ライフサイエンスコーパス: radar

1 of analysis: assembly stock and interaction radar.

2 arasitemias below clinical and immunological radar.

3 mall enough to fly under the immune system's radar.

4 y drifting buoys, gliders and high-frequency radar.

5 y layer using vertical-looking entomological radars.

6 We used insect-monitoring radars [12] to show that up to 4 billion hoverflies (80

7 rometers, global positioning system, forward radar, 4-channel video).

8 We develop RADAR, a comprehensive analytical tool for detecting dif

9 Here we present CNV Radar, a software tool that utilizes next-generation seq

10 rtfolio of ENCODE-RBP experiments to develop RADAR, a variant-scoring framework.

11 We present RADAR--a rigorously annotated database of A-to-I RNA edi

12 es enabled flexible and conformable wideband radar absorber.

13 an provide flexible and conformable wideband radar absorption, which extends the graphene's applicati

14 dimethyl labeling coupled with LC-MS/MS and RADAR algorithm was developed to identify the disulfide

15 RadAR allows users to process radiomic datasets in their

16 RADAR also includes an expandable listing of tissue-spec

17 We combined new radar altimeter measurements from satellites CryoSat-2 a

18 Using 18 years of continuous satellite radar altimeter observations, we have computed decadal-s

19 Radar altimetry also reveals time-varying subsidence in

20 Contemporary applications of radar altimetry include sea-level rise, ocean circulatio

21 Here we use multi-mission radar altimetry with an approximately 23 year data-span

22 and abundance can be addressed using weather radar analyses.

23 airborne ice-penetrating radar, but existing radar analysis approaches cannot discriminate between th

24 York, quantifying behavioral responses with radar and acoustic sensors and modeling disorientation a

25 detection, opening up new possibilities for radar and communication systems, and for the field of pr

26 Applications of this system for discrete radar and digital communication theory are explained.

27 We examine the unique radar and environmental conditions leading to the format

28 nalysis of the drop properties inferred from radar and in situ aircraft measurements obtained in two

29 We used a combination of meteorological radar and lidar instrumentation at a site in Oklahoma, U

30 blished applications in astronomy, medicine, radar and metrology.

31 range of subjects, including communications, radar and metrology.

32 large-scale collection of synthetic-aperture radar and multispectral images has been implemented in G

33 sted a combination of multidate, multisensor radar and optical imagery (Landsat TM/PALSAR/RADARSAT-1/

34 Radar and optical observations reveal that the continuou

35 e wider applications in intelligent sensing, radar and quantum optics.

36 ciprocal microwave devices are ubiquitous in radar and radio communication and indispensable in the r

37 Here using long-term satellite, surface radar and rain-gauge network data and atmospheric reanal

38 e Doppler effect in wireless communications, radar and satellite navigation.

39 Radar and satellite observations reveal that strong conv

40 Radar and seismic imaging combined with in situ borehole

41 d departure of migratory birds using weather radar and simulated their migration trajectories using a

42 coarse root biomass using ground-penetrating radar and total root biomass using soil cores.

43 ata from disparate sensor platforms, such as radar and video, to synthesize information that is more

44 We combine data from entomological radars and ground-based light traps to show that annual

45 tween urban and non-urban areas varied among radars and seasons, but was consistently higher over urb

46 combination of millimetre-wavelength 'cloud radars' and Doppler lidar now provides virtually ideal i

47 scopes, magnetic resonance imaging scanners, radar, and a host of other techniques.

48 s, mapped using LiDAR and ground penetrating radar, and compare these rates to those inferred from ge

49 blebee foragers continuously, using harmonic radar, and examined the process of route formation in de

50 or laser surgery, material processing, laser radar, and free-space communications, and other areas.

51 s Littrow cavities and lasers, spectroscopy, radar, and frequency scanned antenna reflectors.

52 ocaloric coolers for computers, phased-array radar, and three-dimensional trenched capacitors for dyn

53 rmation of the plane-wave projections on the radar aperture is retrieved, resulting in high-fidelity

54 ncode the plane-wave signals incident on the radar aperture using a single antenna.

