reconnaissance observations of rosetta target 67p/c-g
TRANSCRIPT
Reconnaissance Observations of Rosetta Target 67P/C-G
Stephen Lowry Centre for Astrophysics and Planetary Science
University of Kent, UK
RAS – Dec 2010
ESA’s Cornerstone Rosetta mission -
The OSIRIS Project
Research Programmes SEPPCoN - Survey of the Ensemble Properties of Cometary Nuclei
The Asteroidal YORP Effect:
Detection and Theoretical
Investigations
Near Earth Asteroids - Physical Properties and Composition
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
• Discovered in Oct 22nd, 1969 by Klim Ivanovic Churyumov (Univ. of Kiev, Ukraine), and Svetlana Ivanovna Gerasimenko (Inst. Of Astrophysics, Dushanbe, Tajilistan) at the Alma-Ata Astrophysical Institute, Russia.
• Selected to be new target of ESA’s Rosetta mission in 2003. At this time very little known about nucleus.
• Encouraged extensive observations since (initially by Lowry et al., Boehnhardt et al, and HST measurements by Lamy et al.)
67P/Churyumov-Gerasimenko Discovery and Selection as Rosetta Target
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
67P/Churyumov-Gerasimenko Orbital Characteristics
Lamy et al. (2006) Space Sci. Rev.
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
• The orbital evolution of comet 67P/C-G is chaotic due to repeated close encounters with Jupiter (Carusi et al., 1985; Belyaev et al., 1986; Krolikowska, 2003).
• The encounter which occurred in February 1959 at a distance of only 0.0518 AU considerably modified the orbit: the perihelion distance dropped from 2.74 to 1.28 AU, the eccentricity increased from 0.36 to 0.63, its orbital period was shortened from 8.97 to 6.55 yr
67P/Churyumov-Gerasimenko Orbital Evolution
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
• Constraining the nucleus size, shape, spin state and surface properties is critical for establishing likely surface properties (active area, thermal properties):
Important for interpreting ground based observations of coma activity – specifically Thermo-physical models of surface properties that attempt to describe observations (see De Santis et al., Icarus 2010: Shape and obliquity effects on the thermal evolution of the Rosetta target 67P/Churyumov–Gerasimenko cometary nucleus)
Also critical for lander phase!
• Important to set a context for in-situ measurements. - What is the baseline activity throughout orbit? - When does it start outgassing, relative to initial encounter by Rosetta? - Also, how is comet behaving as seen from ground based observations, during encounter? Can use wider suite of instruments from ground.
67P/Churyumov-Gerasimenko Importance of reconnaissance observations
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
• Critical to have detailed models of dust environment that Rosetta will be subjected to, as well as lander.
• Critical to establish models based on ground-based observations (+ HST etc) ahead of encounter so that analysis techniques can be verified ahead of time. Provides robust credibility of remote sensing methods.
67P/Churyumov-Gerasimenko Importance of reconnaissance observations
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
Nucleus HST Observations
• Shortly after selection of a new suitable cometary target for Rosetta, Lamy et al. were granted Director Discretionary Time on the Hubble Space Telescope to pin down the size of its nucleus as this was a critical issue for the safe landing of the Philae surface module.
• The observations were performed on 12 and 13 March 2003, when the comet was 2.50 AU from the Sun, 1.52 AU from the Earth, and at a phase angle of 4.8°.
• Applied coma subtraction technique to ascertain nucleus properties.
HST WFPC2 (PC mode) image from March 2003 with the F675W filter (Lamy et al., A&A 2006)
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
Nucleus HST Observations
- R-band radius = 1.98 ± 0.02 km (assuming A, β = 0.04)
- The rotation period of the nucleus was determined from seven different period searching methods and is 12.41 ± 0.41 hours
- The spheroidal solution implied by the double-peaked light curve has semiaxes lower limits of a = 2.41 km and b = c = 1.55 km.
