ライフサイエンスコーパス: humid

1 e foraging activity when conditions are more humid.

2 .8% for dry (0% RH) conditions and 17.2% for humid (55 and 95% RH) conditions, and normalized root-me

3 y traversodont cynodonts are restricted to a humid 6 degrees equatorial swath that persisted for over

4 esence of water and can be subjected to 1000 humid adsorption/desorption cycles with minimal degradat

5 intain a high capacity of 1600 mA h g(-1) in humid air ( approximately 10% relative humidity).

6 tion layer also allows LixSi to be stable in humid air ( approximately 40% relative humidity).

7 tions of 1606 ppm, 15033 ppm, and 185 ppm in humid air (with 20% RH), respectively.

8 investigated the byproducts generated by the humid air discharge itself, which are the greenhouse gas

9 27(5) A, beta = 97.41(3) degrees), formed in humid air from the solid dimeric [Cu(CF(3)COO)(2) x (qui

10 Hyperventilation of hot humid air induces transient bronchoconstriction in patie

11 al cylinder are impregnated with salt, while humid air is blown through the tube.

12 s is the tetranuclear blue product formed in humid air of the mu(4)-oxo tetramers.

13 y condensation of the water molecules of the humid air on the paper-sensor during the forced exhalati

14 Binary CO2/H2O adsorption measurements for humid air reveal that the presence of H2O at 2.55 kPa en

15 As expected, humid air samples are required for proper sensor functio

16 ted considerably less localised corrosion in humid air than pure magnesium.

17 The passive capture of clean water from humid air without reliance on bulky equipment and high e

18 to collect water and promote nucleation from humid air(7-9).

19 eaction of Fe and O (causing iron to rust in humid air).

20 bonyls into imines mediated by NH3 vapors in humid air, resulted in selective browning of the LSOA sa

21 dsorbed than long chain alcohols, whereas in humid air, this preference is changed, and the sensitivi

22 Pseudomonas putida, i.e., biofilms grown in humid air, were analyzed by atomic force microscopy to d

23 lved in surface-adsorbed water reservoirs in humid air, with the signal strength being governed by th

24 chemistry with the participation of vapor in humid air.

25 sphere under an ultralow contact pressure in humid air.

26 cation of the destruction pathway in dry and humid air.

27 , ways when exposed to HCl and NH3 vapors in humid air.

28 chanically ventilated dogs (n = 8) with warm humid air.

29 rying concentrations of hydrogen fluoride in humid air.

30 iad" of neurons (with a dry-, a cold-, and a humid-air-responding cell [3]), IR40a expression include

31 oups can be explained by their hydrolysis in humid ambient conditions.

32 ine methane sensors for measuring methane in humid and condensing sewer air.

33 ng-term impact of NT/RT on N2 O emissions in humid and dry climatic zones with emissions expressed on

34 nvestigated at the gas/solid interface under humid and dry conditions, along with the nature of the h

35 margins smallest for species occupying both humid and dry tropical environments.

36 and storage in semiarid and arid, but not in humid and dry-subhumid, environments.

37 Our results support that LSTs in semi-humid and semi-arid regions with little vegetation will

38 Flash droughts are most likely to occur over humid and semi-humid regions, such as southern and north

39 ancestor, the Red junglefowl, which lives in humid and sub-humid tropical areas.

40 y of humidity swing driven air capture under humid and windy conditions is tested in the laboratory.

41 ver a wide range of climate conditions (arid-humid) and limiting factors (soil moisture, leaf area, e

42 ens are intensifying (becoming more warm and humid), and thus changes in synoptic meteorology may be

43 ns of grazed livestock agroecosystems (arid, humid, and temperate), and groups of animal production s

44 n soil moisture tended to be greater in more humid areas.

45 esponsive to decreased precipitation in more humid areas.

46 ones, to 13.3% (47 trees per hectare) in sub-humid areas.

47 more pigmented populations are found in more humid areas.

48 increasing in arid regions and decreasing in humid areas.

