ライフサイエンスコーパス: cloud

1 ater droplets and ice particles (mixed-phase clouds).

2 riments 1 & 2) and recognition memory tests (cloud-?

3 ing to a single detection, that form a point cloud.

4 measure the distance to the Large Magellanic Cloud.

5 eed and is often executed in parallel on the cloud.

6 per sample on c5.18xlarge instance of Amazon Cloud.

7 cale genomic analyses on public and academic clouds.

8 trations tend to produce more boundary layer clouds.

9 reflectance, and lifetime of warm low-level clouds.

10 important organic hydroperoxides present in clouds.

11 wave interferometry with free-falling atomic clouds.

12 t low latent heat flux tend to dissipate low clouds.

13 ng photon scattering from points beneath the clouds)(1-3,7,8,10-12).

14 ing flash occurrences over five hours (57 in cloud, 18 cloud-to-ground).

15 Stream is made up of gas stripped from both clouds(2,6,7) and that the majority of this gas is ioniz

16 t photons control the lifetimes of molecular clouds(3-7).

17 n rates, longer average lifetime, and higher cloud albedo and cloud fraction compared with unpolluted

18 as multiple cloud platforms, such as Google Cloud, Amazon Elastic Computing Cloud, Microsoft Azure a

19 plexity could be explained by the changes in cloud amount, and we research that possibility by invest

20 this article, we employ text mining and word cloud analysis techniques to address these challenges.

21 re uploaded continuously via smartphone to a cloud analytics platform.

22 ion of biomass-burning INPs into atmospheric cloud and climate models.

23 n each sample were generated using both read cloud and conventional assembly.

24 s change from 2003 to 2019 using NASA's Ice, Cloud and land Elevation Satellite (ICESat) and ICESat-2

25 However, deforestation-related cloud and radiation effects manifest in coupled climate

26 t visualization of the pacing lead on the HB cloud and reproducible navigation to predetermined HB ca

27 Cloud and sediment formation is a major problem in juice

28 stituents in a spherical atmosphere, such as clouds and aerosols, alter the total amount of energy re

29 es high enough to be relevant to mixed-phase clouds and are active over a wide temperature range, nuc

30 Aerosol effects on convective clouds and associated precipitation constitute an import

31 onary satellite observations provided by the Clouds and Earth's Radiant Energy System (CERES) Synopti

32 his chemistry occurs in "dense" interstellar clouds and protostellar disks surrounding forming stars

33 melting and evaporation to the formation of clouds and the initiation of neurodegenerative diseases(

34 In the central Arctic Ocean the formation of clouds and their properties are sensitive to the availab

35 heric processes that affect the evolution of clouds and their properties including radiative forcing

36 ore-CYPome), CYP co-occurrence networks, CYP clouds, and genome clustering data.

37 ations, we find that abundant boundary layer clouds are associated with low lead flux periods, while

38 ale of about one parsec, indicate that these clouds are mixing with the warmer medium and are possibl

39 ead flux periods, while fewer boundary layer clouds are observed for high lead flux periods.

40 g is inconsistent with the notion that these clouds are part of a ring, bringing the Gould Belt model

41 onstriction sites, whereas dynamic myosin II clouds are present in the vicinity of constrictions.

42 helion, and supersaturation occurs even when clouds are present.

43 HB cloud area was 360 (212) mm(2).

44 ce located in the nearby Ophiuchus molecular cloud at a distance of 144 parsecs(9), and is one of the

45 y eventually break up into scattered cumulus clouds, at concentrations exceeding 1,700 parts per mill

46 s new constraints on the dynamics of the sub-cloud atmosphere.

47 mote participants; (4) extensive reliance on cloud-based artificial intelligence (AI) for data analys

48 (n = 23,763), using the Analysis Commons, a cloud-based computing platform.

