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Akatsuki (spacecraft)

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Akatsuki
A model of the spacecraft Akatsuki
NamesVenus Climate Orbiter (VCO)
PLANET-C
Mission typeVenus orbiter
OperatorJAXA
COSPAR ID2010-020D Edit this at Wikidata
SATCAT no.36576
WebsiteJAXA
JAXA Special Site
Mission duration13 years, 11 months
Spacecraft properties
ManufacturerNEC Space Technologies
Launch mass517.6 kg (1,141 lb)[1]
Dry mass320 kg (710 lb)
Dimensions1.04 × 1.45 × 1.44 m (3.4 × 4.8 × 4.7 ft)
Power>700 watts at 0.7 AU[1]
Start of mission
Launch date21 May 2010, 21:58:22 (2010-05-21UTC21:58:22Z) UTC[2]
RocketH-IIA 202
Launch siteTanegashima YLP-1
End of mission
Declared29 May 2024
Last contactApril 2024
Orbital parameters
Reference systemCytherocentric
Eccentricity0.971
Pericytherion altitude1,000–10,000 km (620–6,210 mi)[3]
Apocytherion altitude370,000 km (230,000 mi)[3]
Inclination3.0°
Period10.8 days[4]
Flyby of Venus (failed insertion)
Closest approach6 December 2010, 23:49:00 UTC
Distance550 kilometers (340 mi)
Venus orbiter
Orbital insertion7 December 2015[5][6]
PLANET series
← Nozomi

Akatsuki (あかつき, 暁, "Dawn"), also known as the Venus Climate Orbiter (VCO) and Planet-C, was a Japan Aerospace Exploration Agency (JAXA) space probe tasked with studying the atmosphere of Venus. It was launched aboard an H-IIA 202 rocket on 20 May 2010,[7] but failed to enter orbit around Venus on 6 December 2010. After the craft orbited the Sun for five years, engineers successfully placed it into an alternative Venusian elliptic orbit on 7 December 2015 by firing its attitude control thrusters for 20 minutes and made it the first Japanese satellite orbiting Venus.[5][6][8][9]

By using five different cameras working at several wavelengths, Akatsuki studied the stratification of the atmosphere, atmospheric dynamics, and cloud physics.[10][11] Astronomers working on the mission reported detecting a possible gravity wave (not to be confused with gravitational waves) in Venus' atmosphere in December 2015.[12][13]

JAXA lost contact with the probe in late April 2024.[14]

Mission

[edit]

Akatsuki is Japan's first planetary exploration mission since the failed Mars orbiter Nozomi probe which was launched in 1998. Akatsuki was originally intended to conduct scientific research for two or more years from an elliptical orbit around Venus ranging from 300 to 80,000 km (190 to 49,710 mi) in altitude,[1] but its alternate orbit had to be highly elliptical ranging between 1,000 and 10,000 kilometres (620 and 6,210 mi) at its nearest point and about 360,000 kilometres (220,000 mi) at its farthest. This larger orbit takes 10 days to complete instead of the originally planned 30 hours.[15] The budget for this mission is ¥14.6 billion (US$174 million) for the satellite and ¥9.8 billion (US$116 million) for the launch.[16]

Observations include cloud and surface imaging from an orbit around the planet with cameras operating in the infrared, visible and UV wavelengths to investigate the complex Venusian meteorology and elucidate the processes behind the mysterious atmospheric super-rotation. On Venus, while the planet rotates at 6 kilometres per hour (3.7 mph) at the equator, the atmosphere spins around the planet at 300 kilometres per hour (190 mph). Other experiments are designed to confirm the presence of lightning and to determine whether volcanism occurs currently on Venus.[17]

Spacecraft design

[edit]
Configuration of Akatsuki spacecraft (left) and a photograph of the spacecraft with the solar array paddles being folded (right).[10]
Schematic of the three-dimensional observation by Akatsuki.[10]

The main bus is a 1.45 × 1.04 × 1.44 m (4.8 × 3.4 × 4.7 ft) box with two solar arrays, each with an area of about 1.4 m2 (15 sq ft). The solar arrays provide over 700 W of power while in Venus orbit. The total mass of the spacecraft at launch was 517.6 kg (1,141 lb).[1] The mass of the science payload is 34 kg (75 lb).[18]

