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1 e 1 ("dust"), type 2 ("sphere"), or type 3 ("cloud").
2 urrounded by his/her own signature microbial cloud.
3 ee-dimensional distribution of the screening cloud.
4 n sites ranging from lab workstations to the cloud.
5 s-a-Service supported by a dedicated compute cloud.
6 d is warmer than that in relatively pristine cloud.
7 y climate models, changing the properties of clouds.
8 rough the expansion of noninteracting atomic clouds.
9 hey showed large discrepancies in dust-mixed clouds.
10 ng a cluster whose nodes come from different clouds.
11 conditions to the temperatures that occur in clouds.
12 her by acting as ice nucleating particles in clouds.
13 across different areas by including density clouds.
14 , and in polar stratospheric and noctilucent clouds.
15 classified into 3 groups: dust, spheres, and clouds.
16 tion of iron remains largely unknown in warm clouds.
17 in the center-of-mass positions of outgoing clouds.
18 ng, and widespread condensational heating in clouds.
19 minergic drug selectivity and design remains clouded.
20 iated with a decrease in marine tropical low cloud (a more positive shortwave cloud feedback) and wit
22 ion (CALIOP) instrument on the polar orbiter Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Ob
26 ent improvements in IRD including the use of cloud and high performance computing resources, analysis
30 ough which anions might form in interstellar clouds and circumstellar envelopes, including the import
35 termittency in solar intensity-step changes (clouds and shadows) and ramp changes (sunrise), respecti
36 erived surface irradiance data from the NASA Clouds and the Earth's Radiant Energy System (CERES) wit
37 tostar is formed in the dense, turbulent gas cloud, and it grows by sporadic mass accretion until it
38 rable to explosions, radiant heat, toxic gas clouds, and air pollution from hydraulic fracturing acti
43 Atmospheric aerosols and their effect on clouds are thought to be important for anthropogenic rad
44 uring the overall atomic loss from colliding clouds as a function of magnetic field, we track the ene
45 rature appear to affect the expansion of the cloud, as if the system has turned into a diffusive coll
46 r package supports Amazon, Google, and Azure clouds, as well as, any other cloud platform based on Op
47 ter activity, viscosity, titratable acidity, cloud assessment and turbidity), antioxidant compounds a
49 ybrid computing infrastructure consisting of cloud AWS, supercomputers and local high performance com
50 ct sites, the formation of interstellar dust clouds, ballistic penetrators, spacecraft shielding and
51 vascular epiphyte communities bracketing the cloud base during a severe, El Nino-impacted dry season.
52 a privacy preserving read mapper for hybrid clouds based on locality sensitive hashing and kmer voti
54 We present interactive analytics using a cloud-based columnar database built on Dremel to perform
57 the cartridge and the patient to populate a cloud-based database for epidemiological reporting of te
58 aphic angiography on arrival to the PSC, and cloud-based image sharing is associated with a reduction
59 cal severity, vessel imaging at the PSC, and cloud-based image sharing) with the efficiency of care a
63 taneous transfer of patient information to a cloud-based server, with the capacity for instant alerts
65 ext-generation sEquencing data (GeMSTONE), a cloud-based variant prioritization tool with high-level
67 the nucleosynthetic makeup of the molecular cloud before the last addition of stellar-derived (26)Al
70 particularly through their interactions with clouds, but the magnitude of this effect is highly uncer
71 ment with satellite observations in pristine clouds, but they showed large discrepancies in dust-mixe
72 but interpretations of these experiments are clouded by the multiple functions of these proteins.
75 al approaches for big data, the denser point clouds can efficiently be processed to ultimately allow
79 ng of aerosols, including wet scavenging and cloud chemistry, could also have substantial effects on
80 w the observations of anions in interstellar clouds, circumstellar envelopes, Titan, and cometary com
83 ergy balance, improved prediction of aerosol-cloud-climate interactions is likely to result in improv
84 edge of a slowly drifting complex convective cloud close to the highest regions at 17 km altitude.
85 aturalistic textures called "compound motion clouds" (CMCs) [15, 16] that simultaneously activate mul
86 x and large simulations on supercomputers or Cloud computers, QwikMD uses the same steps and user int
87 on the use of the recent development in the cloud computing market, which have witnessed more provid
88 move of computational genomics workflows to Cloud Computing platforms is associated with a new level
89 equencing technologies embedded in automated cloud-computing analysis environments are ideally suited
95 m open water and open pack ice increased the cloud condensation nuclei concentration background by at
98 the source of over half of the atmosphere's cloud condensation nuclei, thus influencing cloud proper
99 he latter influences their ability to act as cloud condensation nuclei, whereby they impact cloud cov
100 nd microfluidics, along with developments in cloud-connected point-of-care (POC) diagnostics technolo
101 cold air drainage proceeds more readily when cloud cover and humidity are low, resulting in the great
102 tent yet at sufficiently fine spatial grain, cloud cover dynamics may provide key information for del
103 satellite images that expose spatiotemporal cloud cover dynamics of previously undocumented global c
105 ervational evidence for a strong increase in cloud cover over large forest regions in western Europe
106 t Phase 5 (CMIP5) also exhibit a decrease in cloud cover over the Mediterranean since the 1970 s, in
107 eement between the interannual variations of cloud cover provided by surface observations and several
108 Here we report a widespread decrease in cloud cover since the 1970 s over the Mediterranean regi
109 toring campaign of brown dwarfs to constrain cloud cover variations over a total of 192 rotations.