49 erapeutic modifications to source content, a cloud-based content management system that enables treat

50 Here we developed Cumulus-a cloud-based framework for analyzing large-scale single-c

51 Accessible via standard or cloud-based implementation, CICERO enhances driver fusio

52 a newly developed algorithm that uses point cloud-based morphometry to unpack the rich information e

53 Information Exchange (PeCanPIE), a web- and cloud-based platform for annotation, identification, and

54 th key partners, developed and implemented a cloud-based System for Tracking Epidemiological Data and

55 intained robustness, as well as standardized cloud-based workflows for PDX exome-sequencing and RNA-s

56 The sentences themselves, and word clouds built from them, provide effective summaries of t

57 cts show the characteristics of gas and dust clouds but display the dynamical properties of stellar-m

58 les are ubiquitous in interstellar molecular clouds, but their fundamental formation mechanisms have

59 icism and negative emotional variability was clouded by a dependency between variability and the mean

60 giant planets such as Jupiter, the motion of clouds can be compared with radio emissions from the mag

61 We find that motion of the clouds can be described well based on the peculiarities

62 erformed under atmospheric conditions in the CLOUD chamber at CERN, that below about +5 degrees Celsi

63 r measurements, from a multiphase, turbulent cloud chamber, show a clear transition from a regime in

64 d during the Western Wildfire Experiment for Cloud chemistry, Aerosol absorption and Nitrogen (WE-CAN

65 ons from the Western Wildfire Experiment for Cloud Chemistry, Aerosol Absorption, and Nitrogen (WE-CA

66 using data from the International Satellite Cloud Climatology Project (ISCCP).

67 lable software for ONT data analytics run on cloud/clusters or personal computers.

68 (69)'s origin appears consistent with pebble cloud collapse followed by a low-velocity merger of its

69 mycin-induced mitochondrial fission, F-actin clouds colocalize with mitochondrial constriction sites,

70 lowing the flank collapse, a deep convective cloud column formed over the volcano and acted as a 'vol

71 introduce NanoSPC, a scalable, portable and cloud compatible pipeline for analyzing Nanopore sequenc

72 the three-dimensional structure of all local cloud complexes.

73 gle computer, in an HPC cluster or on Google Cloud Compute resources.

74 SpaRC can run on both cloud computing and HPC environments without modificatio

75 ent of fast-paced technologies, smartphones, cloud computing and machine learning, with deep mathemat

76 range of 1.5-8.5 mg/dL UA, and convenience, cloud computing and personal information management were

77 ted onto multiple workers based on the Spark cloud computing platform.

78 n access biomedical datasets across multiple cloud computing platforms using best-practice Web securi

79 generalizable to most identity providers and cloud computing platforms.

80 being stored on commercial and institutional cloud computing platforms.

81 ssing biomedical datasets distributed across cloud computing platforms.

82 and analyze data distributed across multiple cloud computing providers without any special knowledge

83 Cumulus combines the power of cloud computing with improvements in algorithm and imple

84 immunosensor and transmit it wirelessly for cloud computing.

85 novations, including anti-clotting measures; cloud-computing for optimized treatment prescribing and

86 accumulation mode particles form most of the cloud condensation nuclei (CCN) that influence the indir

87 perties are sensitive to the availability of cloud condensation nuclei (CCN).

88 urce controlling low-level concentrations of cloud condensation nuclei and ice nucleating particles.

89 provide about half the number of atmospheric cloud condensation nuclei, but in many locations, this p

90 by scattering solar radiation and serving as cloud condensation nuclei.

91 s burning BC to act as an INP in mixed-phase cloud conditions is almost entirely unconstrained.

92 ion for data acquisition, visualization, and cloud connectivity.

93 tion for data acquisition, visualization and cloud connectivity.

94 ifetime, albedo, and radiative properties of clouds containing both supercooled liquid water droplets

95 etween two types of microphysical processes: cloud-core-based invigorating processes vs. peripheral s

96 S VI patients may be falsely high because of clouded corneas and increased corneal rigidity.

97 f spatially extended, quantum-coherent Kondo cloud correlations.

98 Thus, after a certain delay, the two clouds corresponding to different components become well

99 can directly affect cloud cover: It reduces cloud cover by modulating the longwave radiative cooling

100 Driven primarily by increased cloud cover resulting in a dampening of daytime temperat

101 Most ecosystems experience frequent cloud cover resulting in light that is predominantly dif

102 We controlled for cloud cover, snow cover and evaluated the impact of sens

103 degrees C more than night-time temperatures, cloud cover, specific humidity and precipitation decreas

104 ratures and mean daytime and mean night-time cloud cover, specific humidity and precipitation have ch

105 .5 degrees C more than daytime temperatures, cloud cover, specific humidity and precipitation increas

106 ry) we investigated corresponding changes in cloud cover, specific humidity and precipitation.

