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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.
46 stronomical units) of the Parker Solar Probe spacecraft(13), each lasting ten days.
47 particle population en route to more distant spacecraft(6).
48                                     The Juno spacecraft acquired direct observations of the jovian ma
49 s first two flybys of Mercury, the MESSENGER spacecraft acquired images confirming that pervasive vol
50                  On 27 August 2016, the Juno spacecraft acquired science observations of Jupiter, pas
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
56                                              Spacecraft and meteorite data now provide a global view
57 more than twice that observed by the Galileo spacecraft and modelled successfully.
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
60                              To communicate, spacecraft and satellites rely on microwave devices, whi
61  sharply, according to the interpretation of spacecraft and stellar occultations.
62                                     However, spacecraft and telescope observations have been unable t
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
65 horizontal offset distance between the Fermi spacecraft and the TGF source.
66 2) samples returned to Earth by the Stardust spacecraft appear to be weakly constructed mixtures of n
67                           As the Shepherding Spacecraft approached the surface, it imaged a 25- to-30
68 larly important at the time when the Voyager spacecraft are leaving our heliosphere.
69                                  The Cassini spacecraft arrived at Saturn in 2004, dropped the Huygen
70                                The Hayabusa2 spacecraft arrived at the near-Earth carbonaceous astero
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
75 ody, acquired during occultation by the Dawn spacecraft at asteroid Vesta.
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
78        The flyby measurements of the Cassini spacecraft at Saturn's moon Rhea reveal a tenuous oxygen
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
83                              None of the 125 spacecraft bacteria showed active growth under the teste
84 nment, GEochemistry, and Ranging (MESSENGER) spacecraft became the first probe to fly past the planet
85                                The MESSENGER spacecraft began detecting energetic electrons with ener
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
88 by the Interstellar Boundary Explorer (IBEX) spacecraft, but they miss the ribbon.
89                             The New Horizons spacecraft carried three instruments that measured the s
90                               The OSIRIS-REx spacecraft carries a sophisticated suite of instruments
91                       Images returned by the spacecraft Clementine have been used to produce a quanti
92                                 The Stardust spacecraft collected thousands of particles from comet 8
93                                  The Cassini spacecraft completed three close flybys of Saturn's enig
94 ill help to determine the biological load of spacecraft components and will also have direct relevanc
95                  The Mars Science Laboratory spacecraft, containing the Curiosity rover, was launched
96 round Saturn bode well for the future as the spacecraft continues to orbit the planet.
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
99  at 94.1 astronomical units, just before the spacecraft crossed the termination shock.
100 tribution of dust impacts indicates that the spacecraft crossed thin, densely populated sheets of par
101                                              Spacecraft data suggest that martian meteorites are not
102 experiments, and there is good evidence from spacecraft data that the process is active on asteroid s
103                                 More than 50 spacecraft debris particles were also identified.
104                                       As the spacecraft descended from 150 to 140 km altitude, the ma
105 , particle size and roughness are beyond the spacecraft design specifications.
106 rs Atmosphere and Volatile Evolution (MAVEN) spacecraft, detected auroral emission in virtually all n
107        From its pole-to-pole orbit, the Juno spacecraft discovered arrays of cyclonic vortices in pol
108                                  The Cassini spacecraft discovered lakes/seas on Titan, however, it d
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
113          The Magnetospheric Multiscale (MMS) spacecraft encounter an electron diffusion region (EDR)
114 of Phoebe resulting from the Cassini-Huygens spacecraft encounter on 11 June 2004.
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
117              In this work, it is shown how a spacecraft equipped with a thrust and subjected to a dra
118                                              Spacecraft exploring Mars such as the Mars Exploration R
119                                     The Dawn spacecraft extensively imaged Vesta's surface, revealing
120                          The Cassini Orbiter spacecraft first skimmed through the tenuous upper atmos
121          On 1 January 2019, the New Horizons spacecraft flew close to (486958) 2014 MU(69), a cold cl
122                                  The Cassini spacecraft flew close to Saturn's small moon Enceladus t
123            In January 2019, the New Horizons spacecraft flew past one of these objects, the 36-kilome
124                  An instrumented Shepherding Spacecraft followed a kinetic impactor and provided--fro
125 sured with Earth-orbiting and interplanetary spacecraft for 40 years.
126 measurement devices and it is widely used in spacecraft for its high accuracy.
