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1 oposed in order to bound the altitude of the spacecraft.
2 ity Recovery and Interior Laboratory (GRAIL) spacecraft.
3 n observed on many cometary nuclei mapped by spacecraft.
4 sions using the combined perspectives of two spacecraft.
5 would be ejected and could be measured by a spacecraft.
6 n the Mars Atmosphere and Volatile Evolution spacecraft.
7 nalysis mass spectrometer aboard the Rosetta spacecraft.
8 ts) of the SBN over the traditional monolith spacecraft.
9 bing a region that has never been visited by spacecraft.
10 creened here were recovered from actual Mars spacecraft.
11 ic particle radiation environment inside the spacecraft.
12 roid Vesta, revealed in images from the Dawn spacecraft.
13 exploration activities and operations aboard spacecraft.
14 early 6 years of observations by the Cassini spacecraft.
15 the plasma-wave instrument on the Voyager 2 spacecraft.
16 , unmanned gliding vehicles and multisegment spacecraft.
17 he embedded dust belts imaged by the Voyager spacecraft.
18 ptured from Comet 81P/Wild 2 by the Stardust spacecraft.
19 and Ionospheric Sounding on the Mars Express spacecraft.
20 ariable at scales that may be sampled by the spacecraft.
21 ter suite of instruments on the Mars Odyssey spacecraft.
22 documented by the instruments on the Cassini spacecraft.
23 to predict measurements from a second/third spacecraft.
24 nstrument on board the orbiting Mars Express spacecraft.
25 g from Earth, and by the Voyager and Cassini spacecraft.
26 the plasma wave instrument on the Voyager 1 spacecraft.
27 lanetary environments on manned and unmanned spacecraft.
28 O observed in a global survey by the Odyssey spacecraft.
29 he Solar and Heliospheric Observatory (SOHO) spacecraft.
30 infrared during the swing-by of the Cassini spacecraft.
31 pectrometer onboard the Mars Global Surveyor spacecraft.
32 ion using data collected by the New Horizons spacecraft.
33 t high altitudes (~5300 km) by the MESSENGER spacecraft.
34 ntification, and Security-Regolith Explorer) spacecraft.
35 nditions, and subsequently could contaminate spacecraft.
36 rs Atmosphere and Volatile Evolution (MAVEN) spacecraft.
37 eme conditions, such as those encountered by spacecraft.
38 ervations of the main rings from the Cassini spacecraft.
39 erved by the Magnetospheric Multiscale (MMS) spacecraft.
40 rs Atmosphere and Volatile Evolution (MAVEN) spacecraft.
41 ov-Gerasimenko (67P), visited by the Rosetta spacecraft.
42 nd attractors, which bound the motion of the spacecraft.
43 ld, a task to be soon undertaken by the Juno spacecraft.
44 able for extreme environment applications in spacecraft.
45 le, in structural components of aircraft and spacecraft.