107 al warming because CO(2) can directly affect cloud cover: It reduces cloud cover by modulating the lo

108 Because stratocumulus clouds cover large swaths of subtropical oceans and cool

109 ping methods to efficiently analyze 3D point cloud data of plant architectures remain challenging for

110 ction of phenotypic properties from 3D point cloud data.

111 ization of particles with minimized atom/ion cloud diffusion.

112 these coordinates, or by analyzing the point cloud directly.

113 by efficient stellar feedback, which drives cloud dispersal on short timescales (around 1.5 million

114 Measurements of polluted clouds downwind of various anthropogenic sources-such as

115 t provides a basis for future development of cloud droplet activation parameterizations that go beyon

116 e models show systematic underpredictions of cloud droplet number concentration across the Southern O

117 vation, potentially substantially increasing cloud droplet number concentration and modifying radiati

118 that the present-day hemispheric contrast in cloud droplet number concentration between the pristine

119 emispheric difference in satellite estimated cloud droplet number concentration implies preindustrial

120 proxy for anthropogenically driven change in cloud droplet number concentration.

121 ion reactions from water-soluble organics in cloud droplets and aerosols create insoluble and soluble

122 e activation of submicrometer particles into cloud droplets in the atmosphere remains a challenge.

123 Aerosol particles become cloud droplets when the ambient relative humidity (satur

124 soot particles sampled after evaporating the cloud droplets, are significantly more compact than fres

125 raction of atmospheric particles that become cloud droplets.

126 ol-induced increases in the concentration of cloud droplets.

127 ify contribution of atmospheric dynamics and cloud effects to radiative imbalance, the satellite-meas

128 Highly portable, cloud-enabled neuroimaging technologies will fundamental

129 e of managing large files, storing them in a cloud environment and extracting subsets of data in an e

130 rs (cloud-ivory), and completed cued-recall (cloud-?; Experiments 1 & 2) and recognition memory tests

131 n hydrodynamic simulations of the Magellanic Clouds falling onto the Milky Way, we can reproduce the

132 Other processes, including the cloud feedback, contribute less to the WPS as their spre

133 g the marine heatwave through a positive low-cloud feedback.

134 on is initiated by the collapse of a cluster-cloud, first forming a nanoparticle.

135 ous processing of biomass-burning phenols in cloud/fog water versus aerosol liquid water.

136 o diverse computing environments, run on the cloud for scalable and cost-effective execution, and are

137 is in canopy species from a tropical montane cloud forest.

138 Focusing on bird communities in tropical cloud forests of the Colombian Andes, we test the perfor

139 properties that are not directly related to cloud formation and are hampered by measurement uncertai

140 The laboratory measurements demonstrate cloud formation in mean-subsaturated conditions (i.e., r

141 strengthening, another one mimicking solute cloud formation, and a third one where dislocation/solut

142 aerosol impacts on human health, visibility, cloud formation, and climate.

143 (INPs) influence global climate by altering cloud formation, lifetime, and precipitation efficiency.

144 metaphor for rapid phase separation based on cloud formation, reasoning that our familiar experiences

145 Clouds forming in relatively polluted trajectories tend

146 While the increase in cloud fraction can be large typically in the beginning o

147 verage lifetime, and higher cloud albedo and cloud fraction compared with unpolluted trajectories.

