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Exploring Mars: Past, Present,
and Future Robotic Missions
Bruce Jakosky
LASP / University of Colorado
The Public’s Fascination With Mars
Overarching Question: Did Mars
Ever Have Life?
Mars appears to meet or have met all of the environmental requirements for the
occurrence of life:
• Liquid water
• Access to the biogenic elements
• Source of energy to drive metabolism
Did Mars ever have life?
If it does, is it related to life on Earth?
How did any life interact with its planetary environment?
How has the habitability of Mars changed over time?
4
MRO
Odyssey
2001 - 2014Operational 2016 2018 2020
Curiosity –
Mars Science
Laboratory
2022
ESA ExoMars
Rover (MOMA)
2020
Mars Rover
4
Future
Planning
Opportunity
ESA Trace Gas
Orbiter
(Electra)
InSIGHT
(Discovery Program)
Mars Express
Collaboration
Explore Habitability
Follow the Water
EVOLVING MARS SCIENCE THEMES
Seek Signs of Life
Prepare for Future Human Explorers
MAVEN
ISRO – MOM
Mangalyaan
Minerals in Watersheds Around Gale Crater
 Mission/instrument:
MRO/CRISM
 Finding: Gale and
surrounding craters host
similar bedrock mineralogy
and altered clay deposits on
their floors, but vary in
evaporate salt content.
 Importance: Fluvial
processes emplaced detrital
clay minerals. As Mars dried
out, the three craters
became hydrologically
isolated and salts were left
behind nonuniformly.
Curiosity will explore this
geologic history.Reference: Ehlmann, B. L., and Buz,
J. (2014) Mineralogy and Fluvial
History of the Watersheds of Gale,
Knobel, and Sharp craters: Context
for MSL Curiosity’s Exploration,
Geophs. Res. Lett.,
DOI: 10.1002/2014GL062553.
4/2/2015
Summit Cape Tribulation
Pancam Sol 3902 Looking South to Marathon Valley
Evidence for Surface Water on Ancient Mars
Where Did the Water Go? Where Did the CO2 Go?
Volatiles can go
into the crust
Volatiles can be lost to space
Carbonate deposits in a Martian meteorite
Abundant evidence for ancient water
Escaping ions detected from Mars
Express
MAVEN Will Allow Us to Understand Escape of Atmospheric
Gases to Space
• Measure energetic drivers from the Sun, response of upper atmosphere and ionosphere,
and resulting escape to space
• Understand the key processes involved, allowing extrapolation over Mars history
Launched on
18 Nov. 2013,
first day of its 20-
day launch period
Ten-month cruise to Mars;
Orbit insertion took place on
21 Sept. 2014
One Year of Science Operations
MAVEN Mission
Orbit shown to scale
Spacecraft Designed For This Mission
Close Encounter With Comet Siding Spring
• MAVEN IUVS imaged CSS in scattered solar
Lyman-alpha two days before closest
approach to Mars
• H detected to distance of ~150,000 km
(comparable to Mars miss distance of comet)
• Suggested significant potential risk to
spacecraft
• Comet Siding Spring had close
approach (~140,000 km) to Mars on
19 Oct. 2014
• Spacecraft took protective measures
to ensure safety
• Strong desire to observe comet and
its effects on Mars’ atmosphere
Breckland Skies Observatory
Detection of Metal-Ion Layer Following
Encounter With Comet Siding Spring
• Cometary dust entering Mars’ atmosphere
is vaporized and ionized
• IUVS saw very bright UV emissions due to
metal ions (left)
• Emission observed at tangent altitude of
~120-150km
Blue = before CSS
Red = after
• NGIMS detected 11 different metal ions
(right); detected in situ as low as periapsis
altitude of ~185 km
• Metals not detected prior to CSS encounter
• Ions lasted hours to days, consistent with
model predictions
• No previous detection of metal-ion layer at
Mars; electron layers had been detected
IUVS Observations of Atomic Components of H2O
and CO2 on Their Way to Escaping
Pre-Escape Energization in Polar Plume (1 of 4)
O2+
O+
He+
H2+
H+
Z = 250 km
Pre-Escape Energization in Polar Plume (2 of 4)
O2+
O+
He+
H2+
H+
Z = 300 km
Pre-Escape Energization in Polar Plume (3 of 4)
O2+
O+
He+
H2+
H+
Z = 400 km
Pre-Escape Energization in Polar Plume (4 of 4)
O2+
O+
He+
H2+
H+
Z = 500 km
Coming Next:
4
MRO
Odyssey
2001 - 2014Operational 2016 2018 2020
Curiosity –
Mars Science
Laboratory
2022
ESA ExoMars
Rover (MOMA)
2020
Mars Rover
4
Future
Planning
Opportunity
ESA Trace Gas
Orbiter
(Electra)
InSIGHT
(Discovery Program)
Mars Express
Collaboration
Explore Habitability
Follow the Water
EVOLVING MARS SCIENCE THEMES
Seek Signs of Life
Prepare for Future Human Explorers
MAVEN
ISRO – MOM
Mangalyaan

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Goddard 2015: Bruce Jakosky, University of Colorado

  • 1. Exploring Mars: Past, Present, and Future Robotic Missions Bruce Jakosky LASP / University of Colorado
  • 3. Overarching Question: Did Mars Ever Have Life? Mars appears to meet or have met all of the environmental requirements for the occurrence of life: • Liquid water • Access to the biogenic elements • Source of energy to drive metabolism Did Mars ever have life? If it does, is it related to life on Earth? How did any life interact with its planetary environment? How has the habitability of Mars changed over time?
