ライフサイエンスコーパス: spring

1 ies of a random coil and acts as an entropic spring.

2 tiates under day-neutral conditions of early spring.

3 ectodomain can act as a stiff or soft gating spring.

4 pollen into the air every year during early spring.

5 igh [CO(2) ] for many generations in a CO(2) spring.

6 s occurs in people born in late winter/early spring.

7 transcriptions of the wheat landrace Chinese Spring.

8 rcuits, where MOR availability peaked during spring.

9 ers advances from low to high latitudes each spring.

10 Bacteroidetes dominated the PR expression in spring.

11 causing larger greenhouse gas losses during spring.

12 rmant through the winter before flowering in spring.

13 minated over oxyanions in many Icelandic hot springs.

14 cilia mexicana, Poeciliidae) from H(2)S-rich springs.

15 tributed among Yellowstone National Park hot springs.

16 laciers, but also snowfields and groundwater springs.

17 een almost no research on the effects of toe springs.

18 tributed up to a few tens of percent in some springs.

19 were also greater in early compared to late springs.

20 From spring 2015 to fall 2017, we quantified adult abundance

21 ginated from domestic anseriforms, either in spring 2016 in east China or in autumn 2016 in central E

22 In spring 2018, the American Heart Association convened the

23 onavirus Disease 2019 (COVID-19) outbreak in Spring 2020.

24 politan area during the COVID-19 outbreak in spring 2020.

25 the highly reducing sediment of Colour Peak springs, a sulfidic and saline spring system located wit

26 ges of advancing (~75%) trends, but farmers' spring activities were the only group with reinforced ad

27 Temporal changes in both spring activity date and early season forage "wait times

28 Our results show that spring activity date is largely dictated by snow melt ch

29 Spring activity date was related to snow cover dynamics

30 Predicted spring activity date was then compared with a daily spri

31 onsistency explained 45% of the variation in spring activity date.

32 Telemetry data were used to identify spring activity dates for 48 individuals in the Yellowhe

33 virtually no areas with significantly later spring activity dates were detected.

34 ure and a transition from winter dormancy to spring activity.

35 g snow melt conditions may result in earlier spring activity.

36 se of their webs for external latch-mediated spring actuation [4].

37 erage and minimum) from late winter to early spring affected the timing of cambial reactivation and x

38 daytime and nighttime periods in autumn and spring, aiming to address the seasonal and day-night var

39 verse dynamics techniques, we found that toe springs alter the joint moments and work at the toes suc

40 consisted of 32 adult eagles tracked for 45 spring and 39 fall migrations from 2014 to 2017.

41 f picoeukaryotic phytoplankton (PEUK) during spring and after spikes in river flow were also detected

42 Seed from populations at the CO(2) spring and an adjacent control site (ambient [CO(2) ]) w

43 T shifts forward and backward by one hour in spring and autumn by comparing the observed and expected

44 ong time series was recently produced of the spring and autumn migration phenology of Brazilian free-

45 uring spring migration and carnivores during spring and autumn migration that migrated across the ent

46 west and the centre of the continent during spring and autumn migration, and carnivores in the west

47 , herbivore-granivores and granivores during spring and autumn migration, except for omnivores in the

48 nt of their annual distributions during both spring and autumn migration, has not been explored.

49 ion, and for nectarivores in the west during spring and autumn migration.

50 termine where and when birds stopover during spring and autumn migration.

51 FORCCHN2 simulates spring and autumn phenological events from heat and chil

52 However, CH(4) emissions in spring and autumn shoulders are often underestimated by

53 reland and Scotland (wintering) and Iceland (spring and autumn staging).

54 lance radars to estimate over 50% SPR during spring and autumn through the Gulf of Mexico and Atlanti

55 l communities in monthly incubations between spring and autumn under different environmental conditio

56 bimodal distribution of acoustic presence in spring and autumn, corresponding to their expected migra

57 sponse to climate change in opposite ways in spring and autumn.