55 channel through the transfer function of the radar aperture.

56 ased antenna array developed in the field of radar applications is a promising approach for increased

57 ini imaging subsystem and synthetic aperture radar are uncorrelated with topography and elevation.

58 ximately 100 km is promising, but additional radars are needed to parameterise spatial covariance.

59 justed for duration of antibiotic risk (DOOR/RADAR) are novel and innovative methods of evaluating da

60 These results demonstrate RadAR as a reliable and valuable tool for the radiomics

61 The ELISA-based RADAR assay can detect Top1-DNA and Top2a-DNA adducts in

62 This method is based on the RADAR assay for DNA adducts that we previously developed

63 We apply the RADAR assay to demonstrate that expression of SLFN11 doe

64 The RADAR assay will be useful for analysis of the mechanism

65 the spatial distribution of regions of high radar backscatter is well matched by the predicted distr

66 are spatially collocated with areas of high radar backscatter postulated to be the result of near-su

67 d understory cover) simultaneously influence radar backscatter.

68 We develop a new radar-based approach to estimate time-varying elevations

69 l state than traditional stationary gages or radar-based measurements.

70 Radar-based research now encompasses foraging as well as

71 h a canted angle similar to that employed in radar bearing locators.

72 We use the angular distribution of energy in radar bed echoes to characterize both the extent and hyd

73 the ice sheet measured from ice-penetrating radar between the two ice core sites.

74 sect species, and will help drive a shift in radar biology from a largely qualitative and phenomenolo

75 re coupled via a planar microstrip-line to a radar board operating in the ISM band 2.4-2.5 GHz.

76 The neutron data indicate that Mercury's radar-bright polar deposits contain, on average, a hydro

77 applications ranging from communications to radar, broadcasting and astronomy.

78 se water systems is airborne ice-penetrating radar, but existing radar analysis approaches cannot dis

79 lar results were observed when comparing CNV Radar calls to single nucleotide polymorphism array resu

80 Our results demonstrate RADAR can successfully pinpoint variants, both somatic a

81 computational time to model and predict the radar characteristics of such large objects.

82 An innovative radar chart analysis method was developed to depict subc

83 Results were visualized in radar charts to assess toxicological response patterns a

84 uman computational phantoms developed by the RADAR committee of the Society of Nuclear Medicine and M

85 The radar cross section (RCS) of the cylinder with and witho

86 electromagnetic wave reflection or backward radar cross section (RCS).

87 000, and using near infrared wavelength, the radar cross section can be determined in a tabletop setu

88 The radar cross section of an object is an important electro

89 lties, and make accurate measurements of the radar cross section of large items.

90 applications of radar often assume that the radar cross sections of flying animals are isotropic, si

91 lometers by 200 kilometers) of near-parallel radar-dark linear features that appear to be seas of lon

92 The radar-dark patches are interpreted as lakes on the basis

93 rth shows more than 75 circular to irregular radar-dark patches, in a region where liquid methane and

94 ations with 21 years of weather surveillance radar data (1995-2015).

95 nalysis applied to ALOS-1 synthetic aperture radar data acquired during 2007-2011 to generate high-sp

96 satellite interferometric synthetic-aperture radar data acquired during the International Polar Year

97 Combined neutron and radar data are best matched if the buried layer consists

98 Moreover, we show that radar data can be used to determine the timing and depar

99 alysis of viscous buckles in ice-penetrating radar data can quantify the seawater content of suture z

100 Here, we demonstrate how analog radar data collected over 40 y ago in Antarctica can be

101 re, we present evidence from ice-penetrating radar data for a 750-km-long subglacial canyon in northe

102 ence from interferometric synthetic aperture radar data for secular inflation of a dike-like magma bo

103 we analyse entomological and ornithological radar data from north-western Europe to investigate how

104 Here we use ice-penetrating radar data from Roi Baudouin Ice Shelf, East Antarctica,

105 en suggested as an explanation for anomalous radar data on Europa, but until now no penitentes have b