HST WFPC2 (PC mode) image from March 2003 with the F675W filter (Lamy et al., A&A 2006)
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
Aphelion Monitoring from ESO 67P/Churyumov-Gerasimenko
Observing Team: Alan Fitzsimmons, Colin Snodgrass, Olivier Hainaut, Laurent Jorda, Mikko Kaasalainen, Philippe Lamy, Miriam Rengel, Imre Toth.
• 26 February, 2004 (VR) (Rh = 4.48 AU [outbound], Δ = 3.96 AU, α = 11.45°)
• 23 April, 2004 (VR), 27 April 2004 (VRI) (Rh = 4.72 AU [outbound], Δ = 3.72 AU, α = 1.12°)
• May 10th, 12th, and 14th, 2004 (VRI) (Rh = 5.60 AU [Q = 5.71 AU], Δ = 4.59 AU, α = 0.07-0.84°)
• July 16th, 19th, 22nd, 2007 (3 nights in VRI) (Rh = 4.63 AU [inbound], Δ = 3.72 AU, α = 6.04-7.28°)
• 13 September, 2007 (0.5 night in VRI) (Rh = 4.40 AU [inbound], Δ = 4.25 AU, α = 13.21°) - Encounter point!
3.5m NTT
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
Aphelion Monitoring from ESO 67P/Churyumov-Gerasimenko
3.5m NTT
• Three nights of data taken with the 3.5m New Technology Telescope (European Southern Observatory, La Silla Chile), under good conditions on May 10th, 12th and 14th, 2004.
• The photometry consists of visual broadband CCD imaging with VRI filters covering the 0.55-0.79 micron range, taken with the EMMI instrument.
• Optical observing sequence for each object was 6R-8V-6R-8I-6R-8V-6R…, which allow colour indices to be determined without the confounding effects of rotation.
• Data set is includes full lightcurve coverage in V, R and I filters.
• This will allow robust determinations of the size, projected shape, synodic spin rate, colour indices (or possible presence of colour variations across surface).
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
Aphelion Monitoring from ESO
May 10 71x100s R-filter images
May 12 123x100s R-filter images
May 14 82x100s R-filter images
67P/Churyumov-Gerasimenko
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
Aphelion Monitoring from ESO 67P/Churyumov-Gerasimenko
1. Mean apparent R magnitude is 22.41 ± 0.03 Δm = 0.38 ± 0.04 (a/b ≥ 1.42 ± 0.05)
2. Mean effective radius is 2.26 ± 0.03 km (for AR of 0.04 and β = 0.035 mags./deg.) 3. Semi-axes: a = 2.07 ± 0.04, b = 2.94 ± 0.15 km
4. Colour index: (V-R) = 0.41 ± 0.04 (Spectral Gradient ~4.7 %/100nm)
5. No dust trail seen in R-filter ultra-deep images
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
Aphelion Monitoring from ESO 67P/Churyumov-Gerasimenko
Synodic rotation period = 12.72 ± 0.05 hrs
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
Aphelion Monitoring from ESO 67P/Churyumov-Gerasimenko
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
Aphelion Monitoring from ESO 67P/Churyumov-Gerasimenko
1. Observations obtained of comet 67P/C-G in May 2005 when comet was at 5.6 AU from Earth and at opposition (4 additional data sets obtained)
2. Comet appeared stellar on co-added ultra-deep images.
3. Best-fit synodic rotation period is 12.72 ± 0.05 hours
4. Asymmetric light-curve observed with full magnitude range of 0.38 ± 0.04, which corresponds to a/b ≥ 1.42 ± 0.05.
5. Mean apparent magnitude is 22.41 ± 0.03, which corresponds to an absolute magnitude HR of 15.34 ± 0.03.
6. Mean effective radius is 2.26 ± 0.03 km (assuming AR of 0.04 and β = 0.035 mags./degree).
5. Semi-axes are: a = 2.07 ± 0.04, b = 2.94 ± 0.15 km (same AR and β).
6. Colour indices: (V-R) = 0.41 ± 0.04 (S′ ~ 4.7 %/100 nm)
7. No dust trail seen in R-filter ultra-deep images.
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
HST/ESO shape Model
Lamy et al. (2006) Space Sci. Rev.