110 as caused primarily by a decrease in daytime cloud cover with a resulting increase in received solar
114 SVs) for SV detection and assembly from read cloud data and apply this method to Illumina-sequenced 1
120 ties in China substantially increases column cloud droplet number concentration and liquid water path
122 face microlayer or as surfactant coatings on cloud droplets are highly concentrated and chemically di
123 pical freshwater environments and in neutral cloud droplets but are likely to aggregate under salty (
124 owth of cloud condensation nuclei (CCN) into cloud droplets under supersaturated water vapour conditi
125 ion varies dramatically over the pH range of cloud droplets with pH = 5.5 solutions absorbing three t
126 luhraun, Iceland, reduced the size of liquid cloud droplets-consistent with expectations-but had no d
133 ethylammonium sulfate seeds was triggered by cloud events with chamber lights on, suggesting photosen
134 These model errors are likely connected to cloud feedback in climate projections, and highlight the
135 ropical low cloud (a more positive shortwave cloud feedback) and with a less negative lapse-rate feed
137 oms of the superposed templates form a point cloud for each position of a target protein, which are r
138 vived this intense drought, epiphytes in the cloud forest experienced the slowest recovery, suggestin
140 Epiphytes are common in tropical montane cloud forests (TMCFs) and play many important ecological
143 ptimal" climatic conditions found in montane cloud forests is similar to that of maritime temperate a
144 nditions, and should affect the modelling of cloud formation and ice particle numbers, which are very
146 e roles of ecosystem Hs and LE on convective cloud formation are explored relative to the entrainment
147 are below 0.1 m s(-1) and about one in 10(4) cloud formation events occur in environments with sigma
148 g., we see a human face when staring up at a cloud formation or down at a piece of toast at the break
149 ate with reanalysis products and an advanced cloud formation scheme results in lower homogeneous ice
150 eft over from the Big Bang prevent early gas cloud formation until rapid gas condensation is triggere
151 lts highlight the need to include impacts on cloud formation when evaluating the water and climate se
152 er insight into the influence of aerosols on cloud formation, and be used as input for the improved m
153 the potential importance of playa dusts for cloud formation, most climate models assume that all dus
154 ur understanding of processes such as cirrus cloud formation, where such topographical features are l
155 lead to a climatic cooling by increasing low cloud formation, which enhances albedo (umbrella effect)
158 ion coupled with a decrease in tropical high cloud fraction is key in modulating precipitation respon
161 al, fine-grain ( approximately 1 km) monthly cloud frequencies from 15 y of twice-daily Moderate Reso
162 seleniranium ion, antiattack of the electron cloud from the aromatic ring at the activated triple bon
164 ent a new package called MC-GenomeKey (Multi-Cloud GenomeKey) that efficiently executes the variant a
166 network, optical network and processing unit cloud have been decoupled from each other, so that their
170 and montane forests, which may be caused by cloud immersion effects within the cloud forest zone.
171 on process is essential to the prediction of clouds in climate models, and given the effect of clouds
173 rees C), conditions necessary to form cirrus clouds in the Earth's atmosphere, routinely observed in
175 ed the efficacy of these pipelines on Amazon cloud instances through the Seven Bridges Genomics imple
178 The magnitude of air-traffic-related aerosol-cloud interactions and the ways in which these interacti
179 general circulation models represent aerosol-cloud interactions at ever-increasing levels of detail,
185 m interferometry, the condition to split the cloud into mainly two equally-populated fragments is onl
186 ational collapse of a massive primordial gas cloud is a promising initial process, but theoretical st
187 given ice water path, the CTT of dust-mixed cloud is warmer than that in relatively pristine cloud.