148 ith the caveat that the aerosol influence on cloud fraction is positive only for stable atmospheric c

149 Warmer ocean conditions then reduce low-cloud fraction, reinforcing the marine heatwave through

150 drop concentration ([Formula: see text]) and cloud fraction, with the caveat that the aerosol influen

151 Ice nucleation and the resulting cloud glaciation are significant atmospheric processes t

152 d by ice-nucleating particles (INPs) enables cloud glaciation at temperatures above the homogeneous f

153 ly modest warming, subtropical stratocumulus clouds gradually thin and may eventually break up into s

154 show that, during the motion, the condensate cloud harvests non-condensed magnons, which results in a

155 The Large Magellanic Cloud has traditionally served as the best galaxy with w

156 the physical relationship between local gas clouds has remained unknown because the accuracy in dist

157 This view is clouded, however, by lingering uncertainty over how to t

158 the nucleation sites for polar stratospheric cloud ice and, after sedimentation into the troposphere,

159 dation chemistry and geostationary satellite cloud imagery data suggests that the lifetime of HPMTF i

160 entation into the troposphere, impact cirrus clouds in the absence of other efficient ice nucleating

161 heterogeneous loss to aerosol and uptake to clouds in the morning and evening.

162 t-of-the-box databases for deployment in the cloud including simple mutant or plasmid collections and

163 e in the amount of water inside liquid-phase clouds induced by aerosols, through the suppression of r

164 ng negative radiative forcing due to aerosol cloud interactions (RF[Formula: see text]) is one of the

165 ervation-based studies underestimate aerosol-cloud interactions because they used measurements of aer

166 Aerosol-cloud interactions constitute the largest source of unce

167 he change in planetary albedo due to aerosol-cloud interactions during the industrial era is the lead

168 ss studies of aerosol production and aerosol-cloud interactions in pristine environments.

169 The variable that controls aerosol-cloud interactions in warm clouds is droplet number conc

170 he radiative forcing since 1850 from aerosol-cloud interactions is constrained to be -1.2 W.m(-2) to

171 for atmospheric aerosol science and aerosol-cloud interactions rely vitally on accurately measuring

172 lenge for large-scale biomedical data on the cloud is providing secure access, especially when datase

173 controls aerosol-cloud interactions in warm clouds is droplet number concentration.

174 he accuracy in distance measurements to such clouds is of the same order as, or larger than, their si

175 C to potential [INP] relevant to mixed-phase clouds is ~5% on a global average.

176 crystallizations, which is named a "cluster-cloud." It is found that nucleation is initiated by the

177 re or after studying a series of word pairs (cloud-ivory), and completed cued-recall (cloud-?; Experi

178 d by vertical convection in the middle/lower cloud layer, and the present result thus introduces new

179 how the super-rotation is maintained in the cloud layer, where the rotation speed is highest.

180 However, the relationship between cloud lifetime and aerosol concentration has been challe

181 This feedback limits cloud lifetimes to about one dynamical timescale (about

182 zed filaments surrounds the Large Magellanic Cloud (LMC) and the Small Magellanic Cloud (SMC), the tw

183 easurements provide a unique opportunity for cloud measurements in the Arctic.

184 omistic simulations suggest that the cluster-cloud-mediated nanocrystallization involves an order-dis

185 ch as Google Cloud, Amazon Elastic Computing Cloud, Microsoft Azure and OpenStack.

186 represented by pharmacophore-annotated point clouds mimicking ideal ligands or fragments.

187 We explain this shift in trend (using a cloud model) as the result of a competition between two

188 our results that the hydrolysis of NO(2) in clouds must be catalyzed by organic or inorganic species

189 sets is often limited as frequent/persistent cloud occurrences reduce their effective temporal resolu

190 stered 26S proteasomes surrounded by a loose cloud of Cdc48.

191 Lead location was tagged on the cloud of HB sites, which was divided into 3 arbitrary se

192 he appropriate number of centrioles inside a cloud of pericentriolar and fibrogranular material.

193 tesimals within a gravitationally collapsing cloud of solid particles.

194 fluctuating selection acts on a microdiverse cloud of strains, and this succession is associated with

195 n immobilized chemokine depot maintaining a 'cloud' of 'solution-phase' chemokines within the glycoca

196 alable architecture by leveraging commercial cloud offerings.

197 Ash-rich particles dominate the volcanic cloud optical properties for the first 60 days.

198 Emerging Linked-Read technologies (aka read cloud or barcoded short-reads) have revived interest in

199 dynamical friction and collisions within the cloud or later gas drag.

200 tures, fundamental uncertainties continue to cloud our view of the future.