106 000 line kilometers of exploratory Antarctic radar data originally recorded on 35-mm optical film bet

107 Here we demonstrate that archival weather radar data over a period of ten years can be used to mon

108 d GPS and interferometric synthetic aperture radar data to model the earthquake rupture as a slip pul

109 Using weather radar data, a unique 23-year (1995-2017) long time serie

110 of Doppler polarimetric weather surveillance radar data, we examined two impediments for nocturnally

111 bbahu rifting episode derived from satellite radar data, which shows that the entire segment ruptured

112 More importantly, CNV Radar demonstrated its utility in the clinical trial set

113 Interferometric synthetic aperture radar-derived measurements of ice surface motion acquire

114 Two novel radar designs introduced in the late 1990s have signific

115 s are too fine (radii < 30 mum) for on-board radar detection and, even in good visibility, ash clouds

116 for the YORP acceleration of a body with the radar-determined size, shape, and spin state of 2000 PH5

117 emporal analyses based on Synthetic Aperture Radar differential interferometry (DInSAR) to study the

118 This is also demonstrated in the radar-driven prototype where the raw data collected at t

119 d system is a developmental platform towards radar-driven wearable continuous BGL monitors.

120 ized by less intense convection with intense radar echoes not extending to extremely high altitudes.

121 RADAR enables accurate identification of altered methyla

122 ascinated humankind, and since the advent of radar entomology much has been revealed about high-altit

123 We show that radar estimates of colony size closely match those deriv

124 Overall, CNV Radar exhibited high concordance with standard methods s

125 f approximately 260 kg of PCBs by a military radar facility over a 30 year period (1970-2000) contami

126 Observations from C-band weather radar, fall deposits and numerical modelling demonstrate

127 urface of Titan, obtained during the Cassini Radar flyby of Titan on 22 July 2006 (T16).

128 The Mars Advanced Radar for Subsurface and Ionospheric Sounding (MARSIS) i

129 s of Mars were probed with the Mars Advanced Radar for Subsurface and Ionospheric Sounding on the Mar

130 and basal topography from the Mars Advanced Radar for Subsurface and Ionospheric Sounding on the Mar

131 The radar forward-scattering properties of different reflect

132 und-Based Interferometric Synthetic Aperture Radar (GBInSAR) is an efficient technique for capturing

133 red that the diffusible TGFss-related factor Radar (Gdf6a) is necessary and sufficient for activation

134 tion with interferometric synthetic aperture radar, Global Positioning System, and seismology data, r

135 Ground Penetrating Radar (GPR) 110-900 MHz surveys showed the wrapped buria

136 graphy, thin sections and ground penetrating radar (GPR) acquisitions.

137 on data collected by the ground-penetrating radar (GPR) onboard the Yutu-2 rover during the initial

138 tion and ranging (LiDAR), ground penetrating radar (GPR), and archaeological surveys, has led to the

139 ng of such footprints via ground-penetrating radar (GPR), including co-associated mammoth and human p

140 mechanisms for the Gamburtsevs, derived from radar, gravity and magnetic data.

141 Flooding detected with synthetic aperture radar (>91% accuracy) extended beyond state-mapped hazar

142 Radar has been used to study insects in flight for over

143 s visible (or invisible) to a human eye or a radar has captured people's imagination for centuries, c

144 ces on forest structure may allow the use of radar imagery for forest biomass estimates beyond common

145 Using satellite-based radar imagery for such purposes has been challenged by t

146 ived from the amplitude and phase content of radar imagery.

147 (GPS), interferometric analysis of satellite radar images (InSAR), and graben formation.