58 ll genetic differentiation between the CO(2) spring and control site populations was found, with evid

59 and railroads affected movement during both spring and fall migrations, but eagles selected areas ne

60 entrations found in the samples collected in spring and in southern Spain.

61 birds concentrated close to the coast during spring and inland in forested landscapes during autumn,

62 patterns which correlate with peaks in late spring and late fall/early winter in California.

63 iation in the timing of events is greater in spring and less in autumn than if all populations follow

64 uspended sediment concentrations (SSC), over spring and neap tides.

65 Each fire occurred during fall or spring and stimulated flowering in the subsequent summer

66 Trends in farmers' spring and summer activities were very likely/likely ass

67 le (AF) seasonal ranges more than doubled in spring and summer and were significantly larger in all m

68 rge increases in abundance, typically in the spring and summer followed, by rapid declines within wee

69 sequential extraction on cores collected in spring and summer from two small agricultural streams in

70 ecreased chilling the advancing phenology in spring and summer is still attributable to warming; even

71 .e., increase of temperature and humidity as spring and summer months arrive in the Northern Hemisphe

72 column from the major basins of each lake in spring and summer over 2 years.

73 Although spring and summer phases in wild plants advanced less (m

74 ated with winter and spring temperatures and spring and summer precipitation, and positively correlat

75 Water profiles during the 2018-2019 southern spring and summer stormy seasons show that high-altitude

76 in four periods of the year (autumn, winter, spring and summer).

77 centrations were similar to within 5% during spring and summer, but mobile P binding fractions nearly

78 can be captured across the United States in spring and summer, while capacity lowers to 0-5 L/m(2)/d

79 flux occurred during peak river discharge in spring and summer.

80 ncentrations reached almost 100 ng/L in late spring and summer.

81 ANO, the current state-of-the-art compressor SPRING and the general compressor pigz on several public

82 ieved a success rate of 68.2%, outperforming SPRING and ZDOCK, with success rates of 52.1% and 35.9%

83 the onset of canopy-level photosynthesis in spring, and its cessation in autumn.

84 risk, complicating forecasts of future false springs, and potentially reshaping plant community dynam

85 trends in fall near the coastal area and in spring around the north area.

86 chanisms, we forecast future trajectories of spring arrival and evaluate the consequences for forest

87 business-as-usual' climate scenario, earlier spring arrival will enhance NPP of temperate and boreal

88 In some Icelandic hot springs, arsenic was nearly quantitatively thiolated.

89 Replicating spring assisted cranioplasty in LC patients allow to tun

90 Surgical correction including the spring assisted cranioplasty is the only option to corre

91 However, the aesthetic outcome from spring assisted cranioplasty may remain suboptimal.

92 50 zJ, from a nano-electromechanical torsion spring at the single molecule level.

93 amples of life's resilience, thriving in hot springs at boiling temperatures, in brine lakes saturate

94 trends were present, being stronger in early spring, at higher elevations, but smaller for nonwoody i

95 ques to trace foliar P uptake in P-deficient spring barley (Hordeum vulgare) and to monitor the effec

96 ntly improving upon the ENSO predictability "spring barrier".

97 In the open Southern Ocean, the spring bloom magnitude is found to be greatest in areas

98 ious for summer-blooming species compared to spring-bloomers driven by their strongly differing offse

99 s for summer-blooming species and herbaceous spring-blooming species.

100 The combination of earlier spring blooms and lower summer food quantity and quality

101 piNET has been built using a modular Spring-Boot JAVA platform as a fast, versatile and easy

102 acquired in fall to fuel winter survival and spring breeding, increased winter energy requirements ha

103 rmyard manure (FYM) or pea vines, no burn or spring burn with application of N fertilizer (0, 45, and

104 creased with higher temperature anomalies in spring but decreased in summer.

105 lowest energy costs and largest reserves in spring, but in cold localities, they risk freezing.

106 o increase earlier from late winter to early spring, cambial reactivation occurred earlier.