127  is generally anhydrous, yet the Deep Impact spacecraft found the entire surface to be hydrated durin
128                             Analysis of Dawn spacecraft Framing Camera image data allows evaluation o
129               The camera onboard the Cassini spacecraft has allowed us to observe many of Saturn's cl
130                                  The Cassini spacecraft has been in orbit around Saturn since 30 June
131                                   The Kepler spacecraft has been monitoring the light from 150,000 st
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
134                                  The Rosetta spacecraft has investigated comet 67P/Churyumov-Gerasime
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
137                                The Hayabusa2 spacecraft has obtained global multicolor images of Ryug
138                                The Voyager 1 spacecraft has passed an important milestone.
139                             The New Horizons spacecraft has performed a comprehensive search for kilo
140              Radio tracking of the MESSENGER spacecraft has provided a model of Mercury's gravity fie
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
143                     A flotilla of subsequent spacecraft has redefined Mars from a volcanic planet to
144                          NASA's New Horizons spacecraft has revealed the complex geology of Pluto and
145             Laser altimetry by the MESSENGER spacecraft has yielded a topographic model of the northe
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
151                 Recent data from the Cassini spacecraft have revealed that Enceladus, the 500-km-diam
152               Measurements by instruments on spacecraft have significantly advanced cosmochemistry.
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
155                                          The spacecraft hovers near the asteroid, with its thrusters
156 s, et l'Activite (OMEGA) on the Mars Express spacecraft identify the distinct mafic, rock-forming min
157                                  The Galileo spacecraft imaged a pair of superimposed ripple patterns
158         During its 1989 flyby, the Voyager 2 spacecraft imaged six small moons of Neptune, all with o
159                         Mariner 9 and Viking spacecraft images revealed that the polar regions of Mar
160 roperties and jet activity from the Stardust spacecraft imaging and the onboard dust monitoring syste
161          Images of Amalthea from two Voyager spacecraft in 1979 and Galileo imaging between November
162  Magnetometer data acquired by the MESSENGER spacecraft in orbit about Mercury permit the separation
163                        New observations from spacecraft in orbit allowed an estimation of gross carbo
164 on scale magnetic cavity observed by the MMS spacecraft in the magnetosheath.
165   Simultaneous measurements by more than ten spacecraft in the near-Earth environment reveal the evan
166                                         Each spacecraft in the network can have different subsystem c
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
169                                The Hayabusa2 spacecraft investigated the small asteroid Ryugu, which
170 orms of perturbations in the altitude of the spacecraft is also investigated in this work, like the s
171 pecific set of parameters of the thrust, the spacecraft is bounded to a given altitude.
172                                   The Kepler spacecraft is monitoring more than 150,000 stars for evi
173  on the European Space Agency's Mars Express spacecraft is providing new constraints on the martian s
174 mapping altitude by the Mars Global Surveyor spacecraft, is presented here.
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
179                                              Spacecraft launched from Earth can transport hitchhiker
180 rs Atmosphere and Volatile Evolution (MAVEN) spacecraft made comprehensive measurements of the Mars u
181               The cameras aboard the Cassini spacecraft mainly observe small (1 to 10 micrometers) du
182 was recently explored by NASA's New Horizons spacecraft, making closest approach on 14 July 2015.
183                             The New Horizons spacecraft mapped colors and infrared spectra across the
184 al-velocity plasma flow, indicating that the spacecraft may be close to the heliopause, the border be
185                         As it is, Mars-bound spacecraft may frequently be contaminated with aspergill
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
189                             The Mars Phoenix spacecraft measurements of carbon isotopes [referenced t
190  with high spatial resolution, obtained from spacecraft measurements of infrared spectra of Jupiter's
191                           New laboratory and spacecraft measurements strongly indicate that much of t
192                                              Spacecraft missions impose serious limitations on instru
193 n and Sensing Satellite (LCROSS) Shepherding Spacecraft monitored the impact and ejecta.
194       Using images acquired by the Chang'e-2 spacecraft, more than 200 boulders have been identified
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
199                         Here, we show, using spacecraft observations and particle-in-cell (PIC) simul
200               By using fortuitous multipoint spacecraft observations during a rare isolated fast plas
201                            Here we show that spacecraft observations during this period were highly s
202                        Here we report Kepler spacecraft observations of a single Sun-like star, which
203                         Here we report three-spacecraft observations of accelerated flow associated w
204                  Here we report the combined spacecraft observations of Saturn acquired over one Satu
205                   We validated the theory by spacecraft observations of the strong, compressional mag
206 situ energy-specific and temporally resolved spacecraft observations reveal an isolated third ring, o
207                                              Spacecraft observations suggest that the plumes of Satur
208               Because of the lack of in-situ spacecraft observations, the onset mechanism of magnetot
209 gnetic field is different compared with past spacecraft observations.
