nrc planetary science decadal survey
DESCRIPTION
NRC Planetary Science Decadal Survey. Wendy Calvin Prof. Geological Sci & Eng, University of Nevada - Reno Vice-Chair Mars Sub-Panel. for Western Space Grant Directors Meeting DRI, 18.Sept.09. Decadal Surveys. Chartered by NASA, but provided by NRC as advisory arm of the NAS. - PowerPoint PPT PresentationTRANSCRIPT
NRC Planetary Science Decadal Survey
Wendy CalvinProf. Geological Sci & Eng,
University of Nevada - Reno
Vice-Chair Mars Sub-Panel
for Western Space Grant Directors MeetingDRI, 18.Sept.09
Decadal Surveys
Chartered by NASA, but provided by NRC as advisory arm of the NAS.
Independent assessment of scientific priorities in a given area.
Earth Science just completed (2007). Astronomy/Astrophysics and Planetary currently
underway. Identify and Prioritize flight investigations believed
to be > 450$M life cycle cost. Include infrastructure, R&A, education, technology
New Frontiers in the Solar System (2003)
Fundamental Science Questions 1st Billion Years of Solar System History Volatiles and Organics stuff of life Origin and Evolution of Habitable Worlds How Planetary Systems Work
Example Recommended Missions Europa Geophysical Explorer Venus In-Situ Jupiter Polar Orbiter S. Pole Aiken (Lunar) Sample Return Mars Network Mars Sample Return
Planetary Science 2013-2022
Overview of planetary science. Survey the state of knowledge, recent discoveries. Inventory top-level science questions that guide
flight missions. Small (Discovery), Medium (New Frontiers), Large
(Flagship) mission classes. (New) priorities for Mars and Earth’s Moon to be
integrated with the rest of the Solar System. (New) assessment and cost modeling of flight
concepts. (New) Astrobiology included in sub panels rather
than separate sub-panel.
Committee Structure
Steering Committee (Squyres, Soderblom) Vice-Chair of each sub panel (5) 9 others not affiliated with any subpanel
Sub-Panels Primitive Bodies (Asteroids, Comets, KBOs,
Meteorites, IDPs) Inner Planets (Mercury, Venus, Moon) Mars Giant Planets (JSUN, exoplanets, rings, fields) Satellites (Europa, Ganymede, Titan Enceladus,
and many, many others)
http://sites.nationalacademies.org/SSB/CurrentProjects/ssb_052412
Mars Panel
13 Members Represent science from core to atmosphere
Strategic missions and design well-considered through MEPAG community process. Goals and Objectives “Living” Document
Life, Climate, Geology/Geophysics, Human Exploration Plans for 2016, 2018 Missions relatively stable
2016 Trace Gas Orbiter, 2018 – Rover (Astrobio) International collaboration developing
Exo-Mars, Mars Sample Return Just had 1st meeting, briefings from MEPAG
community and mission studies. Community white papers just delivered.
Process/Timeline
Sub panels meet, gather information, propose missions for study. Include “White papers” from community Each sub-panel has 2 meetings between Aug-Nov 2009
Steering committee prioritizes input from sub-panels into cross-solar system themes and goals. Strive for consensus and community ownership Fit within current budget constraints
Draft document from sub panels Spring 2010 Draft full report Fall/Winter 2010 External review and release of final report summer
2011.
2003 Mars Themes / Key Questions
Mars as a potential abode of life Does/Did life exist, how habitable?
Water, atmosphere, and climate Sources, sinks, volatile reservoirs Atm evolution, dynamics, atm escape 3D distribution of water in the crust
Structure and evolution of Mars Rock types, origin of crustal magnetism Internal structure, core dynamo Chronology, oxidation with depth
Why Mars?
1. Mars offers crucial information about the early evolution, internal structure, and origin of the terrestrial planets, including Earth.
2. Timeframe for evolution of life on Earth is largely absent from the rock record, but this era is preserved on Mars.
3. Mars provides a means to approach, and possibly answer, origin and evolution of life questions.
4. Excellent opportunity to investigate short- and long-term climate change.
5. Mars science has benefitted from a focused, dedicated program of exploration.
10
Competitive PI-Led Missions
MER Focused Technology
MRO Focused Technology
MSL Focused Technology
MEP—An Integrated Set of ActivitiesCreating a True Program Structure
Advanced Planning & Community InputResearch and E/PO Programs
Base Technology
2007Mars
Reconnaissance Orbiter
Mars Reconnaissance
Orbiter
2001 2003 2005
Curiosity
1996
Phoenix
2011Mars Global
SurveyorMars Global
Surveyor
OpportunitySpirit
Mars OdysseyMars Odyssey
Mars Pathfinder
Year of Launch2013
MAVENMAVEN
Strategic, Core Missions
Last Decade Discoveries: Diverse Planet with Complex History
Mars has areas with diverse mineralogy, including alteration by water, with a change in mineralogy over time and spatial diversity of environments.