148 series optical images (Landsat-8, MODIS) and radar images (PALSAR) in mapping paddy rice planting are

149 to 3 cm/y as measured using satellite-based radar images from 2007 to 2010 and consistent with trans

150 pped from high-resolution ground penetrating radar images of the subsurface and transformed into sea-

151 The most recent Cassini RADAR images of Titan show widespread regions (up to 150

152 e surface (about 2 m deep) has been found by radar images only poleward of 50 degrees latitude, while

153 Further west, space-born radar images reveal networks of-now buried-fossil river

154 terferometric analysis of synthetic aperture radar images to measure postseismic surface deformation

155 Doppler weather radar imaging enabled the rapid recovery of the Sutter's

156 Initial visible and radar imaging failed to find any evidence of an ocean, a

157 of cellular activity, and tomographic, nano-radar imaging of the morphology of vital organelles in t

158 The radar imaging polewards of 70 degrees north shows more t

159 We validate this approach with radar imaging, showing that substantial water volumes ar

160 Evaluation of CNV Radar in a public multiple myeloma dataset demonstrated

161 hat thousands of plasmids remained below the radar in already completed genomic and metagenomic studi

162 We used data from nine weather surveillance radars in the eastern United States to estimate altitude

163 RADAR includes a comprehensive collection of A-to-I RNA

164 ise using interferometric synthetic aperture radar (InSAR) analysis applied to ALOS-1 synthetic apert

165 ace-based interferometric synthetic aperture radar (InSAR) observations provide near-global coverage,

166 satellite interferometric synthetic aperture radar (InSAR) surface deformation and satellite thermal

167 Using Interferometric Synthetic Aperture Radar (InSAR) to observe ground deformation in the Ken R

168 ned using interferometric synthetic aperture radar (InSAR), we find the onset of rapid flow (moving a

169 [GPS and interferometric synthetic aperture radar (InSAR)] show broad ( approximately 100 km) aseism

170 n eastern Texas causes uplift, detectable in radar interferometric data up to >8 kilometers from the

171 Here we use radar interferometry (InSAR) and a simple 1D hydrologica

172 We use satellite radar interferometry and GPS data to show that between 2

173 We produced elevation models using radar interferometry applied to bistatic data gathered b

174 gation Satellite System (GNSS) and satellite radar interferometry from two decades of observations.

175 ata related to the Chaiten eruption based on radar interferometry observations from the Japan Aerospa

176 With radar interferometry, the next-generation Surface Water

177 Radar investigations measure these layers and provide ev

178 RADAR is a web server that provides a multitude of funct

179 on screening and molecular weight match, new RADAR is capable of confirming the matched peptide pairs

180 Our case studies also showed that CNV Radar is capable of detecting abnormalities such as copy

181 We demonstrated that CNV Radar is more sensitive than other CNV detection methods

182 We conclude that Radar is near the top of a signaling cascade that establ

183 se adjusted for duration of antibiotic risk (RADAR) is a novel methodology utilizing a superiority de

184 ening of a(1) ions with customized software, RADAR, is developed.

185 ions from passive spectrometer, active cloud radar, lidar, and wind field simulations from CRM to ide

186 , measurements in the middle atmosphere - by radar, lidar, high-flying aircraft and satellite remote

187 hnique allows the user to choose the optimal radar location for measuring the most significant deform

188 We use a suite of ice-penetrating radar, magnetic and gravity measurements to propose a ri

189 n effective dose was 0.0055 mSv/MBq with the RADAR manual method and 0.0052 mSv/MBq with OLINDA/EXM.

190 However, previous orbital and Earth-based radar mapping and orbital optical imaging have yielded c

191 ace-based interferometric synthetic aperture radar measurements from the Italian constellation COSMO-

192 compare the digitized data with contemporary radar measurements to reveal that the remnant eastern ic

193 bine borehole optical televiewer logging and radar measurements with remote sensing and firn modellin

194 ystem and interferometric synthetic aperture radar measurements, at rates up to 7 centimeters per yea

195 flights, indicating that the behavior of our radar-monitored bees was not due to the attachment of tr

196 Radar-monitored flights were not continuously directed a

197 Radar mutant axons innervate only the dorsal half of the

198 transferred to the electronic domain, where radar, navigation, communications, and fundamental resea

199 A continent-wide weather radar network also reveals a similarly steep decline in

200 on InSAR (Interferometric Synthetic Aperture Radar) observation and the heat transfer model of soils.