49 130 degrees C) and working conditions (i.e., humid) as well as in the presence of various interfering

50 e inherent limitations of sensitivity to the humid atmosphere and dendrite growth.

51 A more humid atmosphere helps to explain PETM temperatures, but

52 ples were subjected to an oxygenated, highly humid atmosphere in a closed chamber for 4 to 5 months.

53 A more humid atmosphere will lead to enhanced moisture transpor

54 n multifarious environments namely, ambient (humid) atmosphere, dry nitrogen, and vacuum.

55 mechanism is revealed to differ for dry and humid atmospheres, changing from a site-specific binding

56 properties were not affected by exposure to humid atmospheres.

57 ter droplets and films on the leaf hair from humid atmospheres; collection of fog droplets on leaf ha

58 arid basin (the Tarim River Basin, TRB) and humid basin (the Yangtze River Basin, YRB) were evaluate

59 rt of Pangea and suggest that the equatorial humid belt in the Late Triassic was about as wide as it

60 prolonged residence in the austral temperate humid belt where a provincial vertebrate fauna with earl

61 ble Deccan Traps drifted into the equatorial humid belt where uptake of CO(2) by efficient silicate w

62 e onto continental crust within the tropical humid belt.

63 ES males, however, from the humid biome, showed a tendency to lunge more per aggress

64 Humid biomes also respond to drought at short time-scale

65 Arid and humid biomes are both affected by drought, and we sugges

66 ed and brominated substances as observed for humid carrier gases.

67 r calculation remains large, particularly in humid catchments (for example, figure 2 in our paper).

68 0.51 kg C m(-2), lower than that observed in humid cities but much higher than that assumed in many r

69 10.1 ka BP indicates a transition to a more humid climate and elevated fluvial runoff.

70 the only time in the last 200,000 years that humid climate conditions encompassed southern and tropic

71 d cities, which is stronger than that in the humid climate due to a stronger longwave radiative forci

72 ite indicates wet conditions in the cave and humid climate from ~ 200 BCE to 100 CE, at the time of t

73 tamination of milk taken from the areas with humid climate was higher than the arid climate.

74 Mesozoic-Cenozoic radiation event, an era of humid climate when terrestrial communities dominated by

75 cted rocks (mafic/ultramafic) and a tropical humid climate with high precipitation rate are needed to

76 te climate, hot and dry climate, and hot and humid climate) for at least 9 days simulating the period

77 , and for biofuels regions of a moderate and humid climate.

78 easures, strong outbreaks are likely in more humid climates and summer weather will not substantially

79 +/- 0.3 kelvin (mean and standard error) in humid climates but decreasing DeltaT by 1.5 +/- 0.2 kelv

80 t decrease in yield-scaled N2 O emissions in humid climates when fertilizer-N was placed at >/=5 cm d

81 Therefore, in humid climates, deep placement of fertilizer-N is recomm

82 cts the species range limits in both dry and humid climates, whereas SLA and longevity do not show cl

83 oses to produce ferric oxyhydroxides in more humid climates.

84 laining local lizard extinctions in cool and humid climates.

85 a-scaled N2 O emissions, in particular under humid climatic conditions.

86 s on the surface of an early Earth beneath a humid CO(2) atmosphere suffering electrical discharge.

87 tic composition (<5 % CO(2) ) and condition (humid), CO(2) permeance and CO(2) /Xe selectivity stabil

88 The warm-humid/cold-dry phases of monsoon cycles correspond close

89 Under humid conditions (50% RH), the major end products were 4

90 osity being retained after exposure to harsh humid conditions (90% relative humidity at 353 K).

91 re used as catalysts for the NO oxidation at humid conditions and low temperatures.