Propulsion is provided by a 500-newton (110 lbf) bi-propellant, hydrazine-dinitrogen tetroxide orbital maneuvering engine and twelve mono-propellant hydrazine reaction control thrusters, eight with 23 N (5.2 lbf) of thrust and four with 3 N (0.67 lbf).[1] It is the first spacecraft to use a ceramic (silicon nitride) retrofire thruster.[19] The total propellant mass at launch was 196.3 kg (433 lb).[1]

Communication is via an 8 GHz, 20-watt X-band transponder using the 1.6 m (5 ft 3 in) high-gain antenna. The high-gain antenna is flat to prevent heat from building up in it.[11] Akatsuki also has a pair of medium-gain horn antennas mounted on turntables and two low-gain antennas for command uplink. The medium-gain horn antennas are used for housekeeping data downlink when the high-gain antenna is not facing Earth.[1]

Instruments

[edit]

The scientific payload consists of six instruments. The five imaging cameras are exploring Venus in wavelengths from ultraviolet to the mid-infrared:[20][21]

  1. the Lightning and Airglow Camera (LAC) is looking for lightning in the visible spectrum (552–777 nm)
  2. the ultraviolet imager (UVI) is studying the distribution of specific atmospheric gases such as sulfur dioxide and the famous unknown absorber at ultraviolet wavelengths (283–365 nm)
  3. the longwave infrared camera (LIR) is studying the structure of high-altitude clouds at a wavelength where they emit heat (10 μm)
  4. the infrared 1 μm camera (IR1) is imaging on the night side heat radiation (0.90–1.01 μm) emitted from Venus's surface and help researchers to spot active volcanoes, if they exist. While on the day side, it sensed the solar near-infrared radiation (0.90 μm) reflected by the middle clouds. Unavailable for observation after December 2016 due to an electronic failure.[22][23]
  5. the infrared 2 μm camera (IR2) studied the night side lower clouds' opacity to the thermal emission from the surface and deeper atmosphere (1.74–2.32 μm). It also sensed on the day side the CO2 band at 2.02 μm, which can be used to infer the altitude of the top of the clouds. Finally, the 1.65-μm filter was used during the cruise phase to study the zodiacal light. Unavailable for observation after December 2016 due to an electronic failure.[23]
  6. the Ultra-Stable Oscillator (USO) for performing radio occultation experiments.

Public relations

[edit]

A public relations campaign was held between October 2009 and January 2010 by the Planetary Society and JAXA, to allow individuals to send their name and a message aboard Akatsuki.[24][25] Names and messages were printed in fine letters on an aluminium plate and placed aboard Akatsuki.[24] 260,214 people submitted names and messages for the mission.[26] Around 90 aluminium plates were created for the spacecraft,[27] including three aluminium plates in which the images of the Vocaloid Hatsune Miku and her super deformed-styled figure Hachune Miku were printed.[28]

Operations

[edit]

Launch

[edit]
The launch of Akatsuki
Animation of Akatsuki trajectory from 21 May 2010 to 31 December 2016
  Akatsuki
  Venus
  Earth
  Sun

Akatsuki left the Sagamihara Campus on 17 March 2010, and arrived at the Tanegashima Space Center's Spacecraft Test and Assembly Building 2 on 19 March. On 4 May, Akatsuki was encapsulated inside the large payload fairing of the H-IIA rocket that launched the spacecraft, along with the IKAROS solar sail, on a 6-month journey to Venus. On 9 May, the payload fairing was transported to the Tanegashima Space Center's Vehicle Assembly Building, where the fairing was mated to the H-IIA launch vehicle itself.[29]

The spacecraft was launched on 20 May 2010 at 21:58:22 (UTC) from the Tanegashima Space Center,[17] after being delayed because of weather from its initial 18 May scheduled target.[30]

Orbit insertion failure

[edit]
Movement of the spacecraft orbit and Venus in a Sun-Earth line fixed rotating coordinate in the original plan. Numerals in the figure indicate days after VOI.[10]