HST May 10
May 12 May 14
Prograde
Retrograde
67P/Churyumov-Gerasimenko
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
Pole Solutions
Lamy et al. (2006) Space Sci. Rev.
HST May 10
May 12 May 14
67P/Churyumov-Gerasimenko
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
67P/Churyumov-Gerasimenko VLT/FORS2 observations
• ESO VLT images: June 2004, May 2006, August 2006 (Tubiana et al. A&A 2008)
• Rh = 4.89 – 5.62 AU, α = 0.5 – 10.6°
• Rotation Period = 12.7047 ± 0.0011 hours
• Effective radius = 2.38 ± 0.04 km (A = 0.04)
• Phase coefficient = 0.076 ± 0.003 mag./°
• No colour variation with rotation seen, based on optical spectra and broadband colours (May 2006)
• Optical dust trail seen (a: I-filter, b: R-filter, c: V-filter, d: VRI composite), Extends more than 153.25”x8” or 4.8x105 km and 2.5 x 104 km at comet.
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
67P/Churyumov-Gerasimenko VLT/FORS2 observations
• ESO VLT images: June 2004, May 2006, August 2006 (Tubiana et al. A&A 2008)
• Rh = 4.89 – 5.62 AU, α = 0.5 – 10.6°
• Rotation Period = 12.7047 ± 0.0011 hours
• Effective radius = 2.38 ± 0.04 km (A = 0.04)
• Phase coefficient = 0.076 ± 0.003 mag./°
• No colour variation with rotation seen, based on optical spectra and broadband colours (May 2006)
• Optical dust trail seen (a: I-filter, b: R-filter, c: V-filter, d: VRI composite), Extends more than 153.25”x8” or 4.8x105 km and 2.5 x 104 km at comet.
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
67P/Churyumov-Gerasimenko VLT/FORS2 observations: Optical Dust Trail
• ESO VLT images: June 2004, May 2006, August 2006 (Tubiana et al. A&A 2008)
• Rh = 4.89 – 5.62 AU, α = 0.5 – 10.6°
• Rotation Period = 12.7047 ± 0.0011 hours
• Effective radius = 2.38 ± 0.04 km (A = 0.04)
• Phase coefficient = 0.076 ± 0.003 mag./°
• No colour variation with rotation seen, based on optical spectra and broadband colours (May 2006)
• Optical dust trail seen (a: I-filter, b: R-filter, c: V-filter, d: VRI composite), Extends more than 153.25”x8” or 4.8x105 km and 2.5 x 104 km at comet.
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
67P/Churyumov-Gerasimenko Spitzer observations: Nucleus & Dust Trail
• Spitzer MIPS 24µm images: Feb 2004, spanning 12.5 hrs (Lamy et al. A&A 2008)
• Rh = 4.48 AU, α = 12.1°
• Rotation period not well constrained
• Semi-axis: 4.40–5.20 km, 4.16–4.30 km, and 3.40–3.50 km (Effective radius = 1.93 – 2.03 km)
• Albedo = 0.039 – 0.043
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
67P/Churyumov-Gerasimenko Spitzer observations: Nucleus & Dust Trail
• Spitzer MIPS 24µm images: Feb 2004, spanning 12.5 hrs (Lamy et al. A&A 2008)
• Rh = 4.48 AU, α = 12.1°
• Rotation period not well constrained
• Semi-axis: 4.40–5.20 km, 4.16–4.30 km, and 3.40–3.50 km (Effective radius = 1.93 – 2.03 km)
• Albedo = 0.039 – 0.043
• The success of the landing of the Philae surface module now remains critically dependent upon the bulk density of the nucleus. A value of 0.1-0.37 g cm−3 (Davidsson & Gutiérrez, 2005) would ensure a safe landing. But this estimate could be as high as 0.5-0.6 g cm−3
Lamy et al. (A&A 2008),
Hilchenbach et al. (in ‘The New ROSETTA Targets’, 2004)
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
Kelley et al. (ApJ 2009)
67P/Churyumov-Gerasimenko Spitzer observations: IR Dust Trail & Nucleus
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
• Spitzer MIPS 24µm images: Feb 2004, spanning 12.5 hrs (Lamy et al. A&A 2008)
• Rh = 5.5 – 4.3 AU, α = 11-13°
• Radiometric effective radius 2.04 ± 0.11 km
• Albedo = 0.054 ± 0.006
• Maximum grain size 5µm. The grain number density near the nucleus is (1.33 ± 0.03) x 10−12 m−3, assuming that the dust is composed of millimeter-sized grains. The density corresponds to a Rosetta dust impact probability upper limit of 0.3% during the spacecraft’s approach to the nucleus in 2014.