92 The colder, more humid conditions and prolonged snow-coverage at north ex

93 n of atmospheric (CH3)2COO may survive under humid conditions and react with SO2, very different from

94 tilization models that already work well for humid conditions but still lack the mechanistically base

95 olumn breakthrough experiments under dry and humid conditions corroborate the excellent CO2 selectivi

96 The results reflect that humid conditions do not have a negative effect in terms

97 ous and the subsequent onset of long-lasting humid conditions during the Late Cretaceous were driven

98 ly Holocene transition and increased as more humid conditions favored forest development after ca. 10

99 Humid conditions first occur at approximately 15 ka, and

100 ons at the interface of hybrid systems under humid conditions has the potential to reveal the local c

101 years ago, coincident with the onset of more humid conditions in central Africa at the beginning of t

102 Rapid changes towards more humid conditions in eastern South Africa as the Northern

103 The combination of warm, humid conditions in neonatal incubators, particularly in

104 ith NO being the major product under dry and humid conditions in the absence of molecular oxygen and

105 s at the polymer/metal oxide interface under humid conditions is vital to understand the long-term du

106 Exposure to humid conditions led to a significant increase in Zn bio

107 mined on bean leaf surfaces maintained under humid conditions or periodically exposed to desiccation

108 jor rise in water levels and a shift to more humid conditions over much of tropical Africa after appr

109 O)2(dobdc), steadily releases bound NO under humid conditions over the course of more than 10 days, s

110 million concentrations of ammonia even under humid conditions was observed.

111 trol experiments (RH < 1%, or no FeCl3 under humid conditions).

112 re error (NRMSE) of 5.5 and 8.4% for dry and humid conditions, respectively.

113 ZnO readily dissolved under humid conditions, whereas ZnS persisted in the dust.

114 African climate changed rapidly towards more humid conditions, while northern sub-Saharan Africa expe

115 f the intervening gas layer in low-pressure, humid conditions.

116 ylene decreased PO2 and PCO2 both in dry and humid conditions.

117 ctions to cause complete depolymerization in humid conditions.

118 ncentration was fixed at 2000 ppm at dry and humid conditions.

119 rawbacks of the instability of ferrate under humid conditions.

120 er, glycerol, and squalane core phases under humid conditions.

121 y and selectivity, particularly under highly humid conditions.

122 y loses 7% of its maximum CO2 capacity under humid conditions.

123 of vocal fold vibration in desiccated versus humid contexts, arid and cold ecologies should be less a

124 of pedogenic carbonates provide evidence of humid cool woodlands with a grassy substrate.

125 accumulation of soil nitrate in Chinese semi-humid croplands based upon more than 7000 samples from 1

126 nitrate reservoir in the vadose-zone of semi-humid croplands, where the nitrate cannot be denitrified

127 nges from increased water content during the humid deposition.

128 is change may be related to fungal growth in humid dust.

129 th fermentation: fusty/muddy sediment, musty/humid/earthy, and winey/vinegary.

130 a transitional zone between the extremes of humid eastern and dry western forest types.

131 In the humid eastern United States, there is evidence of higher

132 e less amenable, when contrasted to warm and humid ecologies, to the development of languages with ph

133 mpling design includes many plots located in humid ecosystems and ignores critical areas for the cons

134 In humid ecosystems, the rate of methane (CH4 ) oxidation b

135 strial ecosystems and decreases from arid to humid ecosystems.

136 s that Eoanabas likewise lived in a warm and humid environment as suggested by the co-existing plant

137 ese sensors exhibited comparable response in humid environment as well, suitable for acetone sensing

138 se without exposing the solid ferrate to the humid environment avoids self-decomposition of the oxida

139 , easy degradation of PQDs in water and in a humid environment is a critical hindrance for applicatio

140 ives the bodies would have decomposed in the humid environment of the tombs.

141 iscible, volatile solvent was deposited in a humid environment on a variety of substrates to achieve

142 , a mode of collective bacterial motility in humid environment through the depinning of bacterial dro

143 l coincides with paleoclimatic change from a humid environment to highly variable and much drier cond

144 At higher coverage and in a humid environment, adsorbate interchange was detected.

145 When exposed to a humid environment, however, fungal growth on wood and st

146 effect of water was more pronounced at high humid environment, while at low RH the matrix plasticiza

147 t role in the migration of microorganisms in humid environment.