49 s first two flybys of Mercury, the MESSENGER spacecraft acquired images confirming that pervasive vol
51 and Neutral Analysis (ROSINA) on the Rosetta spacecraft analyzed the isotopes of xenon in the coma of
52 Laser Altimeter on the Mars Global Surveyor spacecraft and basal topography from the Mars Advanced R
53 in the hypersonic vehicle, rockets, re-entry spacecraft and defence sectors, but few materials can cu
54 2O ice) have been observed numerous times by spacecraft and ground-based telescopes, showing that clo
55 uch missions will require crew to transit in spacecraft and live in surface habitats that instantiate
58 olution images from the Mars Global Surveyor spacecraft and moderately high-resolution Thermal Emissi
59 - as part of instrumental suites on robotic spacecraft and planetary landers; this necessitates robu
63 alogy Mapper instrument on the Chandrayaan-1 spacecraft and the Lunar Reconnaissance Orbiter Camera (
64 pace ENvironment, GEochemistry, and Ranging) spacecraft and the NASA Goddard Geophysical and Astronom
66 2) samples returned to Earth by the Stardust spacecraft appear to be weakly constructed mixtures of n
71 esearch on growth of microorganisms found in spacecraft assembly clean rooms under simulated Martian
72 onate filter assemblies were deployed in the spacecraft assembly cleanroom facility to collect fallou
73 comet 81P/Wild 2 collided with the Stardust spacecraft at 6.1 kilometers per second, producing hyper
74 nment, GEochemistry, and Ranging (MESSENGER) spacecraft at altitudes below 150 kilometers, we have de
76 al remote sensing instruments on the Cassini spacecraft at closest approach during a fly-by on 25-26
77 d by spacecraft near Earth(2,3) and later by spacecraft at heliocentric distances as small as 62 sola
79 onboard the European Space Agency's Rosetta spacecraft at scales of better than 0.8 meter per pixel
80 mentation of the sunshade as a cloud of many spacecraft, autonomously stabilized by modulating solar
81 pressure on the growth of chemoorganotrophic spacecraft bacteria and whether the addition of Mars rel
82 versity of chemoorganotrophic and culturable spacecraft bacteria do not grow under the tested conditi
84 nment, GEochemistry, and Ranging (MESSENGER) spacecraft became the first probe to fly past the planet
86 ss mission, an aerobraking campaign took the spacecraft below the ionosphere into the very weakly ele
87 graph is traded for the inconvenience of two spacecraft, but the daunting optics challenges are repla
94 ill help to determine the biological load of spacecraft components and will also have direct relevanc
97 c fields measured by Voyager 1 show that the spacecraft crossed or was crossed by the termination sho
98 lds measured by Voyager 1 (V1) show that the spacecraft crossed the boundary of an unexpected region
100 tribution of dust impacts indicates that the spacecraft crossed thin, densely populated sheets of par
102 experiments, and there is good evidence from spacecraft data that the process is active on asteroid s
106 rs Atmosphere and Volatile Evolution (MAVEN) spacecraft, detected auroral emission in virtually all n
109 the final phase of the Cassini mission, the spacecraft dived between the planet and its innermost ri
110 resent data collected from Ulysses and other spacecraft during 1992-2002 and a variety of older measu
111 adio Doppler data generated with the Galileo spacecraft during its second encounter with Ganymede on
112 ophic bacteria typically recovered from Mars spacecraft during planetary protection bioburden screeni
115 regime from 10(-14) to 10(-7) kilograms, the spacecraft encountered regions of intense swarms of part
116 acecraft on 11 June 2004 (19 days before the spacecraft entered orbit around Saturn) provided an oppo
127 is generally anhydrous, yet the Deep Impact spacecraft found the entire surface to be hydrated durin
132 unched Interstellar Boundary Explorer (IBEX) spacecraft has completed its first all-sky maps of the i
133 (MARSIS) instrument aboard the Mars Express Spacecraft has detected nadir echoes offset in time-dela
135 on and Neutral Analysis) onboard the Rosetta spacecraft has measured the coma composition of comet 67
136 (VIR) mapping spectrometer onboard the Dawn spacecraft has now detected water absorption features wi
141 pectrometer) instrument on board the Rosetta spacecraft has provided evidence of carbon-bearing compo