107 namics method based on a coarse-grained bead-spring chain model has been proposed to compute the opti

108 action norms tend to accentuate responses in spring (cogradient variation) and attenuate them in autu

109 theless, leaf C:N was low for summer- versus spring-collected plants, consistent with a life history-

110 cted areas near roads to a greater degree in spring compared to fall and at higher latitudes compared

111 is from the Rhynie and Windyfield cherts hot spring complex in Scotland, reveals details of head stru

112 Canada during the anomalously warm winter to spring conditions of 2015 and 2016 (relative to 2010-201

113 e activity through an association with drier spring conditions resulting from weaker moisture transpo

114 om three different LC patients who underwent spring correction were reconstructed from the pre-operat

115 up-call detections in late winter and early spring corresponding to the season when right whales con

116 at the toes such that greater degrees of toe spring curvature resulted in lower work requirements dur

117 uito is well-characterized by a passive mass-spring-damper model which permits the calculation of for

118 There is evidence that the spring Daylight Saving Time (DST) transition acutely inc

119 . shade-grown coffee plantations) relates to spring departure date and migration pace in Swainson's T

120 For Neotropical migrant songbirds, early spring departure from wintering sites, early arrival to

121 Because spring DST also shifts clock time 1 h later, mornings ar

122 We estimate that each spring DST shift is associated with negative health effe

123 stress (such as that experienced around the spring DST shift) on the immune system.

124 hat appear to decrease immediately after the spring DST shift, enriched with infections and immune sy

125 ss all states (1996-2017), and observed that spring DST significantly increased fatal MVA risk by 6%,

126 Biomass production increased in spring due to a warming-induced earlier onset of plant g

127 es) and were compared to U concentrations in spring-dwelling mayflies.

128 Climate cycle indices of spring ENSO, summer NAO, and winter or spring PDO accoun

129 se, given the low host cell densities of hot spring environments, that the TSPV1 filaments serve to i

130 ates marked shifts in the relative timing of spring events across trophic levels and mismatches in th

131 While it is generally recognized that toe springs facilitate the forefoot's ability to roll forwar

132 erance in 10 independent lineages of sulfide spring fishes across multiple genera of Poeciliidae is c

133 s exhibited the highest pathogen loads, with spring floral resources and nesting habitat availability

134 of wintersweet, such as floral transition in spring, floral organ specification, low temperature-medi

135 Subseafloor mixing of high-temperature hot-spring fluids with cold seawater creates intermediate-te

136 activity date was then compared with a daily spring forage availability date dataset, resulting in "w

137 d to simulate the skull expansion due to the spring forces and skull growth between surgery and post-

138 ased winter chilling combined with increased spring forcing limited change in their phenology.

139 Temperate forests are shaped by late spring freezes after budburst - false springs - which ma

140 es, and thioantimonates, in sulfide-rich hot springs from Yellowstone National Park and Iceland is sh

141 The data further highlight how extreme spring frost events can result in significantly increase

142 We find that spring frost events induce farm gate price drops and thu

143 whereas other species appear to be adding a spring generation, revealing a possible shift from vagra

144 A field experiment with 65 spring genotypes and 9 winter genotypes of camelina was

145 show that drought shortened the duration of spring green-up by approximately twofold (2.5 weeks) and

146 ts this important seasonal process and shows spring greenhouse gas emissions are largely due to produ

147 The results showed that warm temperatures in spring had a positive effect on NEP in conifer forests b

148 d on motorised boreholes in lowland areas as springs, hand-dug-wells and open sources failed.

149 Our results help explain why toe springs have been a pervasive feature in shoes for centu

150 ), two treatments were applied: (b) two late-spring heatwaves (June, July) followed by a summer heatw

151 ll reports were presented at the APA Virtual Spring Highlights Meeting, April 25-26, 2020.

152 The osteotomies and spring implantation were performed to simulate the skull

153 The stiffness and tunability of the I-band spring implicate titin as a force contributor that, duri

154 fundamental role as an activation-dependent spring in contracting muscle.

