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Title: Mars Aeronomy Science Themes and the NASA Exploration Initiative Report from the NASA Mars Aeronomy


1
Mars Aeronomy Science Themes and the NASA
Exploration InitiativeReport from the NASA Mars
Aeronomy Working Group
  • Bruce Jakosky (Chair)
  • (bruce.jakosky_at_lasp.colorado.edu)
  • 17 September 2004

2
Overview Mars Upper Atmosphere, Mars Science,
and the Exploration Initiative
  • Determining the history of the Martian climate,
    the chemical weathering and alteration of the
    surface, and the planets habitability requires
    understanding the roles of the solar wind and
    solar radiation inputs the physics, chemistry,
    and dynamics of the upper atmosphere and the
    escape of volatiles to space.
  • The upper atmosphere plays important roles in
    programmatic aspects of the Mars exploration
    program, including communications, energetic
    particle and radiation environments that can
    affect humans, the lifetimes of orbiting
    spacecraft, operational aspects of orbital
    missions, and aerobraking operations.
  • Some limited observations of the upper atmosphere
    are being made at present, and the Mars
    Telecommunications Orbiter has the potential to
    make further contributions, but the desired
    understanding can best be obtained from a
    dedicated upper-atmosphere mission.

3
Mars Aeronomy Working Group
  • Chartered by NASA to explore science and
    programmatic issues related to the Mars upper
    atmosphere in light of recent discoveries and the
    new exploration program.
  • Combined effort of (then) Solar System
    Exploration Division and Sun-Earth Connection
    Division (both now part of the Science Mission
    Directorate).
  • Activity requested by the Directors of the two
    divisions.
  • Working group created to lead discussion,
    organize and run a workshop that would bring
    together the aeronomy community, the
    exploration initiative connections, and the rest
    of the Mars science community, and create a
    white paper reporting back on the results.
    Workshop had nearly 90 participants.
  • Discussions of NASA Code S personnel with working
    group chair on 13 May 04, workshop held on 18-19
    August 04, draft powerpoint report circulated
    within working group and then distributed to
    community for comments, and finalized on 17
    September 04.

4
Mars Aeronomy Working Group (Steering Group)
Membership
  • Bruce Jakosky, Univ. of Colorado (chair)
  • Stephen Bougher, Univ. of Michigan
  • Randy Gladstone, Southwest Research Inst.
  • Joe Grebowsky, NASA/GSFC
  • Rod Heelis, Univ. of Texas at Dallas
  • Jennifer Trosper, NASA HQ
  • Andrew Yau, Univ. of Calgary
  • Richard Zurek, NASA/JPL
  • Key NASA HQ participation
  • Mary Mellott, SEC
  • Denis Bogan, SSED
  • Bill Peterson, SEC

5
Key Components of Working Group Charter
  • Reexamine the upper-atmosphere science questions
    and determine whether and how they should be
    revised in response to the new vision.
  • Understand which operational requirements of the
    Exploration Systems Division involve this region
    and what further understanding is required.
  • Summarize the opportunities available for support
    of the study of this region, including those
    associated with the upcoming Mars Scout and Mars
    Telecommunications Orbiter opportunities.