188 , the upper bound on tropospheric mixing and clouds is constrained by the rapid decrease with height
190 vitreous seed classification (dust, spheres, cloud) is predictive of the total number and dose of IVM
192 ue to the thinness and small scale of cirrus clouds, its lateral boundary may be missed by convention
196 nks ZapB to the chromosomal terminus region, cloud-like ZapA structures still formed but failed to tr
200 r thermally unprocessed primordial molecular cloud material before its pollution by stellar-derived (
204 hat observational findings from the Barbados Cloud Observatory are relevant to clouds across the trop
205 based on a Voronoi partitioning of the point cloud of coarse-grained particles, and is continuously u
206 .6 billion years ago, some event disturbed a cloud of gas and dust, triggering the gravitational coll
207 pathological condition characterized by the clouding of the normally clear eye lens brought about by
208 amyloid deposits within the brain cluster as clouds of conformational variants in different AD cases.
209 ear-global coverage, even in the presence of clouds, of proxies for soil moisture derived from the am
211 s in climate models, and given the effect of clouds on the Earth's energy balance, improved predictio
212 ostatic repulsion between localized electron clouds on Tl and Te ions, are akin to those of rattling
214 AT can be run on a public web portal, in the cloud, or downloaded for local use, and is easily integr
215 omics variant discovery and annotation using cloud- or local high-performance computing infrastructur
216 We reconstructed and quantified the bouton clouds originating from adjacent L5B columns in the BC i
217 he vast majority of proviruses are defective clouds our assessment of the degree to which clonally ex
219 sults show that measurement of personal data clouds over time can improve our understanding of health
220 estimates are directly linked to a weakened cloud-phase feedback arising from a decreased cloud glac
222 rmation, creating a database accessible on a cloud platform and through a controlled-access internet
224 CWL and on the Seven Bridges Cancer Genomics Cloud platform can be obtained by contacting the authors
225 ne is open source and easily deployable to a cloud platform, local cluster, or desktop, making it a s
227 Amazon in combination with the use of other cloud platforms to provide significant cost reduction.
228 The package can run in different commercial cloud platforms, which enables the user to seize the bes
231 rate polymers in which the degradability and cloud point can be independently tuned to create materia
235 based on the preconcentration of arsenic by cloud point extraction (CPE) using o,o-diethyldithiophos
236 rganic drop (VA-DLLME-SFO) and salt-assisted cloud point extraction (SA-CPE) for paraben extraction.
239 ropagates to the Earth as a typical magnetic cloud possessing a similar twist profile obtained by the
241 ium sulfate were determined before and after cloud processing in a temperature- and RH-controlled cha
243 boundary layer, and may therefore influence cloud properties and climate under natural conditions.
251 servations from passive spectrometer, active cloud radar, lidar, and wind field simulations from CRM
252 e, the combination of millimetre-wavelength 'cloud radars' and Doppler lidar now provides virtually i
256 trategies for improving estimates of aerosol-cloud relationships in climate models, for new remote se
259 for detecting and annotating mutations using cloud resources from different commercial cloud provider
263 ance is deployed through iPlant's Atmosphere cloud services, users access the xGDBvm workflow via a u
264 ibution function (PDF) of CTT for dust-mixed clouds shifted to the warmer end and showed two peaks at
268 lted in a juice with improved uniformity and cloud stability by reducing particle size and increasing
269 data stored either locally or retrieved from cloud storage services, and runs on both desktop compute
270 indicating that these indirect effects, and cloud systems in general, are well buffered against aero
273 le biodetectors to map out the anaphylatoxic cloud that surrounds microbes in the presence of host se
274 ntribute to the formation of contrail cirrus clouds that can alter upper tropospheric radiation and w
275 thermal instabilities produce a rain of cold clouds that fall towards the galaxy's centre, sustaining
276 e link through sea ice melt and low altitude clouds that may have contributed to accelerate Arctic wa
278 inement and depending on the velocity of the cloud, three main regimes are observed corresponding (1)
279 significantly mediate the properties of ice cloud through heterogeneous nucleation and lead to cruci
281 partition to aerosol liquid water (ALW) and clouds to form aqueous secondary organic aerosol (aqSOA)
285 elts, passed about 4000 kilometers above the cloud tops at closest approach, well inside the jovian r
286 ts are electric discharges from thunderstorm cloud tops to the bottom of ionosphere at 90 km altitud
289 interest can be immediately analyzed in the cloud using more than 200 preinstalled, curated bioinfor
290 ease: Patients with eyes containing class 3 (cloud) vitreous seeds were significantly older than pati
293 cs implementation of the NCI Cancer Genomics Cloud, which provides graphical interfaces for running a
294 al fraction of the computation to the public cloud, while being highly competitive in accuracy and sp
295 vancements of LiDAR sensor technology, point clouds will affordably reach this required density.
296 Jets may bend when initiated at the edge of clouds with misaligned vertical charge distribution.
298 less like billiard balls and more like dust clouds, with apparent coherence only due to similar init
299 sets to shift part of their analysis to the cloud without sacrificing accuracy or exposing sensitive
300 can modify the thickness and coverage of low clouds, yielding significant radiative forcing of climat
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