EPOXI Status Small Bodies Assessment Group meeting 11/18/2009
Dennis Wellnitz, Co-Investigator for Mike A’Hearn, Principal Investigator
EPOXI EPOXI: EPOCh+DIXI
• Merger at NASA’s direction of EPOCh + DIXI • EPOCh = Extrasolar Planet Observation & Characterization – Ride-along science independent of the spacecraft trajectory • DIXI = Deep Impact eXtended Investigation – DI flyby spacecraft still healthy – DIXI originally proposed flying past 85P/Boethin – Significant orbital uncertainty – Could not find 85P/Boethin in summer-fall 2007 (est mag ~28) – Requested NASA permission to change to 103P/Hartley 2
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 2 Alternate Trajectory Rotating Coordinates
• Ecliptic view in Earth +Y relative rotating Direction of coordinates Earth Motion Hartley 2 TCM-12 Orbit • +X is anti-Sun in Ecliptic
• +Y is direction 2008 Loop of Earth motion in Ecliptic
• Post-perihelion Sun +X encounter on Earth 4 Nov 2010
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 3 Earth-relative Geometry
• June 2008 Earth Distant Distant Earth to Flyby #2 Earth Earth Flyby #3 30 Dec 2008 Flyby #1 Flyby #2 28Jun’10 June 2010 29Jun‘09 28Dec’09
• Latitude extremes north & south EPOXI North EPOXI North between Earth flybys
EPOXI South
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 4 Deep Impact
• Mating of flyby with impactor, April 2004 • Impactor spacecraft – 1/3 ton – 50% copper – Impactor Imaging Camera • White light • Flyby – 2/3 ton – Medium Resolution Imaging camera • 9 filters (2 clear) • 10 µrad/pixel • PSF ~ 1.5 pixel – High Resolution Imaging Camera • 8 filters • 2 µrad/pixel • Out of focus PSF ~9 pixels FWHM – Near-InfraRed Spectrometer • Δλ ~ 1.05 - 4.8 µm • R = δλ/λ ~ 250 to 700 • 10 µrad/pixel
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 5 EPOCh Science
EPOXI Transit Science
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa - 7 Pointing
Spacecraft pointing (in)stability is our principal challenge
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa - 8 EPOCh in “follow-up mode” : Jan-Aug 2008 • HAT-P-4 – a “puffed up” giant planet, R~1.3 times Jupiter, M~0.7 times Jupiter • TrES-3 – a giant planet in a 31-hour orbit! – potential for large reflected light signal (0.1%)! • WASP-3 – a strongly heated giant planet - thermal emission in the visible? • TrES-2 – a giant planet in the Kepler field... can combine with Kepler data • HAT-P-7 – even more strongly heated than WASP-3; also in Kepler field • GJ 436 – Smallest known transiting planet (Neptune-sized); M-dwarf star – Super-earths are predicted! We covered out to the habitable zone!
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa - 9 Nearly photon-limited precision....
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa - 10 GJ 436
• Gliese 436 • Predicted to have second planet to maintain eccentricity of first planet’s orbit • Observations of first planet’s transits yield improved orbital parameters • Upper limits for second planet from absence of transits • Plausible transits below statistical significance • Timing fluctuations • Ballard et al. 2009 submitted to ApJ EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 11 Detection Probability
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 12 Second Planet?
Best fit: R = 1.04 RE, P=8.42 d EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 13 Timing Variations
• EPOCh data Ground-based data • Discrepancies not understood • Variability in EPOCh-only data is still tentative EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 14 EPOCh Earth Observations
Imaging in all HRI filters hourly, (4 at 15 min cadence) IR spectroscopy every 2 hours
Study the Earth-as-an-exoplanet: Rotational light curves Inversion mapping Calibrated astronomical colors Model-independent spectroscopy validation of the Virtual Planet Laboratory (VPL)
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa - 15 Movies of Earth
28-29 May 2008 26-27 March 2009 EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa - 16 Inversion Mapping of Earth
• Sum the EPOXI data spatially - Earth as single pixel
Use PCA to infer what spectral components are present
...then invert the time history of those components as the Earth rotates
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa - 17 Alien Maps of an Ocean-Bearing World
• Inversion maps show oceans and continents, but with no latitude resolution
• Terrestrial Planet Finder will be able to infer the presence of oceans on Earth-like exoplanets
2009 Astrohys. J. 700 915-923
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa - 18 DIXI Science
EPOXI DIXI Objectives
• Probe cometary diversity • Enable separation of primordial heterogeneity from evolutionary heterogeneity – Understanding how comets work
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 20 Why DIXI? Understanding Diversity
• Nuclei are obviously different – Overall shape, topographic features, amount of activity – Nothing is obviously correlated with dynamics or age except that the only Oort cloud comet is more active than the others • What is common? – Source of activity? Depth of ice? Heterogeneity? Cratering? Other topographic features? Basic physics of how comets work? Origin? • What is the pattern that will tell us about origin of solar system? • Which new results at Tempel 1 are due to better measurements and which are unique to that comet? Need to see another nucleus.