Akatsuki was planned to initiate orbit insertion operations by igniting the orbital maneuvering engine at 23:49:00 on 6 December 2010 UTC.[29] The burn was supposed to continue for twelve minutes, to an initial Venus orbit with an apoapsis altitude of 80,000 km (50,000 mi), a periapsis altitude of 300 km (190 mi), and a 30 h orbital period.[31]

The orbit insertion maneuver was confirmed to have started on time, but after the expected blackout due to occultation by Venus, the communication with the probe did not recover as planned. The probe was found to be in safe-hold mode, spin-stabilized state with ten minutes per rotation.[32] Due to the low communication speed through the low-gain antenna, it took a while to determine the state of the probe.[33] JAXA stated on 8 December that the probe's orbital insertion maneuver had failed.[34][35] At a press conference on 10 December, officials reported that Akatsuki's engines fired for less than three minutes, far less than what was required to enter into Venus orbit.[36] Further research found that the likely reason for the engine malfunction was salt deposits jamming the valve between the helium pressurization tank and the fuel tank. As a result, engine combustion became oxidizer-rich, with resulting high combustion temperatures damaging the combustion chamber throat and nozzle. A similar vapor leakage problem destroyed NASA's Mars Observer probe in 1993.[37]

As a result, the probe was in a heliocentric orbit, rather than Venus orbit. Since the resulting orbit had an orbital period of 203 days,[38] shorter than Venus' orbital period of 225 days, the probe drifted around the Sun compared to Venus.

Recovery efforts

[edit]

JAXA developed plans to attempt another orbital insertion burn when the probe returned to Venus in December 2015. This required placing the probe into "hibernation" or safe mode to prolong its life beyond the original 4.5-year design. JAXA expressed some confidence in keeping the probe operational, pointing to reduced battery wear, since the probe was then orbiting the Sun instead of its intended Venusian orbit.[39]

Telemetry data from the original failure suggested that the throat of its main engine, the orbit maneuver engine (OME) was still largely intact, and trial jet thrusts of the probe's onboard OME were performed twice, on 7 and 14 September 2011.[29] However, the thrust was only about 40 newtons (9.0 lbf), which was 10% of expectations. Following these tests, it was determined that insufficient specific impulse would be available for orbital maneuvering by the OME. It was concluded that the remaining combustion chamber throat was completely destroyed by transient ignition of the engine. As a result, the selected strategy was to use four hydrazine attitude control thrusters, also called reaction control system (RCS), to drive the probe into orbit around Venus. Because the RCS thrusters do not need oxidiser, the remaining 65 kilograms (143 lb) of oxidiser (MON) was vented overboard in October 2011 to reduce the mass of the spacecraft.[37]

Three peri-Venus orbital maneuvers were executed on 1 November,[17] 10 and 21 November 2011 using the RCS thrusters. A total delta-v of 243.8 metres per second (800 ft/s) was imparted to the spacecraft. Because the RCS thrusters' specific impulse is low compared to the specific impulse of the OME, the previously planned insertion into low Venusian orbit became impossible. Instead, the new plan was to place the probe in a highly elliptical orbit with an apoapsis of a hundred thousand kilometers and a periapsis of a few thousand kilometers from Venus. Engineers planned for the alternate orbit to be prograde (in the direction of the atmospheric super-rotation) and lie in the orbital plane of Venus. The method and orbit were announced by JAXA in February 2015, with an orbit insertion date of 7 December 2015.[40] The probe reached its most distant point from Venus on 3 October 2013 and had been approaching the planet since then.[41]

Orbit insertion

[edit]
Animation of Akatsuki's trajectory around Venus from 1 December 2015
   Akatsuki ·   Venus

After performing the last of a series of four trajectory correction maneuvers between 17 July and 11 September 2015, the probe was established on a trajectory to fly past Venus on 7 December 2015, when Akatsuki would make a maneuver to enter Venus orbit after a 20-minute burn with four thrusters that were not rated for such a hefty propulsive maneuver.[5][6][42] Instead of taking about 30 hours to complete an orbit around Venus—as was originally planned—the new orbit targeted would place Akatsuki in a nine-day orbit after an adjustment in March 2016.[4]

