ライフサイエンスコーパス: radar

1 essment of Disease Activity in Rheumatology (RADAR).

2 ar with potential exposure to high-intensity radar.

3 centimeter wavelength Goldstone Solar System Radar.

4 of analysis: assembly stock and interaction radar.

5 y layer using vertical-looking entomological radars.

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

7 es enabled flexible and conformable wideband radar absorber.

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

9 ificantly associated with quartiles from the RADAR, AIMS, and HAQ, providing evidence for the validit

10 arthritis composite and the disease-specific RADAR, AIMS, and HAQ.

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

12 RADAR also includes an expandable listing of tissue-spec

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

14 Satellite radar altimeter measurements show that between 1992 and

15 Satellite radar altimeter measurements show that the average eleva

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

17 Radar altimetry also reveals time-varying subsidence in

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

19 Satellite radar altimetry measurements indicate that the East Anta

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

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

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

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

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

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

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

27 ollecting high-resolution synthetic-aperture radar and larger-scale radiometry and scatterometry data

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

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

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

31 asteroid (29075) 1950 DA, which is based on radar and optical measurements spanning 51 years, reveal

32 Radar and optical observations reveal that the continuou

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

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

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

36 Radar and satellite observations reveal that strong conv

37 Radar and seismic imaging combined with in situ borehole

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

58 d understory cover) simultaneously influence radar backscatter.

59 Radar-based research now encompasses foraging as well as

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

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

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

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

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

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

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

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

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

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

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

71 000, and using near infrared wavelength, the radar cross section can be determined in a tabletop setu

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

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

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

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

76 spectrum, indicating large, smooth areas of radar-dark material.

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

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

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

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

81 the Vostok core site, using ice-penetrating radar data and Global Positioning System (GPS) measureme

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

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

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

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

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

87 an, earthquake of moment magnitude 6.5 using radar data from the Envisat satellite of the European Sp

88 Radar data from the parent circulations indicate the exi

89 The earlier Earth-based radar data lack the resolution and coverage for detailed

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

91 d Station (West Antarctica), ice-penetrating radar data reveal a distinctive fold structure within th

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

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

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

95 catalogue of space-borne synthetic aperture radar data.

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

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

98 Interferometric synthetic aperture radar detected a broad area of uplift (2 to 3 millimeter

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

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

101 floodplain lakes with emergent shrubs permit radar double-bounce returns from water and vegetation su

102 asured the magnitude and polarization of the radar echo versus bistatic angle, beta, for selected lun

103 Recent Earth-based radar echoes imply that surface liquid may be present at

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

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

106 A bistatic radar experiment in 1994, involving reception on Earth o

107 During the Clementine 1 mission, a bistatic radar experiment measured the magnitude and polarization

108 Radar exposure had little effect on mortality in this co

109 overall and for the 20,021 sailors with high radar exposure potential.

110 occupations considered a priori to have high radar exposure were compared with the rates for men in l

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

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

113 ystem and interferometric synthetic aperture radar favor creep at approximately 7 millimeters per yea

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

115 phere of Mars with the MARSIS (Mars Advanced Radar for Subsurface and Ionosphere Sounding) instrument

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

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

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

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

120 The radar forward-scattering properties of different reflect

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

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

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

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

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

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

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

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

129 Airborne radar has detected approximately 100 lakes under the Ant

130 l techniques, including ground and air-borne radars, has provided new insights into how the migrants'

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

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

133 Radar imagery shows that basement structures control the

134 data with interferometric synthetic aperture radar imagery to take into account the deformation assoc

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

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

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

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

139 Radar images of near-Earth asteroid 2000 DP107 show that

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

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

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

143 High-resolution radar images reveal near-Earth asteroid (66391) 1999 KW4

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

145 Dark patches in the radar images show high brightness temperatures and high

146 resent new 20-m resolution, 13-cm-wavelength radar images that show no evidence for concentrated depo

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

148 s and interpretations of earlier Earth-based radar images.

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

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

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

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

153 Spontaneous physical activity measured by radar in the chamber and the ratio of 24-hour EE to SMR

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

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

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

157 esolution interferometric synthetic aperture radar (InSAR) permanent scatterer data allow us to resol

158 ite-based interferometric synthetic aperture radar (InSAR) survey of the remote central Andes volcani

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

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

161 tion of measurements consisting of satellite radar interferograms and water-level changes in geotherm

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

163 Spaceborne radar interferometric delay measurements were used to in

164 The radar interferometric map reveals asymmetric, along-stri

165 the western Tibetan plateau using satellite radar interferometry (InSAR) indicate that slip rates on

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

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

168 ubic kilometers per year, based on satellite radar interferometry data.

