Water on Mars
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Transcript of Water on Mars
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Water on Mars
1. Large floods from groundwater origin?
2. Do impacts affect hydrology?
3. Hydrological effects of cooling of the interior?
4. Were there large oceans?
Michael Manga, UC Berkeley
NASA/JPL/Malin Space Science Systems
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Why study water on Mars?
• Climate and habitability (Mars and Earth
were not so different once...)
• Human exploration
• Water and life
• Testing terrestrial science
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Water on present-day Mars
1. Atmosphere– But not much! (precipitable m)
2. Polar Caps
3. Mantle
4. Regolith
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Water on present-day Mars
1. Atmosphere
2. Polar Caps– N cap equivalent to 9m
global ocean
– S cap has CO2 frost cover
(water beneath)
3. Mantle
4. Regolith
NASA/JPL/MSSS
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Water on present-day Mars
1. Atmosphere
2. Polar Caps
3. Mantle (?)– Meteorites contain
hydrous minerals, but these may have formed at the surface
4. Regolith
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Water on present-day Mars
1. Atmosphere
2. Polar Caps
3. Mantle
4. Regolith– Mars Odyssey
mission: abundant ground ice at high southern latitudes NASA/JPL/U. Arizona
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Water-ice lakes
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Water on early Mars
“Valley networks”– Dendritic networks
suggest erosion by surface runoff
– On Noachian-age crust
Viking image of Warrego Valles
50 km
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Water on early Mars
“Valley networks”– Evidence for
sustained flow: Fans, meander bends, scroll bars
NASA/JPL/MSSS
Moore et al., GRL 2003; Malin & Edgett, Science 2003
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Mars Exploration Rovers (MER)
• Outcrop-scale evidence of water-rich environment in Meridiani Planum (Opportunity)
NASA/JPL/Cornell
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Water on early Mars
“Outflow channels”– Large channels originate at
point source
– Q ~100 to 10000 x Mississippi R. (> 106 m3 s-1)
– Spatial association with collapsed terrain suggests subsurface fluid source
– Total Vol ~ 107 km3 (where did it go?)
50 km
150 km
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Global hydrogeology,aquifers on Mars?
• North-south gradient in elevation• Lots of craters
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Global hydrogeology,aquifers on Mars?
• North-south gradient in elevation• Lots of craters
Clif
ford
and
Par
ker
(200
1)
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Water on Mars
1. Large floods from groundwater origin?
2. Do impacts affect hydrology?
3. Hydrological effects of cooling of the interior?
4. Were there large oceans?
Michael Manga, UC Berkeley
NASA/JPL/Malin Space Science Systems
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1. Recent (<10 Ma) floods at Cerberus Fossae
Did these floods have a groundwater origin?
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1. Recent (<10 Ma) floods at Cerberus Fossae
Did these floods have a groundwater origin?
Murray et al., Science (2005)
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Model
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Can subsurface aquifers deliver enough water, and deliver it fast enough to make the features we see?
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Can subsurface aquifers deliver enough water, and deliver it fast enough to make the features we see?
YES
A groundwater source in a large deep aquifer is plausible if k is large enough
Is k ~ 10-9 m2 reasonable?
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Permeability of basalt aquifers: The High Cascades
Cultus River
Quinn River
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Useful features
• Nearly constant discharge• Peak discharges lags recharge by 1-6 months
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Flow governed by
Response characterized by diffusion time
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Conclusion:
A groundwater source in a large deep aquifer is plausible if k is large enough
Is k ~ 10-9 m2 reasonable?
Yes, if aquifers are made of basaltic lava flows, not too much weathering
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Compared with Earth, slow hydrological cycling
Geological processes that are • infrequent• slow may be hydrological important
Two examples
• Impacts• Secular cooling of the planet
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Shaking from earthquakes • changes pore pressure• increases streamflow• causes liquefaction
2. Impacts and groundwater
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Shaking from earthquakes • changes pore pressure• increases streamflow• causes liquefaction
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Shaking from earthquakes • changes pore pressure• increases streamflow• causes liquefaction
Connection to earthquakes? Impacts also shake the ground
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Distance over which liquefaction occurs, streamflow increases
Empirical upper bound
Wan
g, M
anga
, W
ong,
Ica
rus
(200
5)
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Scaling of impact shaking to earthquakes
Size-energy scaling (Melosh, 1978)
Seismic efficiency
Maximum distance for liquefaction
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Scaling consistent with observations?