6
MARS AERONOMY EXPLORATION WORKSHOP AGENDA, 18-19
August 2004 (Agenda and powerpoint presentations
available on web, at http//argyre.colorado.edu/l
ife/aeronomy_workshop) Wednesday, August
18 800-830 Coffee 830-845 Workshop
introduction B. Jakosky 845-855 NASA HQ
perspective, SEC division M. Mellott 855-905 NA
SA HQ perspective, SSE division D.
Bogan 905-925 Mars program and NASA HQ D.
McCuistion 925-955 Status of the Mars
Program M. Meyer 955-1020 Code T requirements
and interest J. Trosper 1020-1035 Break 1035-
1050 Mars Telecommunications Orbiter R.
Zurek 1050-1105 Mars Scout opportunities K.
McBride 1105-1130 MEPAG Goals and Objectives
for upper atmosphere S. Bougher 1130-1145 Lesson
s learned from MGS and Odyssey aerobraking S.
Bougher 1145-1200 Lessons learned at
Venus A. Nagy 1200-1215 MGS Magnetometer
results D. Mitchell 1215-130 Lunch All 1
30-145 Lessons learned at Earth from Earth
missions S. Yee 145-200 Preliminary results
from Mars Express ASPERA J. Sharber
7
Wednesday, August 18, continued 200-515 Discus
sion on these topics - Are the aeronomy
science goals and objectives balanced, complete
, appropriate, etc.? (S. Bougher) - How
do they relate to the rest of the Mars
program? (R. Gladstone) - Can MTO
contribute to aeronomy science goals? (R.
Zurek) - What measurements/analyses are
required prior to human missions? Can they be
obtained via a science-oriented Scout or do
they require a dedicated mission? (J.
Trosper) 515-545 Integration and wrap-up B.
Jakosky
8
Thursday, August 19 800-830 Coffee 830-1200 C
ontinue discussion from before, with these added
topics - What actions/resources from HQ are
required to further develop these topics? -
What are the recommendations from the group as a
whole? - Wrap-up of open workshop 1200-115 L
unch 115-500 Closed session of steering group
to draft report 500 Adjourn
9
Long-Recognized Need for Upper-Atmosphere
Measurements
  • In-depth study of Mars upper atmosphere
    consistently has been judged necessary to
    understand the evolution of Mars and other
    planets.
  • Upper-atmosphere missions have been the subject
    of several advance mission studies and was a
    defining element of the ill-fated Japanese Nozomi
    mission.
  • COMPLEX (National Research Council Committee on
    Planetary and Lunar Exploration) has consistently
    given an aeronomy mission high value within
    planetary science.
  • NRC Decadal Survey (New Frontiers in the Solar
    System An Integrated Exploration Strategy,
    2003) includes Mars upper atmosphere studies as
    an important component of an overall program.
  • MEPAG (Mars Exploration Program Activity Group)
    2004 prioritized ranking of science goals and
    objectives gives high priority to
    upper-atmosphere studies as they pertain to
    evolution and control of planetary habitability.

10
Ongoing and Planned Measurements From Orbit
Relevant to the Upper Atmosphere
  • Mars Global Surveyor (MGS) Magnetometer/Electron
    Reflectometer (MAG/ER) measurements (ongoing)
  • MGS radio occultation (ongoing)
  • Mars Express ASPERA (neutral particle imaging,
    neutral particle detection, electron
    spectrometer, ion mass analyzer ongoing)
  • Mars Express SPICAM (atmospheric occultation
    ongoing)
  • Mars Express MARSIS (long-wavelength radar
    antenna not yet deployed)
  • Mars Reconnaissance Orbiter (MRO) aerobraking
    data
  • MRO radio occultations
  • Requires resoliciting the Radio Science
    investigation or implementing a funded
    Participating Scientist program in a timely
    manner.
  • While these will provide valuable science and
    operations data, they will not, taken together,
    provide the understanding of the upper atmosphere
    structure, composition, dynamics, and variability
    necessary to address the pertinent science
    questions.

11
Relevant Areas for Additional Study Other than
from Spacecraft
  • There is a need for new chemical rate
    coefficients and cross-section data existing
    data are old, out of date, and inconsistent.
  • Some science issues can be addressed very
    effectively using telescopic observations from
    Earth these are complementary to spacecraft
    measurements. Ongoing and recent analyses
    include observations from HST, FUSE, and IRTF, as
    examples.
  • Studying stellar winds and UV output in Sun-like
    stars at various ages will help us infer the
    history of martian interactions with the Sun, and
    thereby its climate history and volatile
    evolution.

12
Key Areas Identified and Discussed
  • How do the Mars upper-atmosphere and aeronomy
    issues relate to the rest of the Mars science
    program?
  • Are the current aeronomy science goals and
    objectives balanced, complete, appropriate, etc.?
  • How can the Mars Telecommunications Orbiter
    contribute to aeronomy science goals?
  • What measurements/analyses are required prior to
    human missions? Can they be obtained via a Scout
    mission designed to address science goals or do
    they require a dedicated mission or missions?

13
Scientific Connections Between Studies of the
Upper Atmosphere and the Rest of the Mars Program
(1 of 2)
  • Mars as an integrated system The martian
    volatile, climate, and habitability system is
    an integrated one, from below the surface to
    above the exobase. Atmospheric dynamics,
    surface-atmosphere volatile exchange, and the
    climate cannot be understood without determining
    the role of the upper atmosphere.
  • Loss of martian water and volatiles The history
    of the martian atmosphere and climate over time
    cannot properly be understood without knowing the
    role of loss of water and other volatiles to
    space. These will affect our general
    understanding of the nature of planetary
    habitability in general and habitability of Mars
    in particular.
  • Evolution of surface and atmospheric chemistry
    Formation of surface weathering deposits (such as
    the sulfates at the Mars Exploration Rover (MER)
    Opportunity site, or carbonates there and
    elsewhere) depends on atmospheric composition and
    oxidation state interpretation of chemical and
    isotopic composition requires understanding
    atmospheric effects.