155 We conclude that a titin-like dynamic spring in the I-band, made by an undamped elastic elemen

156 is an important source of water during early spring in these water-limited ecosystems, and it can als

157 m a Thermoproteales host isolated from a hot spring in Yellowstone National Park (USA).

158 chemistry and U measured in periphyton from springs in Grand Canyon (United States) and were compare

159 Unpowered exoskeletons with springs in parallel to human plantar flexor muscle-tendo

160 gadi, a hypersaline alkaline lake fed by hot springs in the semi-arid southern Kenya Rift Valley.

161 onditions characteristic of the volcanic hot springs in which these archaeal extremophiles reside.

162 ion of temperature from late winter to early spring is a critical factor in determining the timing of

163 acteristics, a piezovoltage is applied and a spring is connected to the sliding end of the deformable

164 ean ecosystems (which show maximum uptake in spring), it is in phase with the seasonal cycle of urban

165 ociated with densities of breeding males two springs later.

166 Climate warming is currently advancing spring leaf-out of temperate and boreal trees, enhancing

167 out-of-plane magnetic field, and an exchange spring-like magnetic depth profile when the system is ma

168 d AMP concentrations as temperatures warm in spring likely means greater secretion rates, the subsequ

169 The reactivity of spring-loaded cyclic reagents is dominated by transforma

170 ally, groundwater discharging at hundreds of spring locations in and near Grand Canyon supports impor

171 ed to sleeping on LR or sleeping directly on spring mattresses without a topper.

172 ty to roll forward at the end of stance, toe springs may also have some effect on natural foot functi

173 hoes for centuries but also suggest that toe springs may contribute to weakening of the foot muscles

174 icing events may cause die-offs, and earlier springs may generate a trophic mismatch in phenology, th

175 ures did contribute strongly to the observed spring migration advancements over the 55-y study period

176 on was also observed for insectivores during spring migration and carnivores during spring and autumn

177 l hypothesis of equal survival and timing of spring migration for High Arctic breeding sanderling Cal

178 Instead, spring migration phenology seems to be predominantly dri

179 ely (~80%) explains interannual variation in spring migration phenology.

180 Flexibility in spring migration timing of long-distance migrants to exo

181 e wind conditions have, furthermore, allowed spring migration to occur 16 days earlier.

182 for insectivores in the west and east during spring migration, and for nectarivores in the west durin

183 migration, and carnivores in the west during spring migration.

184 the phenology of vegetation greenness during spring migration.

185 ion, except for omnivores in the west during spring migration.

186 to accumulate forage resources during rapid spring migrations.

187 e effect of ageing was remarkably evident on spring migratory performance and phenology.

188 Each spring, migratory birds travel tens to tens of thousands

189 In response to a warming planet with earlier springs, migratory animals are adjusting the timing of e

190 end, we developed a coarse-grained bead-and-spring model and investigated its properties through Bro

191 sing a statistical mechanics-based torsional spring model, we extracted values of the chromatin twist

192 Mass-spring models have been a standard approach in molecular

193 a trend dominated by decreased snow cover in spring months.

194 to increased snow exposure in the winter and spring months.

195 erent sample stresses were used to construct spring networks characterized by Hessian and damping mat

196 t, with an average improvement over pigz and SPRING of >24.7% and 6.3%, respectively.

197 velopment of mental health complaints in the spring of 2020.

198 reduction in acidic hyperthermal terrestrial springs of the Kamchatka Peninsula and attributed DSR in

199 le is known about life in the boron-rich hot springs of Trans-Himalayas.

200 ta, a symbiotic archaean found in acidic hot springs of Yellowstone National Park, USA.

201 This study investigated the effects of toe springs on foot biomechanics in a controlled experiment

202 erucic acid in winter forms is lower than in spring ones.

203 perature, winter chilling, and the timing of spring onset, we accurately predicted reductions in the

204 did not find temperature to influence either spring or autumn migration.