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Origin of “chaotic terrain”?
lateralspreading?
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3. Slow processes may be important on Mars:As planet cools, cryosphere gets thicker
Implications for groundwater?
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Water pressure increases
Discharge continues until pressure is hydrostatic
Cooling
Cryosphere thickens
Water erupts when pressure becomes lithostatic
A small number (of large) floods may be possible,
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4. Paleoshorelines on Mars?
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4. Paleoshorelines on Mars?
Carr & Head, JGR 2003
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Webb, JGR 2004
Paleoshorelines on Mars?
~300 kmBonneville paleoshoreline, Utah www.geo.cornell.edu
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Raw elevations from Carr & Head [2003]
Problem: Shorelines don’t follow an equipotential surface [Head et al., 1999; Carr & Head, 2003]
Interpolation artifacts
[Carr & Head, 2003; Webb, 2004]
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Long-wavelength lithospheric deformation
• Loading by H2O (Leverington and Ghent)
• Flexural response to large surface loads
• Dynamic topography (mantle convection)
• True polar wander (TPW)
QuickTime™ and aTIFF (Uncompressed) decompressor
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TPW + elastic lithosphere spatially non-uniform change in topography
a
Initial Final Difference
( ) ( )1cos32
1cos 2
0,2 −= ηηP
( ) ( ) ( )[ ]θγωψθ coscos3
1, 0,20,2
22 PPa i −=ΛDifference in centrifugal potential determines geometry of sea level response [Mound & Mitrovica 1998]
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TPW + elastic lithosphere spatially non-uniform change in topography
a
Topography increases
Topography decreases
Amplitude depends on amount of TPW, elastic thickness of lithosphere, and
internal density structure
( ) ( ) ( )[ ]ff khg
+−Λ
=Δ 1,
,Topoψθ
ψθ
Degree 2 fluid tidal Love numbers
Details of TPW calculations inMatusyama et al. (2006)
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Inversion procedure
• Monte Carlo search for best-fit paleopoles for 100 km ≤ Te ≤ 400 km
• Allow constant C to vary freely
• Minimize RMS misfit between S(θ,ψ) and shoreline topography
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Approach: use shoreline topography to infer paleopole locations
Displacement (km)
Shoreline
Present pole
Paleopole
Elevation increases
Elevation decreases
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Best-fit paleopoles
Te = 200 km
Arabia (older, deeper)
Deuteronilus(younger, shallower)
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TPW can explain long-wavelength shoreline topography
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Inferred TPW path implies Tharsis would remain at the equator
90°
Best-fit paleopoles
What caused the polar wander?
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TPW Implications
Equatorial ocean ~4Ga? Ocean volumes
Arabia, 690 m
Deuteronilus, 150 m
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Oceans on Mars: Open questions
• Source of water, ocean formation time?
• Short- and long-term fates of ocean water?
• Independent evidence of oceans?
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Oceans are a major uncertainty in Mars’ global water budget
Based on data from Clifford and Parker (2001), Zuber et al. (1998), Smith et al. (1999) and Kass (2001) Clifford & Parker [2001], Zuber et al. [1998], Smith et al. [1999], Kass [2001]; as summarized by Carr & Head [2003]
Arabia Deuteronilus
NorthSouth
0.20.150.10.050
Volume in billions of km3)
Northern oceanplains
Lost to space
Regolith
Polar caps
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Collaborators
Chi-Yuen Wang
Martin Saar
Alex Wong
Isamu Matsuyama
Jerry Mitrovica
Taylor Perron QuickTime™ and aTIFF (Uncompressed) decompressor
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QuickTime™ and aTIFF (Uncompressed) decompressor
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QuickTime™ and aTIFF (Uncompressed) decompressor
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QuickTime™ and aTIFF (Uncompressed) decompressorare needed to see this picture.
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Why study water on Mars?
• Climate and habitability (Mars and Earth
were not so different once...)
• Human exploration
• Water and life
• Testing terrestrial science
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Lowell’s canals implied intelligent construction – leading to the idea of a desperate civilization… Invasion of Earth by Martians (Wells 1898)
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Percival Lowell’s canals 1895
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Movie 1953
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Summary
• Large floods on Mars require lots of water (big aquifers) and high permeability
• Some hydrogeological processes may be important on Mars, but not Earth
(e.g., impacts, slow cooling of the planet)
• Mars may once have had large oceans
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