14
Scientific Connections Between Studies of the
Upper Atmosphere and the Rest of the Mars Program
(2 of 2)
  • Follow the dust theme The lower and upper
    atmosphere are tightly coupled. Atmospheric
    structure and change in the escape over time of
    volatiles to space may result from lower-upper
    atmosphere connections, electrodynamic response,
    and dust event heating in the lower atmosphere
    potential importance for exploration missions
    (see below).
  • Interpreting magnetic fields Crustal magnetic
    field measurements are used to improve our
    understanding of the evolution of Mars' interior
    and crust. Crustal magnetic fields and
    variations in external forcing all affect upper
    atmospheric processes, with plasma-neutral
    coupling a key player, and upper-atmospheric
    properties thereby affect our ability to measure
    and understand magnetic fields.
  • Comparative planetology By examining the same
    processes in the different environments of the
    three terrestrial planets, we can better
    understand how they work and better apply them to
    understanding planetary evolution.

15
Influence on the atmosphere and climate via the
role of escape to space shown here.
16
Connections between loss of volatiles to space
and other components of the Mars
climate/surface/interior system (Arrows show
which components of the system directly affect
other components)
17
Are the Aeronomy Science Goals and Objectives
Balanced, Complete, Appropriate, etc.? (1 of 2)
  • The recent Mars Exploration Program Analysis
    Group (MEPAG) Science Goals and Objectives
    document describes the areas that should be
    addressed by upcoming missions. Following
    discussion, the workshop participants concluded
    that
  • The specific MEPAG goals and objectives
    articulated in the document
  • Address key, high-priority issues in aeronomical
    science
  • Can frequently only be achieved by making
    measurements which are traditionally viewed as
    aeronomical in nature
  • The MEPAG investigations listed under the
    objectives should
  • Note that several required aeronomical
    measurements can be made with Earth-based
    observations ( e.g., from earth-orbiting or
    ground-based platforms) and/or in situ
    measurements
  • Consider the potential role of atmospheric
    electrical properties
  • The MEPAG listed investigations should strengthen
    emphasis on
  • Dust impact on the entire atmosphere (including
    aerosol charging)
  • Plasma-neutral coupling
  • External drivers at the top of the atmosphere
    (e.g., solar radiation and particle effects)
  • Implications of the crustal magnetic fields and
    their interaction with upper atmospheric
    processes over time

18
Are the Aeronomy Science Goals and Objectives
Balanced, Complete, Appropriate, etc.? (2 of 2)
  • What role do upper-atmosphere missions play in
    the Pathways architecture?
  • Concern was expressed over how an
    upper-atmosphere mission fits within the
    Pathways concept described in Mars Exploration
    Strategy, 2009-2020, published in 2003 by the
    Mars Science Program Synthesis Group
  • An aeronomy mission was called out in only one of
    the four pathways (never any water, in which it
    was a forced fit), and recent science results
    from MER appear to have rendered that pathway
    moot.
  • All need to be reminded that the pathways were
    examples to show the diversity of potential
    missions and mission architectures and the
    ability of the science program to respond to new
    discoveries. It was not a menu of four options.
  • Aeronomy/upper-atmosphere studies address key
    science objectives for Mars, ensuring that a
    mission in this area is credible and appropriate
    within any actual architecture.

19
How Can the Mars Telecommunications Orbiter (MTO)
Contribute to Aeronomy Science Goals? (1 of 2)
  • The theme recommended by the MTO Science
    Definition Team, of Mars environmental
    monitoring is supported.
  • It appropriately takes advantage of the expected
    long lifetime of MTO, potentially to observe the
    behavior of components of the upper atmosphere
    over a full 11-yr. solar cycle.
  • It could provide the solar cycle context in
    which a shorter-lived upper-atmosphere mission
    could provide the detailed coverage of physical
    and chemical processes related to volatile
    evolution and therefore climate change.
  • Example candidate instruments for long-term
    monitoring include
  • Radiation fields, including Solar Energetic
    Particles (SEPs) and Solar UV irradiance
  • Atmospheric emissions from which composition can
    be inferred
  • Solar-wind interactions at the 4000-km MTO
    orbital altitude
  • Atmospheric dust and temperature structure to
    high altitudes
  • Ionosphere electron density profiles.