148 Humid environments can serve as a reservoir and source o

149 occurring in agricultural workers in hot and humid environments may represent harbingers of the detri

150 In humid environments or biological systems, hydrolytic sta

151 Shrubs in humid environments tend to be hydraulically integrated,

152 We attribute this 'dry' behaviour in humid environments to the presence of curved S-Mo-S plan

153 ubsequent mud formation on solid surfaces in humid environments typically have adverse effects on sur

154 temperature required for radiant cooling in humid environments will form condensation; and 2) cold s

155 in designing better synthetic adhesives for humid environments.

156 some MOFs can be structurally compromised in humid environments.

157 e species tended to be less related in warm, humid environments.

158 : (1) short exposures to moderately warm and humid environments; (2) active warm-up protocols; (3) in

159 northward dispersal likely occurred during a humid episode in the Sahara within Marine Isotope Stage

160 hern margin of Amazonia, which show that the humid evergreen rain forests of eastern Bolivia have bee

161 biomarkers (even at p.p.b. levels) in highly humid exhaled breath.

162 This work evaluated the humid extraction of barley beta-glucans and partially ch

163 adsorption-desorption cycling with simulated humid flue gas and enables regeneration using low-temper

164 cm) of three ecosystems (semiarid, subhumid, humid) for one year.

165 vanna zones in the north gradually turn into humid forest zones in the south).

166 ize variation along temperature gradients in humid forests may therefore reflect a trade-off between

167 Sites in closed humid forests of northwest Madagascar and a montane eric

168 ozone recovery in a colder and possibly more humid future Arctic lower stratosphere.

169 limits of low proton affine analytes even in humid gas mixtures containing high proton affine compoun

170 is mandatory to obtain reliable analyses of humid gaseous media such as ambient air and exhaled brea

171 Stability in both gaseous (such as humid gases) and aqueous media is considered.

172 ent with adjacent "hot," "cold," "dry," and "humid" glomeruli-an organization that allows for both un

173 In a temperate, humid grassland, we examined the seasonal impacts of cli

174 oss of kleaf and turgor loss point) than the humid-habitat Ranunculus lanuginosus Accordingly, water

175 These lineages originated in humid habitats and colonized dry/seasonally dry environm

176 ies living in tropical, densely forested and humid habitats in Africa have evolved darker faces.

177 Furthermore, humid heat affects both performance and thermoregulatory

178 V-1 DNA in dried blood spots (DBS) stored in humid heat and at -20 degrees C.

179 CP) (>=12 months) during exercise in dry and humid heat, across their active OCP cycle.

180 ) ] eumenorrheic women exercising in dry and humid heat, across their menstrual cycle.

181 d, flies avoided dry heat more robustly than humid heat, and this modulation was abolished by silenci

182 across the menstrual cycle, yet is lower in humid heat, in conjunction with reduced evaporative cool

183 rual cycle phase, but differ between dry and humid heat.

184 associated with menstrual phase and dry vs. humid heat.

185 nd quasi-luteal (qL) phases in dry (DRY) and humid (HUM) heat matched for wet bulb globe temperature

186 and mid-luteal (ML) phases in dry (DRY) and humid (HUM) heat matched for wet bulb globe temperature

187 This study investigates the impact of humid indoor conditions on the bioaccessibility of Zn in

188 northern and southern hemispheres, producing humid intervals in one hemisphere matched to aridity in

189 It consists in exposing humid kernels to high steam pressure followed by a decom

190 ing, reveal that landslide frequency in many humid landscapes may be insensitive to projected changes

191 Recharge in some humid locations varies by as little as five per cent (by

192 We show that humid, low-elevation communities are phylogenetically ov

193 the contemporary northern limit (colder and humid maritime regions; Denmark and Norway) will probabl

194 to the ecological opportunities provided by humid, megathermal forests, which were increasingly avai

195 Humid montane forests are challenging environments for h

196 reatest in species with the coldest and most humid native ranges, respectively.