In situ confirmation of increased water activity in the past.Pervasive water ice in globally distributed, near-surface reservoirs.
Sources, phase changes, and transport of volatiles (H2O, CO2) are known & some are quantified.
Increasing evidence for geologically recent climate change.Dynamic change occurring even today: landslides, new gullies, new
impact craters, changing ice cover.Presence of methane indicative of active chemical processes either
biogenic or abiotic. Based on much of the above, the perception of Potential for past Life
has increased, and Modern Life may still be possible.
Last Decade Discoveries: Diversity of Environments
-12
Lyell
Steno
Smith
Gilbert area
PHX
Victoria Crater
MER
Hesperian subsurface water, diagenesis
Chemistry and morphology indicate changing environments throughout geologic history
• Acidic waters at Meridiani• Basic waters at Phoenix landing site• Mineralogy: clays to sulfates to oxides
MRO
Melas Chasma
Large-scale sedimentary structures
MRO
MRO
Delta, showing phyllosilicate layers
Eberswalde Delta
Past Decadal Results: Wide variety of sedimentary deposits
-13
MeridianiMER
Fine-scale sedimentary structures
Depositional processes created a sedimentary record
• Developed in topographically low areas
• Spectacular stratification at multiple scales
• Evidence of persistent standing water, lakes
• Sediments systematically change in character with time
• Multiple facies recognized
-14
Gamma Ray Spectrometer• Global hydrogen
abundance and equivalent H2O
• Ground ice to +/-60° in high abundance
ODY
Global Near-Surface Reservoirs of Water
Past Decadal Results: Distribution of Modern Water
SHARAD and MARSIS• Nearly pure water ice • Distinct layering• No deflection of crust• Ice-cored lobate debris
aprons in mid-latitudes
MRO MEX
Phoenix results PHX
Past Decadal Results: Periodic Climate Change
Volatile-rich, latitude dependent deposits (mantle, glaciers, gullies, viscous flow) coupled to orbitally-forced climate change
Periodicity of layering in the north polar cap deposits as well as sedimentary deposits
• Latitude dependent mantle
Modeled Ice Table Depth [m]
MGS, ODY, MEX MRO
Evidence of an active subsurface?
Biotic?
Abiotic?
courtesy Mark Allen
courtesy Lisa Pratt
NAIDetection of Methane on Mars
Cou
rtes
y M
ike
Mum
ma
NAI, R&A
Past Decadal Results:
Modern Methane
MEX NAI R&A
Sulfates Anhydrous Ferric OxidesClays
Past Decadal Results:
Mars Planetary Evolution
Hydrous Mineralogy Changed Over Time
• Phyllosilicate minerals (smectite clay, chlorite, kaolinite…) formed early
• Evaporates dominated by sulfate formed later with opal/hydrated silica
• Few hydrated mineral deposits since
Evolution of Aqueous, Fluvial and Glacial, Morphology with Time
• Valley networks, lake systems
• Gullies • Viscous flow, glaciers,
latitude dependant mantle
acidicNeutral pH
Questions for the Next DecadeIntegrating the MEPAG science priorities and the programmatic factors,
these specific questions are highest priority for the next decade.
• What is the diversity and nature of aqueous geologic environments? (Goal I, II, III--MSL will contribute)
• What is the detailed mineralogy of the diverse suite of geologic units and what are their absolute ages? (Goal II, III)
• Are reduced carbon compounds preserved and, if so, in what geologic environments? (Goal I--MSL may contribute)
• What is the complement of trace gases in the atmosphere and what are the processes that govern their origin, evolution, and fate? (Goal I, II, III)
• How does the planet interact with the space environment, and how has that affected its evolution? (Goal II—addressed by MAVEN mission)
• What is the record of climate change over the past 10, 100, and 1000 Myrs? (Goal II, III)
• What is the internal structure and activity? (Goal III)