169 surface deformation in Yellowstone, based on radar interferometry observations from the European Spac

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

171 Using satellite radar interferometry observations of Greenland, we detec

172 Satellite radar interferometry observations of Pine Island Glacier

173 Results obtained with satellite radar interferometry reveal that bottom melt rates exper

174 unar poles have been obtained by Earth-based radar interferometry with the 3.5-centimeter wavelength

175 lapagos Islands, constructed using satellite radar interferometry, that might help explain this dicho

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

181 Satellite interferometric synthetic aperture radar is uniquely suited to monitoring year-to-year defo

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

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

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

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

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

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

188 The Cassini Titan Radar Mapper imaged about 1% of Titan's surface at a res

189 Cassini's Titan Radar Mapper imaged the surface of Saturn's moon Titan o

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

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

194 enerated from space-based synthetic-aperture radar measurements, which reveals that parts of New Orle

195 central Amazon by the Space Shuttle imaging radar mission, to measure subtle water level changes in

196 Radar mutant axons innervate only the dorsal half of the

197 h the Doppler On Wheels (DOW) mobile weather radar near the point of landfall of hurricane Fran (1996

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

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

200 High-resolution DOW radar observations are contrasted with lower-resolution

201 conventional methods, and suggest that such radar observations can be used for forecasting and to st

202 Radar observations have found specular reflections in 75

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

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

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

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

207 Radar observations of comet Hyakutake (C/1996 B2) made a

208 Radar observations of periodically solar-illuminated lun

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

210 Interferometric Synthetic Aperture Radar observations of surface deformation due to the 199

211 Radar observations of the main-belt, M-class asteroid 21

212 Arecibo radar observations of Titan at 13-centimeter wavelength

213 The radar observations suggest that a comet's activity may b

214 Such a fracture network also explains radar observations that reveal a complex pattern of echo

215 Combined with the specular signatures from radar observations, we infer mechanisms that produce ver

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

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

218 that much of the surface thus far imaged by radar of the haze-shrouded Titan is very young, with per

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

220 clear whether these sequences are 'below the radar' of current sequence alignment tools or whether th

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

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

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

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

225 Moreover, Radar overexpression "dorsalizes" retinal ganglion cell

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

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

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

229 Radar plot of the electronic nose analysis showed that t

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

231 lear from a visual inspection of each of the radar plots that there was a characteristic pattern in t

232 ice, on the basis of modelling of bi-static radar polarization properties and interpretations of ear

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

234 0 km from a subglacial lake seen by airborne radar profiling.

235 h on Adverse Drug/Device events And Reports (RADAR) project.

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

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

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

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

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

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

242 Radar ranging from Arecibo, Puerto Rico, to the 0.5-kilo

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

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

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

246 Radar reflections within the deposits reveal a laterally

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

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

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

250 Although radar remote sensing techniques using interferometric ph

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

252 s obtained with a mobile pencil-beam Doppler radar revealed many previously unresolved structures wit

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

254 re we use interferometric synthetic aperture radar (SAR) data, acquired over the central Amazon by th

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

256 Satellite synthetic aperture radar (SAR) interferometry shows that the magnitude 7.6

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

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

259 The radar scattering characteristics of aerial animals are t

260 detailed studies of the relationship between radar scattering properties, cold traps in permanently s

261 the global ocean from the QuikSCAT satellite radar scatterometer reveal the existence of surprisingly

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

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

264 resent images produced by ground penetrating radar showing the three-dimensional sedimentary structur

265 To produce the strong radar signal, the frozen lake must consist of a mix of s

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

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

268 A method of processing synthetic aperture radar signals that avoids some of the approximations cur

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

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

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

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

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

274 Shallow Radar soundings from the Mars Reconnaissance Orbiter rev

275 We report the first radar soundings of the ionosphere of Mars with the MARSI

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

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

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

279 Our radar stratigraphy rules out hypotheses of erosional inc

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

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

282 analysis is presented of the first harmonic radar studies of pheromone-plume locating flights of mal

283 the ice-sheet structure from airborne 60-MHz radar studies, which indicates that distinct zones of ba

284 Spontaneous physical activity measured by a radar system was also significantly lower (4.6 +/- 0.6%

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

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

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

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

289 (0.5lambda0) aiming at a compact antenna or radar systems.

290 Arecibo and Green Bank radio telescopes as a radar to probe Titan's hidden surface.

291 elocity measurements from synthetic aperture radar to reassess the mass balance of the Ross Ice Strea

292 Using harmonic radar to record the actual flight paths of recruited bee

293 outh America generated from the 2000 Shuttle Radar Topography Mission were compared with earlier cart

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

295 Radar tracking of selected flights revealed a dramatic d

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

297 Using harmonic radar, we show for the first time a striking ontogeny to

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

299 vations obtained with an operational weather radar, which underestimated peak low-level wind speeds.

300 RADAR will be able to assist scientists in performing ma