201 o the formation and persistence of low-level clouds over [Formula: see text] spatial domains using mu

202 A theoretical mechanism involving electron cloud overlap is proposed to explain all of these result

203 xide (H(2)O(2)) is considered to be the main cloud oxidation pathway.

204 mate; however, BC can also act as a seed for cloud particles, which may offset much of its warming po

205 ) on the ecology of Antarctica and on marine cloud phase, no previous region-wide assessment of bioae

206 files with raw reads uploaded to the ARESdb cloud platform (ares-genetics.cloud; released for resear

207 cient, turn-key, portable pipeline on Google Cloud Platform (GCP) that uses a novel pipeline manager

208 pore data on HPC cluster as well as multiple cloud platforms, such as Google Cloud, Amazon Elastic Co

209 , and that can be deployed on GPU servers or cloud platforms.

210 sentially a miniaturized form of traditional cloud point extraction (CPE) in which only a few microli

211 simple method combining ultrasound assisted cloud point extraction (UA-CPE) and dispersive mu-solid

212 s of endogenous membrane proteins enabled by cloud point extraction and multidimensional liquid chrom

213 The cloud point extraction efficiently enriched membrane pro

214 Our investigations show that cloud point extraction of NPs and their subsequent cryst

215 l as well as environmental water samples via cloud point extraction on a repetitive basis.

216 Cloud point extraction with cold column trapping (CPE-CC

217 lved and nanoparticulate CuO fractions using cloud point extraction.

218 mize parameters such as pH, incubation time, cloud point temperature and surfactant concentration.

219 te saturation concentrations and temperature cloud points in vitro and in cells.

220 ur core phenotyping tasks: classification of cloud points into stem and lamina points, graph skeleton

221 gine for visualizing plants with millions of cloud points, and several graph-theoretic and machine-le

222 ore contribute to brown carbon production in cloud-processed pollution plumes as oxidizing volatile o

223 ance in the Arctic region is sensitive to in-cloud processes, which principally depend on atmospheric

224 of electric charging during the vapor plume cloud processes.

225 id and sulfur-containing organic species via cloud processing is suggested.

226 itted and interstitial soot, confirming that cloud processing, not just exposure to high humidity, co

227 le sizes during the event, indicative of fog/cloud processing.

228 opy and show extensive soot compaction after cloud processing.

229 e, iodine NPF has the potential to influence cloud properties over the Arctic Ocean.

230 We introduce a methodology for ascribing cloud properties to CCN and isolating the aerosol effect

231 s to one in which the fluctuations determine cloud properties.

232 the lower troposphere, where CCN can affect cloud properties.

233 und only when the inter-model differences in cloud radiative effects are considered.

234 This reveals a much greater sensitivity of cloud radiative forcing to CCN than previously reported,

235 fects are one of the leading contributors to cloud radiative properties relevant to climate.

236 Saturn's moon Titan has a methane cycle with clouds, rain, rivers, lakes, and seas; it is the only wo

237 te analyses reveal that the convective anvil cloud, reaching 16-18 km above sea level, was ice-rich a

238 Fog and cloud readily form under winter haze conditions, leading

239 Point cloud registration is used to find the transformation en

240 to the ARESdb cloud platform (ares-genetics.cloud; released for research use in 2020).

241 endence of the reactions was investigated at cloud relevant pH of 3-6, and the results reveal their i

242 clouds, which could be expected if the local cloud represented an isolated remnant of the most recent

243 Measurements of cloud residuals suggest that particles smaller than 30 n

244 tive results, we conducted three-dimensional cloud-resolving simulations to investigate the underlyin

245 nts and Jupyter Notebooks that can be run on cloud resources such as Google Colaboratory.

246 This is because cloud-scale computing resources, from robust backup to h

247 of precipitation unambiguously attributed to cloud seeding are isolated from natural precipitation (<

248 n seven decades ago in Vonnegut's pioneering cloud seeding experiments, it remains unclear what makes

249 For over half a century, cloud seeding has been evaluated as a technology to incr

250 represent a critical step toward quantifying cloud seeding impact.

251 lly based approach to quantify snowfall from cloud seeding in mountain cloud systems is presented.