After JAXA engineers measured and calculated its orbit following the 7 December orbital insertion, JAXA announced on 9 December that Akatsuki had successfully entered the intended elliptical orbit, as far as 440,000 km (270,000 mi) from Venus, and as close as 400 km (250 mi) from Venus's surface with an orbital period of 13 days and 14 hours.[43]

A follow-up thruster burn on 26 March 2016 lowered Akatsuki's apoapsis to about 370,000 km (230,000 mi), periapsis altitude periodically changing from 1,000 to 10,000 kilometres (620 to 6,210 mi), and shortened its orbital period from 13 to about 10 days.[3][4]

Status

[edit]

The orbiter started its two-year period of "regular" science operations in mid-May 2016.[44] Since 9 December 2016, the near-infrared 1-μm and 2-μm cameras have been unavailable for observations due to an electronic failure.[22][23] Its long-wave infrared camera, ultraviolet imager, and lightning and airglow camera continue normal operation.[23]

By April 2018, Akatsuki finished its regular observation phase, and entered an extended operation phase.[45] Extended operations are approved until the end of 2020, with further mission extensions to be considered based on the spacecraft's condition at that time. Akatsuki has enough fuel to continue operating for at least 2 more years as of November 2019.[46]

As of March 2024, operation was planned to continue through FY2028.[47] In April 2024, degraded precision of attitude control resulted in failure of communication.[48] JAXA declared the spacecraft's loss of contact with Earth on May 29, 2024.[49][50]

Science

[edit]

Three hours after insertion in December 2015 and in "a few glimmers in April and May" 2016 the craft's instruments recorded a "bow-shape feature in the atmosphere stretching 6,000 miles, almost pole to pole — a sideways smile".[51] Scientists on the project termed the feature a "gravity wave" in the planet's winds above the Aphrodite Terra region of rift valleys and mountains reaching heights of over 4,000 metres (13,000 ft).[12][13] The mission is collecting data in all relevant spectral bands from ultraviolet (280 nm) to mid-infrared wavelengths (10 μm).[52]

Images from the Akatsuki orbiter revealed something similar to jet stream winds in the low and middle cloud region, which extends from 45 to 60 kilometres (28 to 37 mi) in altitude.[53] The wind speed maximized near the equator. In September 2017, JAXA scientists named this phenomenon 'Venusian equatorial jet'.[54] They also published results on equatorial winds at the cloud-top level by tracking clouds on the UV spectrum.[55] A significant result in 2018 is the appearance of thick clouds of small particles near the transition between upper and middle clouds, what was described as a "new and puzzling morphology of the complex cloud cover."[51] By 2017, the science team published 3D maps on the Venus atmosphere structure.[51] The physical quantities retrieved include the pressure, the temperature, the H
2SO
4 vapor density, and the ionospheric electron density and their variations.[51] By the year 2019, the first results about the morphology, temporal changes[56] and the winds at the middle clouds of Venus were published and merited the cover in Geophysical Research Letters, reporting unexpectedly high contrasts that might indicate the presence of absorbers like water.[57]

To image lightning, the orbiter has sight of the dark side of Venus for about 30 minutes every 10 days.[58] As of July 2019, it has accumulated 16.8 hours of observations of the night side, and no lightning has been detected.[59]

[edit]
  • An image of Venus with AKATSUKI Ultraviolet Imager (UVI)
    An image of Venus with AKATSUKI Ultraviolet Imager (UVI)
  • An image of Venus with a crescent shaped area that is illuminated by sunlight. The image was taken with UVI.
    An image of Venus with a crescent shaped area that is illuminated by sunlight. The image was taken with UVI.
  • An image of the night side of Venus with the AKATSUKI 2-μm Camera (IR2). In the dark areas the light is absorbed by CO2 clouds.
    An image of the night side of Venus with the AKATSUKI 2-μm Camera (IR2). In the dark areas the light is absorbed by CO2 clouds.
  • An image of the surface of Venus with the AKATSUKI 1-μm Camera (IR1)
    An image of the surface of Venus with the AKATSUKI 1-μm Camera (IR1)

See also

[edit]