210 r cap has remained enigmatic since the first spacecraft observations.
211 ations of supernova remnant W44 by the Fermi spacecraft observatory support the idea that the bulk of
212                             On approach, the spacecraft observed frequent natural outbursts, a mean r
213                        The New Horizons (NH) spacecraft observed Io's aurora in eclipse on four occas
214                             The New Horizons spacecraft observed Jupiter's icy satellites Europa and
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
220 ection from Ryugu's surface by the Hayabusa2 spacecraft on 21 February 2019.
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
225                         In 2017, the Cassini spacecraft passed inside the planet's rings, allowing in
226                                  The Cassini spacecraft passed within 168.2 kilometers of the surface
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
231                            Since the Cassini spacecraft reached Saturn's orbit in 2004, its instrumen
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
234  radio-communications between the ground and spacecraft returning to Earth.
235 ptured from comet 81P/Wild 2 by the Stardust spacecraft reveal indigenous aliphatic hydrocarbons simi
236                   Instruments on the Cassini spacecraft reveal that a heat source within Saturn's moo
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
240                         Data from the Kepler spacecraft reveal transits of the planet across both sta
241 ocal plasma flow speed is high, and near the spacecraft's closest approach, where atmospheric density
242          Radio Doppler data from the Galileo spacecraft's encounter with Amalthea, one of Jupiter's s
243                             The New Horizons spacecraft's encounter with the cold classical Kuiper Be
244                         By using the Cassini spacecraft's gravitational data, along with Pioneer and
245                                  The Cassini spacecraft's in situ observations reveal that energetic
246                                The MESSENGER spacecraft's observations of Mercury's ionized exosphere
247 ument onboard the Cassini Orbiter during the spacecraft's passage over the rings.
248  on dust impacts detected during the Galileo spacecraft's traversal of the outer ring region: we find
249  1998 until September 2005, when the Cassini spacecraft saw them reappear.
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
258                 The variations measured from spacecraft since 1978 are too small to have contributed
259 the Mercury Laser Altimeter on the MESSENGER spacecraft spans approximately 20% of the near-equatoria
260                                  The Rosetta spacecraft spent 2 years orbiting comet 67P/Churyumov-Ge
261 d, and oligotrophic in nature for assembling spacecraft subsystems.
262  and Security-Regolith Explorer (OSIRIS-REx) spacecraft surveyed Bennu's immediate environment, photo
263                                     The Dawn spacecraft targeted 4 Vesta, believed to be a remnant in
264 aging science experiment onboard the Cassini spacecraft that address some of these issues.
265            We present a design concept for a spacecraft that can controllably alter the trajectory of
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
268          We present observations by the Dawn spacecraft that reveal a heavily cratered surface, a het
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
271 was collected during passage of the Stardust spacecraft through the coma of comet 81P/Wild 2.
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.
274 cs and Space Administration's (NASA) Cassini spacecraft to generate transit spectra.
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
281                                              Spacecraft-to-spacecraft tracking observations from the
282  occasional temporary re-orientations of the spacecraft (totalling about 10-25 hours every 2 months)
283                                Spacecraft-to-spacecraft tracking observations from the Gravity Recove
284                             The New Horizons spacecraft traversed the length of the jovian magnetotai
285                             The New Horizons spacecraft traversed the magnetotail to distances exceed
286  and gravity field are derived from measured spacecraft velocity perturbations at fly-by distances be
287         Over the past five decades, however, spacecraft visits to many targets transformed these earl
288  in the solar wind have been measured by the spacecraft Voyager 1 and Voyager 2.
289 we show, based on observations from the NASA spacecraft Voyager and Cassini, that gases alone cannot
290                         Recently, the Hinode spacecraft was launched to observe and measure the plasm
291 n the Mars Atmosphere and Volatile Evolution spacecraft, we demonstrate that water is instead transpo
292                     Using imaging from three spacecraft, we have mapped two global-scale organized co
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
295                By using data from the Kepler spacecraft, we report the detection of such a "self-lens
296            Using a conjunction between eight spacecraft, we show that this conversion takes place wit
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

 
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