142 low from Dawn Framing Camera images.The Dawn spacecraft has provided orbital bistatic radar observati
146 The Huygens probe, launched from the Cassini spacecraft, has made the first direct observations of th
147 the Gravity Recovery and Interior Laboratory spacecraft have clarified the origin of lunar mass conce
148 Optical observations from the New Horizons spacecraft have identified lightning at high latitudes a
149 here made by instruments on the New Horizons spacecraft have implications for the stability and dynam
150 and contorted F ring returned by the Cassini spacecraft have revealed phenomena not previously detect
153 ions have been observed, consistent with the spacecraft having crossed the termination shock into the
154 thermal infrared imager (TIR)(4) onboard the spacecraft Hayabusa2(5), indicating that the asteroid's
156 s, et l'Activite (OMEGA) on the Mars Express spacecraft identify the distinct mafic, rock-forming min
160 roperties and jet activity from the Stardust spacecraft imaging and the onboard dust monitoring syste
162 Magnetometer data acquired by the MESSENGER spacecraft in orbit about Mercury permit the separation
165 Simultaneous measurements by more than ten spacecraft in the near-Earth environment reveal the evan
167 entes have been observed by the New Horizons spacecraft in the Tartarus Dorsa region of Pluto (220 de
168 es in technology have enabled telescopic and spacecraft instruments to provide important data that si
170 orms of perturbations in the altitude of the spacecraft is also investigated in this work, like the s
173 on the European Space Agency's Mars Express spacecraft is providing new constraints on the martian s
175 fter 40 close flybys of Titan by the Cassini spacecraft, it has become clear that no such oceans exis
176 Emission Imaging System on the Mars Odyssey spacecraft, it is possible to observe such heterogeneiti
177 ations, Geodesy and Heat Transport (InSight) spacecraft landed successfully on Mars and imaged the su
178 highly variable within the potential Phoenix spacecraft landing ellipses, and is likely to be variabl
180 rs Atmosphere and Volatile Evolution (MAVEN) spacecraft made comprehensive measurements of the Mars u
182 was recently explored by NASA's New Horizons spacecraft, making closest approach on 14 July 2015.
184 al-velocity plasma flow, indicating that the spacecraft may be close to the heliopause, the border be
186 e gamma ray spectrometer on the Mars Odyssey spacecraft measured an enhancement of atmospheric argon
187 ng its first flyby of Mercury, the MESSENGER spacecraft measured the planet's near-equatorial magneti
188 e after solar eruptions has been verified by spacecraft measurements near Earth, its formation on the
190 with high spatial resolution, obtained from spacecraft measurements of infrared spectra of Jupiter's
195 maging 3D distribution functions during fast spacecraft motion, we also discuss the operation strateg
196 ersonic solar wind(1) was first confirmed by spacecraft near Earth(2,3) and later by spacecraft at he
197 e magnetometer data collected by the Galileo spacecraft near Io provide evidence of electromagnetic i
198 he reliability of the wireless links between spacecraft (nodes) to enable any survivability improveme
206 situ energy-specific and temporally resolved spacecraft observations reveal an isolated third ring, o
211 ations of supernova remnant W44 by the Fermi spacecraft observatory support the idea that the bulk of
215 maging Instrument (MIMI) onboard the Cassini spacecraft observed the saturnian magnetosphere from Jan
216 nt periodic structures in waves, the Cluster spacecraft observes 'ring' distributions of protons in v
217 In February and March 2007, the New Horizons spacecraft obtained a global snapshot of Io's volcanism.
218 We combine measurements made by the four spacecraft of the Magnetospheric Multiscale mission to d
219 lose fly-by of Phoebe by the Cassini-Huygens spacecraft on 11 June 2004 (19 days before the spacecraf
221 e-based networks (SBNs) allow the sharing of spacecraft on-orbit resources, such as data storage, pro
222 nd is accordingly favoured as a location for spacecraft operation because of the benign environment.
223 iment on the European Space Agency's Rosetta spacecraft orbiting comet 67P/Churyumov-Gerasimenko.