References

[edit]
  1. ^ a b c d e f g Takeshi, Oshima; Tokuhito, Sasaki. "Development of the Venus Climate Orbiter PLANET-C (AKATSUKI)" (PDF). NEC Technical Journal. 6 (1): 47–51.
  2. ^ Stephen Clark (20 May 2010). "H-2A Launch Report – Mission Status Center". Spaceflight Now. Archived from the original on 20 May 2010. Retrieved 20 May 2010.
  3. ^ a b c "AKATSUKI:PLANET-C project" (PDF). Retrieved 22 January 2022.
  4. ^ a b c "Japanese probe fires thrusters in second bid to enter Venus orbit". The Japan Times. 7 December 2015. Retrieved 7 December 2015.
  5. ^ a b c Szondy, David. "Akatsuki probe enters orbit around Venus". Retrieved 7 December 2015.
  6. ^ a b c Clark, Stephan. "Japanese probe fires rockets to steer into orbit at Venus". Retrieved 7 December 2015.
  7. ^ Chris Bergin (20 May 2010). "AXA H-IIA carrying Akatsuki and IKAROS launches at second attempt". NASASpaceFlight. Retrieved 19 November 2010.
  8. ^ Limaye, Sanjay. "Live from Sagamihara: Akatsuki Orbit Insertion – Second Try". Retrieved 7 December 2015.
  9. ^ Wenz, John (21 September 2015). "Japan's Long Lost Venus Probe May Boom Back to Life". Popular Mechanics. Retrieved 14 October 2015.
  10. ^ a b c d M. Nakamura; T. Imamura; N. Ishii; T. Abe; T. Satoh; et al. (21 June 2011). "Overview of Venus orbiter, Akatsuki". Earth, Planets and Space. 63 (5): 443–457. Bibcode:2011EP&S...63..443N. doi:10.5047/eps.2011.02.009. ISSN 1880-5981.
  11. ^ a b "Exploring the Venusian Atmosphere – AKATSUKI/PLANET-C". Akatsuki Special Site. Retrieved 5 December 2015.
  12. ^ a b Kenneth Chang (16 January 2017). "Venus Smiled, With a Mysterious Wave Across Its Atmosphere". The New York Times. Retrieved 17 January 2017.
  13. ^ a b T. Fukuhara; M. Futaguchi; G. L. Hashimoto; T. Horinouchi; T. Imamura; et al. (16 January 2017). "Large stationary gravity wave in the atmosphere of Venus". Nature. 10 (2): 85–88. Bibcode:2017NatGe..10...85F. doi:10.1038/ngeo2873.
  14. ^ Jones, Andrew (31 May 2024). "Japan loses contact with Akatsuki, humanity's only active Venus probe". space.com. Retrieved 4 October 2024.
  15. ^ "JAXA | Takeshi Imamura Project Scientist, AKATSUKI "Venus Unveiled: A Planet Beyond Our Imagination"".
  16. ^ Staff writers (8 December 2010). "Japan probe shoots past Venus, may meet again in six years". Spacedaily.com. Retrieved 3 December 2011.
  17. ^ a b c "AKATSUKI orbit control at perihelion". JAXA. 1 November 2011. Archived from the original on 13 May 2012. Retrieved 3 December 2011.
  18. ^ "Mission overview". PLANET-C Team/JAXA. Retrieved 3 December 2011.
  19. ^ "Venus Climate Orbiter "AKATSUKI" (PLANET-C)". JAXA. 5 September 2017. Retrieved 11 April 2023.
  20. ^ "Akatsuki (Venus Climate Orbiter / Planet-C)". The Planetary Society. Archived from the original on 18 March 2012. Retrieved 19 November 2010.
  21. ^ Nakamura, Masato; Imamura, Takeshi; Ueno, Munetaka; et al. (2007). "Planet-C: Venus Climate Orbiter mission of Japan" (PDF). Planetary and Space Science. 55 (12): 1831–1842. Bibcode:2007P&SS...55.1831N. doi:10.1016/j.pss.2007.01.009.
  22. ^ a b Initial products of Akatsuki 1-μm camera Archived 3 June 2018 at the Wayback Machine. Earth, Planets and Space. 2018, vol. 70, nbr. 6. doi:10.1186/s40623-017-0773-5
