Enceladus Dual Star Occultation Update C. J. Hansen 19 June 2012 Plume jets 2005 - gamma Orionis Occultation The Occultation Collection 2007 - zeta Orionis Occultation 2011 occ was a horizontal cut through the plume also 2010 - Solar Occultation Orion’s Belt Dual Occultation Geometry Rev 155 • Dual stellar occultation by Enceladus’ plume, E15, 19 October 2011, of epsilon Orionis (blue) and zeta Orionis (white) • Horizontal cut through plume Dual Occultation • Eps Ori (Alnilam, B star) – 16.5 km at closest point – HSP centered on eps Ori – Dimmer star in uv by ~2x • Zeta Ori (Alnitak, O star) – 37.9 km at closest point Eps Ori I/I0 Best fit is 1.35 x 1016 cm-2 • Ratio of occulted signal to unocculted signal: I/I0 • From average of data records above FWHM • Compare to water vapor – Cross-sections from Mota, 2005 – Same as we used for 2007 zeta Orionis occ Calibrated data • Summed spatial rows 2-4 • I0 calculated from 11 samples before and after the occultation • I calculated from records 317-324 (records with absorption > FWHM) • Best fit for wavelength channels 100-450 (broad absorptions) was 1.5 x 1016, but that resulted in too much absorption at deepest feature Zeta Ori I/I0 Best fit is 1.25 x 1016 cm-2 Calibrated data • Summed spatial rows 2-4 • I0 calculated from 11 samples before and after the occultation • I calculated from records 318-326 (absorption > FWHM) • Best fit for wavelength channels 100-450 (broad absorptions) was 1.3 x 1016, but that resulted in too much absorption at deepest feature Estimate of Water Source Rate from Enceladus = 200 kg/sec S = flux (source rate) = N * x * y * vth = (n/x) * x * y * vth = n * y * vth Where N = number density / cm3 2011: x * y = area vlos = 7.48 km/sec y = vlos * t at FWHM vth = thermal velocity = 45,000 cm/sec for T = 170K n = column density measured by UVIS y x v Year n (cm-2) Uncertainty +/- y (x 105 cm) vth (cm / sec) Flux: Flux: Molecules Kg/sec / sec Fraction of orbit from periapsis 2005 1.6 x 1016 0.15 x 1016 80 (est.) 45000 5.8 x 1027 170 0.27 2007 1.5 x 1016 0.14 x 1016 110 45000 7.4 x 1027 220 0.70 2010 0.9 x 1016 0.23 x 1016 150 45000 6 x 1027 180 0.19 2011 - e 1.35 x 1016 120 45000 7.3 x 1027 220 0.70 2011 - z 1.25 x 1016 133 45000 7.5 x 1027 224 All Horizontal Cuts Basemap from Spitale & Porco, 2007 Zeta Ori 2011 Solar occ In all occultations we look through the plume The groundtrack is the perpendicular dropped to the surface from the ray to the star • Blue => zeta Orionis 2007 • Red => Solar occ 2010 • Green => zeta Orionis 2011 Zeta Ori 2007 2007 The Jets – Past Occs 2010 a b c e d f • In the past we have identified collimated jets of gas from enhanced absorption features in the HSP (2007 zeta Ori occ) and the EUV (2010 solar occ) • Features in the 2007 HSP data were validated by Bonnie Meinke using her F ring statistical test techniques • Features in the 2010 solar occ were identified by looking for matching absorptions in the two windows, and making the argument that it was unlikely to be shot noise if they matched The Jets – 2011 HSP Data • This time the HSP data was lower snr Are these features real? – Eps Ori instead of zeta Ori – no features passed the rigorous statistical tests applied • Must rely on FUV data, cross-correlation of absorptions in same place / shifted in time No Statistically Significant Features in HSP From Bonnie: • Smallest m values are on the order of a few • Optical depths are below 0.4 • Nothing passes more stringent tests of repeated significance • NOTE: – Attenuation in plume ~5%, was ~10% last time – Perhaps this is more diffuse overall compared to 2008 zeta Ori occultation – Also, geometry made jets harder to distinguish from plume • Bonnie’s conclusions were verified by Bob West with a different technique Solar Occ • Geometry gave us well-separated jets Spacecraft viewed sun from this side Ingress Minimum Altitude Egress Basemap from Spitale & Porco, 2007 FUV Data vs. Time • Two sec integrations – Data is summed over all wavelengths, all spatial pixels • Zeta Ori trails eps Ori by ~4 sec • Enhanced absorption times input to groundtrack plot Eps – Zeta Direct Comparison • Zeta Ori is