197 hat is capable of >=90% CO(2) capture from a humid natural gas flue emission stream, as confirmed by

198 radation upon exposure to dry air/oxygen and humid nitrogen/water environments, thus separating the e

199 breakthrough experiments using both dry and humid NO(2) gas streams verify the excellent stability a

200 Flies inhabiting the colder and more humid north-facing slope carried about 6% more transposa

201 C stocks in arid sites but decreased them in humid ones.

202 However, these membranes require humid operating conditions, which limit the temperature

203 Only when the overlying air is humid or droplet concentrations are very low does suffic

204 tural conditions comprise half of the global humid or moist tropical forest estate, largely limited t

205 ith the transition between the Iberian Roman Humid Period and the Migration Period.

206 of the onset and termination of the African Humid Period are contested, with strong evidence for bot

207 nd termination of the Early Holocene African Humid Period are subjects of ongoing debate, with direct

208 strong terrestrial evidence that the African Humid Period ended abruptly, supporting the hypothesis t

209 rupt transitions into and out of the African Humid Period in northeast Africa.

210 suggests that the termination of the African Humid Period in the Horn of Africa occurred within centu

211 hemispheric coherence of this early African Humid Period is challenging due to opposing seasonal ins

212 deposition of F- and Na+ during the African Humid Period suggests rapidly fluctuating lake levels be

213 sal was possible because during the Holocene humid period the region contained a series of linked lak

214 ad timing of this period, termed the African Humid Period, is well known.

215 mong Near Eastern farmers during the African Humid Period.

216 in this region, possibly during the Holocene humid period.

217 anges in atmospheric wet deposition (arid vs humid periods).

218 Hominin occupations correspond with humid periods, particularly Marine Isotope Stages 7 and

219 exception, correspond approximately to warm-humid phases caused by a strengthened monsoon.

220 animals and humans populated it during past humid phases.

221 These conditions led to humid pulses in South Africa and potentially to the crea

222 vegetation ranging from wooded savannahs to humid rainforest.

223 NE-II serotype was more common in hot, humid regions (P = .02) but was also present in other re

224 uggesting that any land cover changes in non-humid regions (P/PET<1) or in watersheds of low water re

225 refore leave peatlands that dominate dry sub-humid regions across the boreal, on the edge of their cl

226 However, more humid regions are more likely to increase SOC only, whil

227 ater-resource and land-use management in sub-humid regions of the world.

228 In most humid regions worldwide, the characterization factor is

229 conventional oil (semiarid regions) and gas (humid regions) plays.

230 are most likely to occur over humid and semi-humid regions, such as southern and northeastern China.

231 e darkest flies were collected from the most humid regions.

232 to be a major cause of rock fracture in cold humid regions.

233 sure risk of flash drought over southernmost humid regions.

234 Here, we report the identification of the humid-responding neuron that completes the hygrosensory

235 n the Vaejovis vorhiesi group, restricted to humid rocky habitats in mountains across southwestern No

236 d in four clusters representing dry savanna, humid savanna, dry forest and moist forest, characterize

237 on and climate-induced conversions among sub-humid, semi-arid, arid, and hyper-arid subtypes will lea

238 al closure) than conspecific plants from the humid site.

239 However, SOC losses in humid sites were counterbalanced by the effect of planta

240 both structure and porosity under prolonged humid SO(2) exposure whereas many other well-known ZIFs

241 OM) is correlated with reactive iron (Fe) in humid soils, but Fe also promotes SOM decomposition when

242 Periodic O(2) limitation is common in humid soils, so Fe does not intrinsically protect OM; ra

243 Near room temperature, the humid source produces abundant gold-hydroxy cluster anio

244 GW depletion was to transport water from the humid south.

245 he school term in late May-June 2009 in more humid southeastern states), school vacations (preventing

246 arlier societal disruption in the relatively humid southern Maya Lowlands.

247 outbreaks of pandemic influenza during more humid spring, summer, and autumn months might appear to

248 from a cold-dry polar-type climate to a warm-humid sub-Antarctic-type climate.

249 India's humid subtropical region experienced a unique summer pne

250 (C(2) ) from humid subtropical to arid habitats on the coasts of the

251 cal, predominantly deciduous), early Eocene (humid subtropical, mixed deciduous and evergreen), and m

252 cal patterns over topoclimate gradients in a humid temperate broadleaf forest in southern Appalachian

253 seful to enhance ecohydrological modeling in humid temperate forests.