  23. ^ a b c d "Two cameras on Akatsuki pause observations". JAXA. 3 March 2017. Retrieved 6 May 2017.
  24. ^ a b "Messages From Earth: Send your Message to Venus on Akatsuki". The Planetary Society. 2010. Archived from the original on 7 April 2010. Retrieved 2 April 2010.
  25. ^ "We will deliver your message to the bright star Venus – Akatsuki Message Campaign". JAXA. 10 January 2010. Archived from the original on 25 November 2010. Retrieved 19 November 2010.
  26. ^ "Thank you very much for participating in the AKATSUKI message campaign". JAXA. 10 February 2010. Archived from the original on 19 August 2010. Retrieved 2 April 2010.
  27. ^ "金星へ届け！ 県民が寄せ書き" [Hoping that It Will Reach Venus! Residents of The Prefecture Write Something Together]. Oita Godo Shimbun (in Japanese). 17 May 2010. Archived from the original on 20 May 2010. Retrieved 20 July 2010.
  28. ^ "打ち上げを目前に控えた「あかつき」と「IKAROS」の機体が公開" [The Airframes of "Akatsuki" And "IKAROS" just before Those Launch Are Opened]. Mycom Journal (in Japanese). Mainichi Communications. 12 March 2010. Archived from the original on 14 March 2010. Retrieved 20 July 2010.
  29. ^ a b c "Venus Climate Orbiter "AKATSUKI" (PLANET_C): Topics". JAXA. 1 November 2011. Archived from the original on 5 October 2013. Retrieved 3 December 2011.
  30. ^ "Bad weather postpones Japan rocket launch". phys.org. 18 May 2010. Retrieved 11 April 2023.
  31. ^ "Akatsuki Mission Overview". JAXA. Retrieved 23 January 2022.
  32. ^ "金星探査機「あかつき」の状況について" [About the State of Venus Probe Akatsuki] (PDF) (in Japanese). JAXA. 7 December 2010. Retrieved 8 December 2010.
  33. ^ JAXA's press briefing, 22:00, 7 December 2010 JST
  34. ^ Eric Talmage. "Japan's Venus Probe Fails to Enter Orbit". ABC News. Archived from the original on 13 December 2010. Retrieved 8 December 2010.
  35. ^ "Akatsuki Mission Statement: 20101207". The Planetary Society. Archived from the original on 14 March 2012. Retrieved 8 December 2010.
  36. ^ David Cyranoski (14 December 2010). "Venus Miss is a Setback for Japanese Programme". Nature. 468 (7326): 882. Bibcode:2010Natur.468..882C. doi:10.1038/468882a. PMID 21164456.
  37. ^ a b M. Nakamura; Y. Kawakatsu; C. Hirose; T. Imamura; N. Ishii; et al. (2014). "Return to Venus of the Japanese Venus Climate Orbiter AKATSUKI". Acta Astronautica. 93: 384–389. arXiv:1709.09353. Bibcode:2014AcAau..93..384N. doi:10.1016/j.actaastro.2013.07.027. S2CID 110719337.
  38. ^ "Akatsuki: Importance". University of Colorado. Archived from the original on 1 October 2017. Retrieved 13 June 2017.
  39. ^ "Japanese Venus Probe Misses Orbit". Aviation Week & Space Technology.[permanent dead link‍][permanent dead link‍]
  40. ^ Stephen Clark (7 February 2015). "Japanese craft to get second chance after missing Venus in 2010". Spaceflight Now. Retrieved 26 August 2024.
  41. ^ "「あかつき」の旅 (2013年特別公開向け資料)" [“Akatsuki” Journey (Press Kit in 2013)] (PDF) (Press release) (in Japanese). JAXA. 26 August 2013. Retrieved 8 June 2014.
  42. ^ "AKATSUKI: Orbit successfully controlled". PLANET-C Team/JAXA. 5 August 2015. Retrieved 10 September 2015.
  43. ^ "Venus Climate Orbiter "AKATSUKI" Inserted Into Venus' Orbit". JAXA. 9 December 2015.