201 n 11-year record of spaceborne precipitation radar observations and establish that a relatively small

202 Here we use firn cores, radar observations and regional climate models to show t

203 ed by cloud seeding is then quantified using radar observations and snow gauge measurements.

204 e bat agree with controlled measurements and radar observations made during a field study of bats in

205 awn spacecraft has provided orbital bistatic radar observations of a small body in the solar system.

206 We present orbital bistatic radar observations of a small-body, acquired during occu

207 The weather radar observations of approximately 2,000 storms, on ave

208 Finally, we show that radar observations of flying-foxes can be used to identi

209 We analyzed radar observations of mayfly emergence flights to quanti

210 Cassini radar observations of Saturn's moon Titan over several y

211 Using seismic and radar observations on the Larsen C Ice Shelf of the Anta

212 Satellite radar observations revealed hundreds of previously unmap

213 pheric environment modeling and ground-based radar observations.

214 blished in the same coordinate system as the radar observations; (iii) the high resolution temperatur

215 ular properties of proteins that fall on the radar of protein quality control (PQC)?

216 ed from animal to animal, slipping under the radar of the immune system.

217 olution maps, acquired using ice-penetrating radar, of the bed topography across parts of PIG.

218 s an alternative, biological applications of radar often assume that the radar cross sections of flyi

219 Recently, ground-penetrating radar on Phra Thong Island identified a region that coul

220 in the eastern Hellas region by the Shallow Radar on the Mars Reconnaissance Orbiter reveal radar pr

221 pulse-echo ambiguity, a serious problem for radar or sonar.

222 can also be extended to optical microscopy, radar, or seismic imaging.

223 Moreover, Radar overexpression "dorsalizes" retinal ganglion cell

224 ALOS) Phased Array L-band Synthetic Aperture Radar (PALSAR) mosaic dataset and the phenological infor

225 lysine 19 (K19R), the target residue of the RADAR pathway within Pex20p, leads to a stable but non-f

226 ried out based on elemental composition by a radar plot and multivariate data analysis, including pri

227 Radar plot of the electronic nose analysis showed that t

228 differentiated from foreign rice samples by radar plots and multivariate data analysis.

229 modelling of Bennu's thermal inertia(12) and radar polarization ratios(13)-which indicated a generall

230 A new Doppler radar, previously used to track small debris particles s

231 ar on the Mars Reconnaissance Orbiter reveal radar properties entirely consistent with massive water

232 In addition, RADAR provides two salient features: (i) constrained ali

233 cape, based on new data from ice-penetrating radar, provides an improved understanding of the topogra

234 iversion and Addiction-Related Surveillance (RADARS(R)) System in 2006 and 2007.

235 dosimetry estimates were performed using the RADAR (RAdiation Dose Assessment Resource) method for in

236 Here we present RadAR (Radiomics Analysis with R), a new software to per

237 ates improved rainfall estimates by updating radar rainfall fields with windshield wiper observations

238 The RaDAR (RanGDP/AR) pathway represents a general importin-

239 the Animal and Plant Health Agency (APHA)'s RADAR (Rapid Analysis and Detection of Animal-related Ri

240 This new 'RADAR' (rapid approach to DNA adduct recovery) assay acc

241 g persistent AF underwent ablation using the RADAR (Real-Time Electrogram Analysis for Drivers of Atr

242 rototype where the raw data collected at the radar receiving channel shows obvious patterns that refl

243 tin-dependent quality control pathway called RADAR (receptor accumulation and degradation in the abse

244 Anomalously specular radar reflections (ASRR) from Titan's tropical region we

245 Radar reflections within the deposits reveal a laterally

246 eted as lakes on the basis of their very low radar reflectivity and morphological similarities to lak

247 eveals the regulating role of the background radar reflectivity on their observed characteristics.