Basilevsky & Keller 2007 Sol.Sys.Res.41, 109
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 21 Why DIXI? Understanding Diversity
• Observe more comets with same instruments and similar spatial resolution to find patterns – DI has best imaging and spectroscopy of any comet mission to date • Look for commonality of new phenomena discovered at Tempel 1 to find patterns
• DI flyby spacecraft is already out there and fully functional – Allows relatively cheap exploration of patterns among comets a la CONTOUR – Could allow discovery of yet other unexpected, new phenomena at another comet – Supports interpretation of returned samples from Stardust and provides opportunity for more insight into cometary origin and evolution before Rosetta
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 22 Origins Layering
• DI results suggested that cometesimals come together gently and preserve their integrity (limited interpenetration) leaving layers that persist today - TALPS (Belton et al. 2007 Icarus 187, 332) Images: D.D. Wellnitz • Some layers can be global - need to see both sides of nucleus • Other comets show signs of Dark layer layering but spatial resolution too limited - DI can see them easily
Stretched dark side of nucleus
Terminator
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 23 Origin vs. Evolution Chemical Differences
• H2O is released primarily in sub- solar region
• CO2 released primarily in “south” Sun – Enhanced near negative pole • Is this a sign of primordial cometesimals from different parts of protoplanetary disk? • Or is it a sign of evolution while negative pole was in “antarctic” Temperature Map Groussin et al. 2007 Icarus 187, 16 summer? • Need to observe another comet with a different polar orientation
Sun
Feaga et al. 2007. Icarus, 190, 345 EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 24 How Do Comets Work? Evolutionary Processes
• Why is ice localized on surface? – Related to outbursts? – Frost from previous night? • How do jets form?
– Why better correlated with CO2? • How deep is the ice? – Independent of surface morphology? Sunshine et al. 2006 Science 311, 1453 – Different for CO2 and H2O? • Would a fast rotator respond instantly to sunlight?
Farnham et al. 2007. Icarus, 187, 26 EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 25 How Do Comets Work? Evolutionary Properties
• Sudden outbursts are common • At certain rotational phases • Are they triggered by pockets with super-volatiles? • Or is it a structural difference? • Are these associated with the ice on the surface? • Is this phenomenon induced during evolution? Or primordial?