  44. ^ Clark, Steven (17 May 2016). "Japanese orbiter officially begins science mission at Venus". Spaceflight Now. Retrieved 26 November 2019.
  45. ^ 「あかつき」定常観測フェーズ終了 (PDF). ISAS News (in Japanese). May 2018. p. 4. ISSN 0285-2861.
  46. ^ Nakamura, Masato (19 November 2019). "あかつきの現状" [Current Status of Akatsuki] (PDF) (in Japanese). ISAS/JAXA. Retrieved 26 November 2019.
  47. ^ T. Satoh; A. Yamazaki; T. Imamura; N. Ishii; M. Nakamura; T. Abe (25 March 2024). "一番星へ行こう！日本の金星探査機の挑戦 その57 〜あかつき運用を再延⻑し，金星大気⻑期変動の要因解明に挑む〜" [Road to the first star: Venus orbiter from Japan (57) - Akatsuki challenges the mechanisms of long-term variations in Venus' atmosphere through another mission extension] (PDF). Planetary People (in Japanese). 33 (1). The Japanese Society for Planetary Sciences. ISSN 0918-273X.
  48. ^ "金星探査機「あかつき」との通信状況について" [Communication status with the Venus Climate Orbiter "AKATSUKI"] (in Japanese). ISAS / JAXA. 29 May 2024. Retrieved 21 July 2024.
  49. ^ Passant Rabie (31 May 2024). "Venus' Only Active Probe Mysteriously Falls Silent". Gizmodo.com. Retrieved 24 August 2024.
  50. ^ Eric Berger (29 May 2024). "Our only mission at Venus may have just gone dark". Ars Technica. Retrieved 24 August 2024.
  51. ^ a b c d M. Nakamura; D. Titov; K. McGouldrick; P. Drossart; J. L. Bertaux; H. Liu (December 2018). "Akatsuki at Venus: The First Year of Scientific Operation". Earth, Planets and Space. 70 (144). doi:10.1186/s40623-018-0916-3.
  52. ^ J. Peralta; Y. J. Lee; K. McGouldrick; H. Sagawa; et al. (2017). "Overview of useful spectral regions for Venus: An update to encourage observations complementary to the Akatsuki mission". Icarus. 288: 235–239. Bibcode:2017Icar..288..235P. doi:10.1016/j.icarus.2017.01.027.
  53. ^ Damia Bouic (16 January 2018). "A new look at Venus with Akatsuki". The Planetary Society. Retrieved 28 January 2018.
  54. ^ "Venus: Jet-setting Atmosphere". JAXA. 5 September 2017. Retrieved 26 September 2017.
  55. ^ T. Horinouchi; T. Kouyama; Y. J. Lee; S. Murakami; K. Ogohara; et al. (15 January 2018). "Mean winds at the cloud top of Venus obtained from two-wavelength UV imaging by Akatsuki". Earth, Planets and Space. 70 (10). Bibcode:2018EP&S...70...10H. doi:10.1186/s40623-017-0775-3.
  56. ^ Larry O. Hanlon (29 April 2019). "New research takes deeper look at Venus's clouds". blogs.agu.org/geospace. American Geophysical Union. Retrieved 23 August 2024.
  57. ^ J. Peralta; N. Iwagami; A. Sánchez-Lavega; Y. J. Lee; R. Hueso; et al. (2019). "Morphology and Dynamics of Venus's Middle Clouds With Akatsuki/IR1". Geophysical Research Letters. 46 (5): 2399–2407. arXiv:1903.02883. Bibcode:2019GeoRL..46.2399P. doi:10.1029/2018GL081670. S2CID 119195952.
  58. ^ Y. Takahashi; M. Sato; M. Imai (23–28 April 2017). Hunt for Optical Lightning Flash in Venus using LAC onboard Akatsuki spacecraft. 19th EGU General Assembly. Vienna, Austria. p. 11381. Bibcode:2017EGUGA..1911381T. EGU2017.
  59. ^ R. D. Lorenz; M. Imai; Y. Takahashi; M. Sato; A. Yamazaki; et al. (3 July 2019). "Constraints on Venus Lightning From Akatsuki's First 3 Years in Orbit". Geophysical Research Letters. 46 (14): 7955–7961. Bibcode:2019GeoRL..46.7955L. doi:10.1029/2019GL083311.
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