254 ated human malaria, including P. vivax, into humid temperate or warm climate refuges around the Medit

255 dry tropical Slope (AS) and a European-like humid temperate Slope (ES), separated by 250 meters.

256 f 29 dryland rivers with catchments across a humid to arid gradient covering >1,800,000 km(2) of cont

257 aracterized by a substantial transition from humid to drier conditions during the Early (925-1150 C.E

258 ly show that the Tortonian Europe mainly had humid to subhumid summers and no arid climate has been c

259 of current agro-industrial scale clearing in humid tropical Africa.

260 Oxisol soils are widely distributed in the humid tropical and subtropical regions and are generally

261 Glaciation in the humid tropical Andes is a sensitive indicator of mean an

262 nated in the region, which formed a warm and humid tropical archipelago in the Early Triassic.

263 Red junglefowl, which lives in humid and sub-humid tropical areas.

264 radiant cooling system that made the hot and humid tropical climate of Singapore feel cool and comfor

265 tion satellite datasets was used to quantify humid tropical forest clearing from 2000 to 2005.

266 ca contributes 5.4% to the estimated loss of humid tropical forest cover, reflecting the absence of c

267 We present a worldwide analysis of humid tropical forest dynamics and tree species richness

268 of redox fluctuations on lignin breakdown in humid tropical forest soils during ten-week laboratory i

269 and represents a 2.36% reduction in area of humid tropical forest.

270 Long-term monitoring of plots in mature humid tropical forests concentrated in South America rev

271 Humid tropical forests have the fastest rates of organic

272 Psychotria marginata, a shrub common to humid tropical forests in Central America, produces leav

273 ntributes to rapid rates of C cycling across humid tropical forests in spite of periodic O2 limitatio

274 constant proportion (9%) of biomass, but in humid tropical forests this ratio varies from 2% in undi

275 ions for understanding the global ecology of humid tropical forests, and their functional responses t

276 fference between the two models occurred for humid tropical forests, where the CLM-CN simulated a 62%

277 ional species pools and local assemblages in humid tropical forests.

278 crease the accuracy of ecological studies in humid tropical forests.

279 omote forest regeneration and restoration in humid tropical lowland areas with high biomass resilienc

280 ed the largest area of GFCL, followed by the humid tropical, dry tropical, and temperate biomes.

281 esculenta) is an important root crop in the humid tropics and a valuable source of essential mineral

282 However, every year vast areas of the humid tropics are disturbed by selective logging, unders

283 Extrapolation to perennial plants in the humid tropics is risky because functional relationships

284 Terrestrial ecosystems in the humid tropics play a potentially important but presently

285 ritionally rich fruit crop indigenous to the humid tropics, known by their place of origin.

286 rather unfavorable climate conditions of the humid tropics.

287 ighest in the boreal biome and lowest in the humid tropics.

288 tent estimates of forest clearing within the humid tropics.

289 uxes from land to water to atmosphere in the humid tropics.

290 ide food for over 800 million throughout the humid tropics.

291 nd 0.8 +/- 0.3 for rubber plantations in the humid tropics; and (ii) land use management policies sho

292 nd orders differently on both plastics under humid versus dry environments.

293 y volunteers randomized to simulated hot and humid vs nonhumid conditions.

294 es and vegetation during the late Paleocene (humid, warm temperate to subtropical, predominantly deci

295 10(-6)s(-1) and 1.05x10(-6)s(-1) for dry and humid weather respectively.

296 urrence of disease is best predicted by wet, humid weather.

297 ace mixed layer was also observed to be more humid with higher relative humidity.

298 2) in the West African Sahara, Sahel and sub-humid zone, using submetre-resolution satellite imagery

299 ly occur in hyper-arid zones and smallest in humid zones, highlighting the dependency on available su

300 cation of fossil-rich outcrops and temperate humid zones, indicating that climate change from arid to