205 intained in the presence of H(2)S in sulfide spring P. mexicana but not ancestral lineages from nonsu

206 After bonding open spring palatal expanders for 3-day, 5-day, 7-day, and re

207 es of spring ENSO, summer NAO, and winter or spring PDO accounted for 40-54% of the variation in gras

208 ibuted members from terrestrial thermal acid springs (pH < 4; T > 65 degrees C).

209 Findings for crop spring phases were similar, but were less pronounced.

210 Globally, spring phenology and abiotic processes are shifting earl

211 ndings suggest that interannual variation in spring phenology could be much stronger in the future in

212 Spring phenology has mostly advanced, but large, unexpla

213 a indicate significant advancement in alpine spring phenology over decades of climate warming, but co

214 ough positive responses to rapidly advancing spring phenology.

215 P and chlorophyll a, and these indicate that spring phosphorus loads are a weak algal biomass predict

216 Spring phytoplankton blooms in temperate environments co

217 ute to 'sustained quenching' of winter/early spring pine needles, time-resolved fluorescence analysis

218 Transdermal drug delivery using spring-powered jet injection has been studied for severa

219 formance and high thermal sensitivity into a spring-powered system with extreme performance and funct

220 Surveys in winter and spring produced the best datasets, and, as post-burial t

221 curvature in the toe region to simulate toe springs ranging from 10 to 40 degrees of curvature.

222 d wheat (Triticum aestivum) cultivar Chinese Spring reference genome allows a detailed study of its N

223 domains preferentially from the distal titin spring region become oxidized in vivo through the mechan

224 ion profiles of populations derived from the spring relative to the control population, providing the

225 est that climate change-which will make most springs relatively "early"-could lead to a future with m

226 diffusion and ebullition and 2.6-3.3 Tg from spring release of CH(4) stored in bubbles in winter lake

227 ents that reach the atmosphere (ebullition); spring release of CH(4) trapped in bubbles in and under

228 ds, ENANO is 2.9x and 1.7x times faster than SPRING, respectively, with memory consumption up to 0.2

229 vered from samples collected during fall and spring, respectively; these are subtypes that can have s

230 potentially magnified the variation in false spring risk among species with an increase in risk for e

231 which were the strongest predictors of false spring risk and how these predictors shifted with climat

232 All predictors influenced false spring risk before recent warming, but their effects hav

233 ate change has reshaped the drivers of false spring risk, complicating forecasts of future false spri

234 on the multiple underlying drivers of false spring risk.

235 onstrained by a phenological "green wave" of spring salt marsh productivity at breeding sites.

236 The date of spring sea-ice retreat in the previous year was positive

237 ferent environments (E) in the 2017 and 2018 spring seasons.

238 ffect is limited in BP lattices due to their spring-shaped space structure.

239 on rate-and-state friction in the manner of spring-sliders, and analyze conditions for the emergence

240 Here, we examine how changing spring snow cover dynamics and early season forage avail

241 ular migrant, all followed, as expected, the spring snowmelt during their migrations.

242 ing to the Arctic are expected to follow the spring snowmelt to optimise their arrival time and selec

243 n warmer, wetter conditions on the Icelandic spring staging grounds and survival.

244 en by wind conditions at likely wintering or spring stopover areas during the migration period.

245 e of budburst more in early compared to late springs, suggesting that to simulate interannual variabi

246 tion, and delta(13) C(ph) monthly throughout spring, summer, and autumn in Eucalyptus tereticornis gr

247 derable heterogeneity of movement, including spring/summer accelerations.

248 slow-growing winter annuals to fast-growing spring/summer annuals.

249 that could be used in the future to optimise spring surgery.

250 Both signals are generated using an elastic spring system (ESS), which includes a protractor muscle

251 f Colour Peak springs, a sulfidic and saline spring system located within the Canadian High Arctic.

252 alt marsh biomass accumulation and with peak spring temperature acceleration (GDD jerk).