252 oral evolution of precipitation generated by cloud seeding is then quantified using radar observation

253 ution of snowfall generated from glaciogenic cloud seeding of winter mountain cloud systems and its s

254 .05 and 0.3 mm as precipitation generated by cloud seeding passed over the instruments.

255 The total amount of water generated by cloud seeding ranged from 1.2 x 10(5) m(3) (100 ac ft) f

256 m 1.2 x 10(5) m(3) (100 ac ft) for 20 min of cloud seeding, 2.4 x 10(5) m(3) (196 ac ft) for 86 min o

257 regional weather modification methods, like cloud seeding, are being used to counteract increasing w

258 o 3.4 x 10(5) m(3) (275 ac ft) for 24 min of cloud seeding.

259 application and utility of metagenomic read cloud sequencing and assembly to study the underlying st

260 securely stored and analysed in an encrypted cloud server.

261 n either a local computer or a remote server/cloud service.

262 e wirelessly transmitted to a smart-phone or cloud sever through the Wi-Fi connection for visualizing

263 ellanic Cloud (LMC) and the Small Magellanic Cloud (SMC), the two most massive satellite galaxies of

264 corded RGC responses to a correlated noise ("cloud") stimulus in an in vitro preparation of mouse ret

265 t fluorescence images, and store the data in cloud storage via a WiFi network.

266 MAESTRO can gather data using cloud storge for further research and in-depth analysis.

267 vealed the importance of the divalent cation cloud surrounding exposed phosphates on the DNA.

268 glaciogenic cloud seeding of winter mountain cloud systems and its spatial and temporal evolution.

269 tify snowfall from cloud seeding in mountain cloud systems is presented.

270 ly in the web browser through modern web and cloud technologies as an open source extendable web app.

271 geometrical distance to the Large Magellanic Cloud that is precise to 1 per cent based on 20 eclipsin

272 pre-galactic haloes and their associated gas clouds that are exposed to a Lyman-Werner intensity roug

273 this region's marine boundary layer and the clouds that overtop it is that it is truly pristine, fre

274 c strategies occur across vertebrate groups, clouding the homology between their developmental progra

275 he input precursors and the output products, clouding the pathway toward Fe-N-C catalyst improvement.

276 low resolution, and their consensus quality clouds the accurate annotation of complete, partial, and

277 d that on a global scale when accounting for cloud, the worst time of year for an earthquake disaster

278 olar neighbourhood that contains many of the clouds thought to be associated with the Gould Belt.

279 ltiple out-and-in relaxations of the cluster-cloud to improve crystallinity: from a poorly crystalliz

280 analysis framework that assigns localization clouds to individual molecules, thus eliminating a sourc

281 use idealized high-resolution simulations of clouds to show that, even under a sustained solar geoeng

282 All 18 cloud-to-ground flashes were negative polarity, supporti

283 e leaders(11,16,17,20-22) and cause multiple cloud-to-ground lightning events(1).

284 Any changes in cloud-to-ground lightning frequency due to climatic chan

285 positive leaders(22), or why the current in cloud-to-ground lightning never goes to zero(23).

286 occurrences over five hours (57 in cloud, 18 cloud-to-ground).

287 which maintains the rotation peak, near the cloud top at low latitudes.

288 Cloud-top temperatures hovered around -80 degrees C and

289 material is associated with atomic hydrogen clouds travelling in the nuclear wind(8).

290 f great importance for the simplification of cloud water chemistry models.

291 We estimate that the observed decrease in cloud water offsets 23% of the global climate-cooling ef

292 small OAs (e.g., FA) are highly sensitive to cloud water pH.

293 decreases, caused by enhanced evaporation of cloud water, partially cancel each other out.

294 dfires and ships-reveal that aerosol-induced cloud-water increases, caused by suppressed rain formati

295 Read clouds were found to improve the completeness and contig

296 he evolution of low-temperature interstellar clouds, where the quantum tunnelling effect becomes sign

297 g Earth's passage through local interstellar clouds, which could be expected if the local cloud repre

298 passage of our SS through such interstellar clouds, which have a significantly larger particle densi

299 g coincided with the rapid growth of the ash cloud, while the second maxima occurred near the time of

300 isional modeling of a recently produced dust cloud yields results consistent with the observations.