exploring venus limaye iaa
TRANSCRIPT
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IAA Pre Summit Conference,
9 January 2014
Exploring Venus with International Coordinated Missions
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IAA Pre Summit Conference,
9 January 2014
Exploring Venus with International Coordinated Missions Limaye - 3
How did these
environments come
about?
Did life evolve on all
three planets?
Topography from Magellan
about 100 times coarser than
measured for Mars
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Why are the three planetary neighbors sodifferent?
How, why and when did they take different
evolutionary paths? What can these three planets inform us about
exo-planets with atmospheres?
Venus is a key piece of the puzzle.
IAA Pre Summit Conference,
9 January 2014
Exploring Venus with International, Coordinated Missions Limaye - 4
Exploration of the solar system began with Venus,
and much about Venus remains a mystery for lack of
a comprehensive and coordinated effort
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Venus should be the most Earthlike planet we know Formed at about the same time
Similar bulk composition with same size
Comparable solar energy input despite orbit differences
An accessible planet for validating ideas about exo-planets with atmospheres
Early Venus was probably much like early Earth Hot dense atmosphere rich in CO2 and water
Similar initial inventory of volatiles and noble gas isotopes
Liquid water on the surface, so climate was very different
Likely spinning faster
Venus also illustrates an extreme fate of the Earth Run-away greenhouse effect restricted by the deep oceans to lower than Venus
temperatures, but still worrisome. In the far future, the insolation at Earth willbe similar to Venus today. Without the ubiquitous cloud cover, what will theclimate be like?
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Why does Venus spin backwards and so slowly? Did it have a moon? Did the atmosphere slow the forward
spin and make it spin backwards?
How does Venus lose its heat?
Why doesnt Venus have a magnetic field? Did Venus ever have a liquid water ocean? How and
when did Venus lose its water? Did life ever evolve on Venus?
Why does the atmosphere rotate so fast? What absorbs the incident sunlight in the ultraviolet ? Does Venus have active volcanoes?Are any of the terrestrial rocky exo-planets with atmospheres like
Venus?IAA Pre Summit Conference,
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IAA Pre Summit Conference,9 January 2014 Exploring Venus with International Coordinated Missions Limaye et al.-8
NASAVenus Flagship Mission Study (NASA)
Venus Climate Mission (Decadal 2013-2022)
Venus In-Situ Explorer (NF, Decadal Survey)
Discovery and NF Proposals (24 so far, 7 last AO)
Russia
Venera-D Mission (Launch in 2021-2023)
ESA
Venus Express (through 2014)
Cosmic Vision Proposals: EVE balloon
and Envision radar orbiter (2007, 2010)
Also Proposed for L2/L3 Themes
JAXA
Venus Climate Orbiter (Akatsuki, VOI in 2015)
ISRO
??
Venera-Dolgozhivushaya (long-lasting) - the
first Russian project in the post-Soviet era to
explore Venus (2003-2013)
NASA Venus Flagship
Mission Study (2008)
Proposed to ESA L2/L3
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IAA Pre Summit Conference,9 January 2014 Exploring Venus with International Coordinated Missions Limaye et al. - 9
ESA Balloon Mission Study
VESPER Orbiter
Discovery Proposal
SAGE New
Frontiers Proposal
VESAT
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OrbiterBalloons (54
and 70 km)Landers (2)
4 years 1 Month1-1.5 h (Entry)
and 5 h (Surface)
Instruments Entry Surface
InSAR ASI ASI Microscopic Imager
Vis-NIR Imaging GC-MS
Vis-NIR Cameras,
SpotSpectrometer
XRD/XRF
Neutral Ion Mass
SpectrometerNephelometer GC-MS Heat Flux Plate
Sub-mm
Spectrometer
Vis-NIR
CameraMagnetometer
Passive Gamma Ray
Detector
Magnetometer Magnetometer Net FluxRadiometer
Sample Acquisition,
Xfer andPreparation System
Langmuir Probe Radio Science Nephelometer Drill to ~ 10 cm
Radio Science
(USO)
Microwave Corner
Reflector
Launch 2020 - 2025
Technology
Readiness LevelTRL 6 by 2015
Mission Cost $3-4 B (FY08)
Launch Vehicle Delta IVH Equivalent
DSN 34 m Ka Band stations
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Launch Vehicle Atlas V-551 (w/ 5 m diameter fairing)
Mass (CBE + Cont.) 5306 kg (wet); 2275 kg (dry)
Payload mass (CBE + Cont.) 290.4 kg
Design Dual string design
Power 32 m2 solar panels (9868 W EOL)
Attitude Control 3 axis stabilized
Telecom4 m Ka/X-band (Orbiter-to-Earth to 34-m DSNantennas); 0.5m S-band (Orbiter-to-in situ); 2.5m
S-band (Orbiter-to-in situ);
Functions
Relay telecom support for in situ elements (30
days); 6 months of aerobraking to science orbit;Science orbiter (2 years baseline & 2 years
extended)
Science data return~300 Tbits of data to Earth over 2 years of
science ops.
Venus Design Reference Mission Orbiter
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Proposed to ESA
Cosmic Vision
L2/L3
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Proposed to ESA
Cosmic Vision L2/L3
S
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Exploring Venus with International Coordinated Missions Limaye et al. - 15
Proposed to ESA
Cosmic Vision L2/L3
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International Collaboration: Recent Developments COSPAR International Venus Exploration Working
Group (IVEWG) formed at the 2012 General
Assembly to foster dialog
Proximity of Venus and short journey makes Venus agood exploration target for a collaborative and
coordinated independent effort by the international
agencies
Concurrent and overlapping missions can increase the
science value returned by deploying coordinated
missions Deployment of innovative technologies and sharing of
ground resources is crucial through international
agreements
Exploring Venus with International Coordinated Missions
Low Level Balloon UAV at cloud tops
SAR or InSAR from orbit
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Exploring Venus: An International Effort
The international Venus community is united regarding the key
science goals and has come together through past and continuing
collaborations:
VeGa Balloon Mission (US and USSR)
Magellan and Venera 15/16
Venus International Reference Atmosphere
Venus Express Mission (ESA/NASA)
Akatsuki (JAXA/NASA/ESA)
Venera-D (IKI/Roscosmos and NASA)
International Space Science Institute International Teams for Models
of Venus Atmosphere
COSPAR International Venus Exploration Working Group (IVEWG)
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Coordinated Effort with Collaborations under the
constrained budgets will be successful through:
Independent and coordinated effort with
international participation throughexchange of mission elements,
instruments and scientists
Planning, Coordination and sharing of
data
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Thank you!