253 Here, we assessed the effects of mean spring temperature, distance from the coast, elevation a

254 ng was negatively correlated with winter and spring temperatures and spring and summer precipitation,

255 n cold snap occurrence and generally warming spring temperatures can affect reproductive success and

256 While increased spring temperatures did contribute strongly to the obser

257 Similar approaches were applied to spring temperatures to detect extreme years and to the t

258 (up to 30 days) in 1983 and 1996 due to cool spring temperatures.

259 h is consistent with the greater increase in spring than summer temperatures recorded for this region

260 with the sarcomere end, working as an I-band spring that accounts for the rise of passive force with

261 measure the undamped stiffness of an I-band spring that at SL > 2.7 um attains a maximum constant va

262 The extreme warm spring that occurred in 2012 resulted in the occurrence

263 nclude that the carotenoid does not act as a spring that, releasing its internal strain, induces the

264 ) flux (0.88 +/- 0.03 mg m(-2) hr(-1) ) than spring thaw (0.48 +/- 0.04 mg m(-2) hr(-1) ).

265 9 days) is significantly longer than that of spring thaw (20.94 +/- 7.79 days), which predominates th

266 280.39 mg m(-2) year(-1) ) than that during spring thaw (307.39 +/- 46.11 mg m(-2) year(-1) ).

267 is study investigates CH(4) emissions during spring thaw and autumn freeze using eddy covariance CH(4

268 teresis effect on CH(4) emissions from early spring thaw to late autumn freeze.

269 es and differences in CH(4) emissions during spring thaw versus autumn freeze to accurately estimate

270 ission to total annual emission than that of spring thaw.

271 d subsequently in terrestrial geothermal hot springs, the Nanoarchaeota species that have been descri

272 infusa) complete an astonishing journey: In Spring, they migrate over 1,000 km from their breeding g

273 eDNA in the bay on a near monthly basis from spring through mid-fall in 2018 and 2019.

274 During spring, time spent near linear features often occurred d

275 /- 1.3 Tg N[Formula: see text] in the boreal spring to a high of 5.5 +/- 2.0 Tg N[Formula: see text]

276 .7-3.1 um, showing the ability of the I-band spring to adapt its length to the width of the I-band.

277 motypic interactions within the distal titin spring to stabilize this segment and regulate myocardial

278 Maumee spring TP load was not strongly related to lake TP, and

279 prior to the final frost date of the winter/spring transition may damage flower buds or open flowers

280 y 90 g/m(2) more carbon during the winter to spring transition than in other recorded years.

281 allowing time to heal graft wounds prior to spring transplanting or double cropping is suitable for

282 However, photosynthetic enhancement from spring warming was partially offset by greater ecosystem

283 nds were strongly attributable to winter and spring warming.

284 delayed senescence in response to winter and spring warming.

285 The spring-water chemistry and sinter mineralogy were domina

286 In the warm spring, we found that photosynthesis was enhanced more t

287 are soil deposited by an extinct iron-sulfur spring, we found that WPS-2 comprised up to 24% of the b

288 The precise time window during which spring weather advances phenology varies considerably ac

289 uctive condition per annum was influenced by spring weather conditions, (iii) in both species males t

290 tudy period, supporting the possibility that spring weather regime shifts contributed to the increasi

291 rong (Pembina) and a weak (Harvest) hard red spring wheat flour were examined at a 1 and 2% salt leve

292 explore the geomicrobiology of a 4438-m-high spring which emanates ~70 degrees C-water from a boratic

293 y late spring freezes after budburst - false springs - which may shift with climate change.

294 g summer and fall, and ease-of-travel during spring, while patterns of selection during winter aligne

295 nfluence on net CO(2) exchange in winter and spring, while soil moisture has a primary control on net

296 transcriptome time series for Brassica napus spring, winter, semi-winter, and Siberian kale crop type

297 mille) during summer and high values during spring/winter (0 to - 3 per mille), while 70% of the ann

298 s from frog skeletal muscle reveal an I-band spring with an undamped stiffness 100 times larger than

299 ly present in the archipelago from autumn to spring with marked seasonal differences in the use of di

300 ence predictions of a template-based method (SPRING) with a template-free method (ZDOCK).