A’Hearn et al. 2005 Science 310, 258 EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 26 Flight System
• Telecom anomaly in 2008 – Prime TWTA showing obvious degradation beginning in 2007 – Overheating condition near perihelion in 2008 (80% of power reflected back into electronics) but also coincident with moving wave-guide switch – Now operating normally on backup TWTA for HGA observations, switch to prime TWTA for LGA operations when needed (only once thus far) • Telecom rate increased (after tests) from 200 kbps to 400 kbps since range is consistently small for DIXI • Star-tracker software patches being used experimentally to reduce jitter in pointing • All other systems operating nominally
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 27 Target Comparison
Tempel 1 Boethin Hartley 2
Nuclear Radius [km] 3.0±0.05 <0.5 ? 0.57±0.08
Nuclear Albedo 0.04 ? 0.03±0.01
Dust Production = log(Afρ) [cm] 2.2 2.3 2.6
Water Production = log(Q(OH)) [s-1] 27.6 28.3 28.6
r [AU] 1.49 1.16 1.064
Δ [AU] 0.9 0.9 0.156
Encounter Speed [km/s] 10.3 10.2 12.3
Approach Phase [°] 63 90 86
Hartley 2 is an IDEAL target scientifically for an extended mission EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 28 Hartley 2 vs. T1 Better SNR: Better Science
• All aspects of the observations on approach will see larger signals than at Tempel 1
– Smaller r ==> 1.9x more sunlight – Nucleus • Similar albedo to Tempel 1 and little variation due to phase angle difference ==> 1.9x brightness (visible imaging), but maybe 1.5x due to lower albedo (0.03/0.04) • Short exposures, thus insensitive to tracking (which was already excellent at Tempel 1) – Dust • Dust release scaled using optical data (in table) and confirmed using 10-12 micron data (ISO & IRAS) • Dust ~2.5x greater than Tempel 1 ==> >4x brightness (vis & near-IR) • Trace dust jets all the way to the surface? (dust brighter relative to nucleus) – Gas
• release ~7-20x greater than Tempel 1 scaled using optical data (OH, CN, C2) and ISO data (H2O, CO2) ==> ~15-40x brightness in near-IR emission bands and in narrow- band visible filters • Unprecedented signals for mapping innermost coma structures • Lack of impactor – More memory for flyby data – Simplified operations – More bandwidth for real-time data from flyby • Earth range 0.156 AU!! --> Higher data rates & better Earth-based observations
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 29 Encounter Conditions Hartley 2
• Approach Speed V = 12.319 km/s faster than baseline • Approach Phase Φ = 86.1º higher than baseline • Sun Distance r = 1.064 AU closer than baseline • Earth Distance r = 0.156 AU farther than baseline
Hartley 2 Encounter Sun-Velocity Plane Flyby “below” 4 November 2010 (perihelion + 7 days) nucleus at 90º Sun to Sun direc- 1.064 AU tion. Earth* 0.156 AU HGA pointing to
Approach phase Earth not avail- angle = 86.1º able in imaging V = 12.319 km/s attitude until after closest
* Earth 30.3º below Sun - V-inf plane approach. Nucleus Comet declination 6.6º from Earth EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 30 HST Lightcurve
• Initial Reductions: Weaver – Removal of CRs requires median combining - non-trivial for moving objects – Preliminary photometry – Added the orbits “blindly” based on pointing and commanded offsets – Data near 15 and 24 hrs may be near bad pixels • To Be Done – Look at jitter files to assess where telescope really was – Need to measure field stars and then shift & add with the comet rates – Must take account of parallax EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 31 GN and GS Data 5/22/09
50” FOV, N up E left; plate scale 2x2 binned: 0.146”/pix Sloan r’, 300 sec exposures - raw data frames L: Gemini S (4:30 UT), M & R: Gemini N (10:30, 13:30 UT)
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa - 32 HST Orbit 3
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa - 33 Hartley 2’s Rotation – P~16.6 hr
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa - 34 Observing Scenario Tentative
• E-30d to E-24d - cold soak to get spectrometer as cold as possible • E-24d to E-15d - peek-a-boo every 12 hours (downlink to Earth in cold attitude throughout approach) - imaging and spectroscopy • E-15d to E-1d - decrease interval between peeks to 8 hours at E-10d, 4 hours at E- 5d, continuous pointing at E-1d, imaging and spectroscopy • E-1d to E+3h - continuous observations, imaging and spectroscopy – Fill memory, downlink after E+30m – Nucleus diameter = 1 pixel E-18h to E+18h – CA = 900 km (will consider 750-800 for safety) • E+3h to E+30d - frequent imaging, continuous downlink
• Optional extra observations, staffing permitting – Enhance phase angle variation even more, better view of secular changes in comet – E-60d to E-30d - imaging – E+30d to E+60d – imaging
• Team meeting in late fall to design final plan
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 35 DIXI Bottom Line
• Small, active nucleus • Better SNR than at Tempel 1 • Expect at least as many interesting results as at Tempel 1
• All data from Tempel 1 publicly available in PDS • All data from Hartley 2 will be delivered to PDS within 6 months of encounter
• Alternative analyses welcomed – Either in collaboration or in competition
EPOXI 17 Nov 2009 EPOXI Status - SBAG 11/18/2009 mfa 36