20
How Can the Mars Telecommunications Orbiter (MTO)
Contribute to Aeronomy Science Goals? (2 of 2)
  • Notes with regard to MTO
  • MTO radiation measurements would enhance similar
    and contemporaneous measurements on the Mars
    surface.
  • Spacecraft-to-spacecraft radio occultations would
    broaden coverage of atmospheric neutral and
    ionospheric structure beyond that attainable by
    MTO alone.
  • Magnetic field measurements can significantly
    enhance interpretation of the SEP and pick-up-ion
    distribution measurements that would address the
    proposed Mars space environment monitoring.
  • The measurements obtainable within the
    constraints imposed by MTO (instrument mass,
    power, available funding, viewing geometry, s/c
    orbit, etc.) are such that no plausible
    instrument selection would allow us to check the
    box that MTO has made the aeronomy measurements
    necessary to understand key volatile escape
    processes and their current rates.

21
Human Exploration Program Considerations(1 of 2)
  • Upper-atmosphere studies have the potential to
    play important roles in the following areas
  • Understanding the human-related radiation
    environment and the relationship between the
    radiation incident on the upper-atmosphere and
    the surface radiation hazard.
  • The role of the ionosphere in communications
    links.
  • Lifetime of orbital instruments and platforms and
    related planetary protection concerns, and
    operational aspects of orbital missions at
    moderate altitudes that still feel the effects of
    the upper atmosphere (such as reaction wheel
    desaturation operations).
  • Aerobraking operations and hazards associated
    with upper-atmosphere structure and variability
    including dust influence, variability, and
    evolution.

22
Human Exploration Program Considerations(2 of 2)
  • Understanding the influence of the upper
    atmosphere in these areas requires knowledge
    (observation and modeling) of the
  • Diurnal variability
  • Seasonal variability
  • Solar-cycle variability
  • Spatial (geographical) variability
  • Altitude variability (including effects from the
    lower atmosphere)
  • It is necessary to establish measurement
    requirements in terms of a well-defined risk and
    mitigation strategy (i.e., whether the system can
    handle the potential variations vs. simultaneous
    observations to allow optimization and control).
  • Upper-atmosphere studies do support aerobraking
    of robotic missions, but may not be needed for
    aerocapture due to the low altitude of primary
    deceleration (30-50 km) expected for human
    missions.

23
Ongoing Participation and Responsibility of the
Aeronomy Community
  • Making the scientific connections between the
    Mars upper atmosphere and the broad Mars science
    goals via a science traceability matrix is the
    responsibility of any proposer for instruments or
    missions.
  • Mars Express results are relevant to the upper
    atmosphere and to evolution processes, and need
    to be incorporated into any discussion of science
    results and proposals for future instruments or
    missions.
  • Generally, the Mars aeronomy/upper-atmosphere
    community has not been heavily engaged in MEPAG
    activities, and as a result the potential
    contributions of aeronomical science to achieving
    high-priority Mars science goals and objectives
    have not been incorporated as thoroughly as they
    could be.
  • The discussion represented by this workshop and
    white paper needs to be the first of an ongoing
    dialog and integration of the community, not a
    one-time activity.

24
Summary Recommendations and Conclusions
  • The upper atmosphere is an important part of the
    martian climate system. Understanding the
    behavior of the key components of the system
    (such as surface habitability or geochemical
    evolution) will require understanding the entire
    system from the interior to the exobase.
  • Important aspects of the upper-atmosphere can be
    observed from the unique perspective of MTO,
    especially with observations potentially made
    over an entire solar cycle.
  • Although some notable observations of the upper
    atmosphere are being made at present, they are
    limited in scope and coverage and do not provide
    the detailed information necessary to address the
    major science and programmatic issues.
  • The necessary observations can be made from a
    dedicated s/c mission with appropriate orbit,
    lifetime, and instrumentation. The necessary
    observations are thought to be possible within
    the constraints of a Scout mission, although
    detailed analysis of this opportunity has not
    been done.
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