248 e observe significant differences in surface radar reflectivity, implying substantial spatial variati

249 DOOR/RADAR represents a new paradigm in assessing the risks a

250 As such, radar represents an extremely promising tool for the con

251 ent storm circulation through the use of the radar's unique high-resolution waveforms, which allow th

252 istinctive feature in the synthetic aperture radar (SAR) imagery of the sea surface.

253 al scales and were combined with optical and radar satellite imagery in a machine learning algorithm

254 In the past decade, a new generation of radar satellites have revolutionised our ability to meas

255 hange data, obtained from Synthetic Aperture Radar satellites, form the basis for estimates of aquife

256 or limitation to mapping AGV with the latest radar satellites.

257 The radar scattering characteristics of aerial animals are t

258 hat important metabolites still lie "off the radar screen" in reports of global and comprehensive met

259 The Shallow Radar (SHARAD) on the Mars Reconnaissance Orbiter has im

260 Compared to other CNV callers, CNV Radar showed high sensitivity and specificity.

261 r efficient beam collimation and for guiding radar signals around obstacles, opening a new paradigm f

262 The radar signals penetrate deep into the deposits (more tha

263 ticles were observed to leave a well-defined radar signature (or streak), which could be analyzed to

264 Using data from the Shallow Radar sounder on the Mars Reconnaissance Orbiter, we pre

265 Airborne radar sounding can measure conditions within and beneath

266 We use airborne radar sounding data with a subglacial water routing mode

267 r evaluating imagery, spectral data, and now radar sounding data, the better to understand the link b

268 osses along tens of kilometres with airborne radar sounding of the Dotson and Crosson ice shelves, wh

269 In Antarctica, most digital radar-sounding data have been collected in the last 2 de

270 Shallow Radar soundings from the Mars Reconnaissance Orbiter rev

271 Observations of radar speckle patterns tied to the rotation of Mercury e

272 lychlorinated biphenyls (PCBs) by a military radar station into Saglek Bay, Labrador (Canada) has con

273 flectivity data from 12 weather surveillance radar stations and modelled diurnal probability of occur

274 Our radar stratigraphy rules out hypotheses of erosional inc

275 l conditions leading to the formation of the radar streaks and develop a theoretical framework which

276 Radar studies of a honeybee's flights when it first leav

277 Earlier studies based on radar suggested that most songbirds cross deserts in int

278 and spatial information was streamed to the RADAR system and analyzed to identify driver domains to

279 es in the MIRD system or dose factors in the RADAR system) by patient organ mass.

280 d States in summer using the Next-Generation Radar system; (ii) the altitude-dependent distribution o

281 In general, RADARS System programs reported large increases in the r

282 version, and Addiction-Related Surveillance (RADARS) System to describe trends between 2002 and 2013

283 to 5 GHz (satellite services, LTE networks, radar systems, and WiFi bands).

284 (0.5lambda0) aiming at a compact antenna or radar systems.

285 This study uses the approach of combining radar technology and precipitation gauge measurements to

286 have revealed features not previously on the radar-the "nonswapped" transmembrane architecture, an "i

287 We used RadAR to analyze the radiomic profiles of more than 850

288 From flight to radar to Velcro, biological form and function have inspi

289 8 years of data from 12 weather surveillance radars to estimate over 50% SPR during spring and autumn

290 Using honeybees radar-tracked during their orientation flights in a nove

291 Here, harmonic radar tracking of artificially over-wintered Bombus terr

292 Radar tracking of selected flights revealed a dramatic d

293 RADAR uses conservation, RNA structure, network centrali

294 ltiple myeloma dataset demonstrated that CNV Radar was able to detect a variety of CNVs associated wi

295 Using entomological radar, we demonstrate that free-flying individuals of th

296 Using entomological radar, we showed that the ability to select seasonally f

297 ors from RAdiation Dose Assessment Resource [RADAR] website) and OLINDA/EXM software (version 2.0; HE

298 RADAR will be able to assist scientists in performing ma

299 oved rainfall estimates by combining weather radar with windshield wiper observations.

300 als dispersed from the range of the harmonic radar within less than two days and did not return.