224 uorescence spectra obtained by the MESSENGER spacecraft orbiting Mercury indicate that the planet's s
227 System visible images from the Mars Odyssey spacecraft permit more comprehensive geologic and climat
228 or an outbreak of an infectious disease in a spacecraft presents one such concern, which is compounde
229 a-ray Burst Monitor (GBM) on board the Fermi spacecraft provided the energetic radiation measurements
230 tandard ground timing allowed a solution for spacecraft range, range rate, and acceleration, as well
232 and Security-Regolith Explorer (OSIRIS-REx) spacecraft recently arrived at the near-Earth asteroid (
233 ued planetary scientists since the Mariner 9 spacecraft returned the first close-up image in 1972, bu
235 ptured from comet 81P/Wild 2 by the Stardust spacecraft reveal indigenous aliphatic hydrocarbons simi
237 mera onboard the Mars Reconnaissance Orbiter spacecraft reveal that Athabasca Valles is now entirely
238 images of Mercury obtained by the MESSENGER spacecraft reveal that its surface has an overall relati
239 he Cosmic Dust Analyzer on board the Cassini spacecraft reveal that the Saturnian system is passed by
241 ocal plasma flow speed is high, and near the spacecraft's closest approach, where atmospheric density
248 on dust impacts detected during the Galileo spacecraft's traversal of the outer ring region: we find
250 rstellar dust clouds, ballistic penetrators, spacecraft shielding and ductility in high-performance c
251 raRed Mapping Spectrometer on board the Dawn spacecraft show a clear detection of an organic absorpti
252 btained during the flyby of the New Horizons spacecraft show an unexpected lack of ultraviolet nightg
253 tary nuclei imaged from flyby and rendezvous spacecraft show common evidence of layered structures an
254 nment, GEochemistry, and Ranging (MESSENGER) spacecraft show decreases in the flux of epithermal and
255 om the Interstellar Boundary Explorer (IBEX) spacecraft show that the relative motion of the Sun with
256 nment, GEochemistry, and Ranging (MESSENGER) spacecraft, show that the spatial distribution of region
257 measurements of Ceres obtained from the Dawn spacecraft, showing that it is in hydrostatic equilibriu
259 the Mercury Laser Altimeter on the MESSENGER spacecraft spans approximately 20% of the near-equatoria
262 and Security-Regolith Explorer (OSIRIS-REx) spacecraft surveyed Bennu's immediate environment, photo
266 ions considered consist of several networked spacecraft that can tap into each other's Command and Da
267 from the European Space Agency Mars Express spacecraft that indicate that such lakes may still exist
269 ing Spectrometer (VIMS) on board the Cassini spacecraft, that strongly indicate that ethane, probably
270 solid state passive switchable radiator for spacecraft thermal control have been performed in a simu
272 mical units from the Sun, becoming the first spacecraft to begin exploring the heliosheath, the outer
273 eutral Mass Spectrometer onboard the Cassini spacecraft to detect molecular hydrogen in the plume.
275 on the European Space Agency's Venus Express spacecraft to identify compositional differences in lava
276 use data obtained from the orbiting Akatsuki spacecraft to investigate how the super-rotation is main
277 ity Recovery and Interior Laboratory (GRAIL) spacecraft to investigate the gravitational field of Ori
278 We used the spectrometer onboard the Dawn spacecraft to map their spatial distribution on the basi
279 lize magnetic cavity observations by one MMS spacecraft to predict measurements from a second/third s
280 Emission Spectrometer (TES) aboard the Aura spacecraft, to investigate aspects of the atmospheric hy
282 occasional temporary re-orientations of the spacecraft (totalling about 10-25 hours every 2 months)
286 and gravity field are derived from measured spacecraft velocity perturbations at fly-by distances be
289 we show, based on observations from the NASA spacecraft Voyager and Cassini, that gases alone cannot
291 n the Mars Atmosphere and Volatile Evolution spacecraft, we demonstrate that water is instead transpo
293 d energy/charge spectrometers on the Cassini spacecraft, we have obtained evidence for tholin formati
294 (TEC) maps and measurements from the THEMIS spacecraft, we investigated simultaneous ionosphere and
297 erial was observed by a second "shepherding" spacecraft, which carried nine instruments, including ca
298 onnaissance Orbiter Camera (LROC) on the LRO spacecraft, which indicates the peak ring is composed of
299 r aboard the European Space Agency's Rosetta spacecraft, which is found to be (5.3 +/- 0.7) x 10(-4)-
300 bservations of lightning flashes by the Juno spacecraft with energies of approximately 10(5)-10(8) jo