• Rotation period well constrained 12.7047 hrs
67P/Churyumov-Gerasimenko Spitzer observations: IR Dust Trail
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
Kelley et al. (ApJ 2009) • Spitzer MIPS 24µm images: Feb 2004, spanning 12.5 hrs (Lamy et al. A&A 2008)
• Rh = 5.5 – 4.3 AU, α = 11-13°
• Radiometric effective radius 2.04 ± 0.11 km
• Albedo = 0.054 ± 0.006
• Maximum grain size 5µm. The grain number density near the nucleus is (1.33 ± 0.03) x 10−12 m−3, assuming that the dust is composed of millimeter-sized grains. The density corresponds to a Rosetta dust impact probability upper limit of 0.3% during the spacecraft’s approach to the nucleus in 2014.
• Rotation period well constrained 12.7047 hrs
The Rosetta lander (delivery planned at 3 AU), may collect a monolayer of grains larger than two microns every five days.
While the Rosetta probe orbiting at a distance of 10 km from the nucleus will collect the first monolayer of grains larger than two microns after the first four months
(i) grains larger than 1 cm are ejected from the coma;
(ii) the mass loss rate is larger than 100 kg s−1;
(iii) the mass loss rate is dominated by the largest ejected grains;
(iv) the dust coma brightness (e.g. the Afρ quantity) depends significantly or even mainly upon the largest ejected dust grains;
(v) a low Afρ = 0.1 m is consistent with such a scenario;
(vi) the first dust monolayer will be collected by the lander in the first week;
(vii) the first dust monolayer will be collected by the orbiter in the first four months spent at distances less than 10 km from the nucleus;
(viii) since the dust brightness is dominated by, or at least significantly depends upon the largest ejected grains, spurious identifications of stars by the navigation cameras is a primary danger for the mission: robust software against false nucleus detection is mandatory.
67P/Churyumov-Gerasimenko Dust Environment (Fulle, A&A 2004)
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
67P/Churyumov-Gerasimenko Jet Structures
Lara et al. (A&A 2011)
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
67P/Churyumov-Gerasimenko Jet Structures
Lara et al. (A&A 2011)
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
67P/Churyumov-Gerasimenko EPOXI images of 103P/Hartley 2
Image Credit: NASA. 2010
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
67P/Churyumov-Gerasimenko Coma Production Rates
- The Rosetta lander (delivery planned at 3 AU), may collect a monolayer of grains larger than two microns every five days (Lara et al. A&A 2011).
- C2 and CN production rates are stable around perihelion (also no major outbursts detected – unlike 17P/Holmes – 0.5m fold increase in brightness – occurred on previous orbits – would represent major risk to spacecraft.
- Rates imply ‘typical’ classification: Could imply Oort Cloud source for 67P/C-G – which in turn implies an original formation location at the Uranus-Neptune region and slightly beyond.
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
Rosetta phase
Perihelion
Nucleus Monitoring periods
67P/Churyumov-Gerasimenko Future Observability
Aphelion
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
67P/Churyumov-Gerasimenko Future Observability Rosetta phase
Perihelion Aphelion
Nucleus Monitoring periods
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G
67P/Churyumov-Gerasimenko Future Observability Rosetta phase
Perihelion Aphelion
Nucleus Monitoring periods
RAS SDM: Dr. Stephen Lowry – Observations of 67P/C-G