the reproducibility of simulation dat

227 usceptible individuals during the outbreak's ascent, with all ORs for each of those age groups vs. gr

228 sorption isotherms, characterized by a rapid ascent within the 40-60% relative humidity range with a

229 c hypoxic conditions in the weeks before the ascent would be helpful.

230 that both this uplift and bat high-altitude ascents would be highly predictable.(18) By superimposin