  • 4. 4 MRO Odyssey 2001 - 2014Operational 2016 2018 2020 Curiosity – Mars Science Laboratory 2022 ESA ExoMars Rover (MOMA) 2020 Mars Rover 4 Future Planning Opportunity ESA Trace Gas Orbiter (Electra) InSIGHT (Discovery Program) Mars Express Collaboration Explore Habitability Follow the Water EVOLVING MARS SCIENCE THEMES Seek Signs of Life Prepare for Future Human Explorers MAVEN ISRO – MOM Mangalyaan
  • 5. Minerals in Watersheds Around Gale Crater  Mission/instrument: MRO/CRISM  Finding: Gale and surrounding craters host similar bedrock mineralogy and altered clay deposits on their floors, but vary in evaporate salt content.  Importance: Fluvial processes emplaced detrital clay minerals. As Mars dried out, the three craters became hydrologically isolated and salts were left behind nonuniformly. Curiosity will explore this geologic history.Reference: Ehlmann, B. L., and Buz, J. (2014) Mineralogy and Fluvial History of the Watersheds of Gale, Knobel, and Sharp craters: Context for MSL Curiosity’s Exploration, Geophs. Res. Lett., DOI: 10.1002/2014GL062553.
  • 6. 4/2/2015 Summit Cape Tribulation Pancam Sol 3902 Looking South to Marathon Valley
  • 7.
  • 8. Evidence for Surface Water on Ancient Mars Where Did the Water Go? Where Did the CO2 Go? Volatiles can go into the crust Volatiles can be lost to space Carbonate deposits in a Martian meteorite Abundant evidence for ancient water Escaping ions detected from Mars Express
  • 9. MAVEN Will Allow Us to Understand Escape of Atmospheric Gases to Space • Measure energetic drivers from the Sun, response of upper atmosphere and ionosphere, and resulting escape to space • Understand the key processes involved, allowing extrapolation over Mars history
  • 10. Launched on 18 Nov. 2013, first day of its 20- day launch period Ten-month cruise to Mars; Orbit insertion took place on 21 Sept. 2014 One Year of Science Operations MAVEN Mission Orbit shown to scale Spacecraft Designed For This Mission
  • 11. Close Encounter With Comet Siding Spring • MAVEN IUVS imaged CSS in scattered solar Lyman-alpha two days before closest approach to Mars • H detected to distance of ~150,000 km (comparable to Mars miss distance of comet) • Suggested significant potential risk to spacecraft • Comet Siding Spring had close approach (~140,000 km) to Mars on 19 Oct. 2014 • Spacecraft took protective measures to ensure safety • Strong desire to observe comet and its effects on Mars’ atmosphere Breckland Skies Observatory
  • 12. Detection of Metal-Ion Layer Following Encounter With Comet Siding Spring • Cometary dust entering Mars’ atmosphere is vaporized and ionized • IUVS saw very bright UV emissions due to metal ions (left) • Emission observed at tangent altitude of ~120-150km Blue = before CSS Red = after • NGIMS detected 11 different metal ions (right); detected in situ as low as periapsis altitude of ~185 km • Metals not detected prior to CSS encounter • Ions lasted hours to days, consistent with model predictions • No previous detection of metal-ion layer at Mars; electron layers had been detected
  • 13. IUVS Observations of Atomic Components of H2O and CO2 on Their Way to Escaping
  • 14. Pre-Escape Energization in Polar Plume (1 of 4) O2+ O+ He+ H2+ H+ Z = 250 km
  • 15. Pre-Escape Energization in Polar Plume (2 of 4) O2+ O+ He+ H2+ H+ Z = 300 km
  • 16. Pre-Escape Energization in Polar Plume (3 of 4) O2+ O+ He+ H2+ H+ Z = 400 km
  • 17. Pre-Escape Energization in Polar Plume (4 of 4) O2+ O+ He+ H2+ H+ Z = 500 km
  • 19. 4 MRO Odyssey 2001 - 2014Operational 2016 2018 2020 Curiosity – Mars Science Laboratory 2022 ESA ExoMars Rover (MOMA) 2020 Mars Rover 4 Future Planning Opportunity ESA Trace Gas Orbiter (Electra) InSIGHT (Discovery Program) Mars Express Collaboration Explore Habitability Follow the Water EVOLVING MARS SCIENCE THEMES Seek Signs of Life Prepare for Future Human Explorers MAVEN ISRO – MOM Mangalyaan