green; eps Ori is blue • Enhanced absorption shown as dots S/C • Clear correlation at Baghdad fissurecrossing • Damascus II and III (“c”), Baghdad I detected (“d”) • Slow return to unocculted signal may be activity between BI and BVII c/a Eps and Zeta Orionis Comparison a B c/a c d • • • • Calibrated data summed over rows 2-4 and over wavelength Average computed for each star, then ratios computed for each Time shifted to align enhanced absorption feature at B because geometry clearly correlated with fissure-crossing (4 sec) Also aligns egress Eps – Zeta Direct Comparison a S/C B c d • Clear signal of gas from Baghdad fissure (B), though no dust jet nearby • New Gas Jet • Damascus jets (DII and DIII): “c”, and BI detected: “d” • Weak feature at “a” is not located at a published dust jet, but ISS and CIRS have reported enhanced activity here Altitude of ray for eps and zeta Orionis Ingress Egress • Need to adjust timing for fact that zeta trailed eps Ori Altitude of ray for eps and zeta Orionis Altitude of Ray 70 60 Altitude (km) 50 40 eps Ori 30 Zeta Ori 20 10 0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 Sec after 640 • Altitude of zeta Ori shifted 4 sec • Offset of the two stars is ~ constant over the same territory • Delta ~ 20.5 km HSP • Comparison of HSP (targeted to eps Ori) to FUV for eps Ori • 0.008 sec integration summed to 2 sec to match FUV • Although features did not pass our statistical tests we can compare to the FUV data set • Then, bootstrap back to lesssummed HSP data to get better time resolution Now consider HSP Reconstructed trajectory • FUV eps Ori is blue • HSP eps Ori is red • Zeta Ori is green • Dots show enhanced absorption in HSP data summed to 1 sec • HSP groundtrack = eps Ori • All channels show enhanced absorption at Baghdad fissure; Align data from each channel there HSP and FUV Why is the HSP signal more attenuated than the FUV? h8 h1 h2 B h7 h4 • • • (Probably due to I0 calculation – it really needs to be a ramp?) h6 h5 Eps Ori FUV and HSP collected at the same time HSP summed to 1 sec could shift +/- 1 sec relative to FUV Aligned at new Baghdad jet B HSP - FUV h1 h2 B h7 h4 h6 h5 HSP enhanced absorption features do not pass statistical tests, however some appear to be correlated to jets: h2: feature “a” in FUV h4: Damascus III h5: Damascus II h6-h7: Baghdad I h8: Baghdad VII FUV Plume: Water Vapor Column Density eps Orionis From Don, column density as a function of time: • New Baghdad jet (“B”) emitting gas with column density = 1.6 x 1016 cm-2 • Deepest absorption (2.4 x 1016 vs 1.35 x 1016), due to Baghdad I Baghdad I B FUV Plume: Water Vapor Column Density zeta Orionis Baghdad I B Don’s plot of column depth as a function of time Zeta Orionis signal attenuation ~ 20 km higher than eps Ori Gas Dissipation eps BI zeta BI B B Column Density: Be = 1.6 x 1016 Bz = 1.0 x 1016 Bz/Be = 0.6 Range delta = 39.6 - 18.9 = 20.7 km BIe = 2.4 x 1016 BIz = 1.65 x 1016 Biz/BIe = 0.7 Range delta = 37.8 – 18.9 = 18.9 km Summary • Mass flux determined, comparable to other occs – Work to do to better quantify uncertainties • Jets tougher to identify because of low snr – Features in HSP data did not pass statistical tests – Geometry of occ along rather than across fissures may also have an effect? • Determination of spreading at the two altitudes also limited by temporal resolution of the FUV (2 sec integration time) – 2 sec x 7.48 km/sec line-of-sight velocity = 15 km – That is the approx. width of the jets derived in earlier occultations – But overall width of plume does not expand much Summary What can we learn from two cuts through the plume at different altitudes? • Overall width of plume is not very different (120 vs. 133 km) – Consistent with gas leaving at escape velocity on ~linear trajectory • Close to surface see less gas between jets/fissures than at higher altitude (gas is collisionless, diffusion is from slightly different trajectories leaving fissure) • DIII differentiable from BI jet at 18 km, not at 40 km • Can compare column density at jets at two altitudes -> dissipation -> spreading Back-up Jets vs. Tiger Stripes • As before, gas jets appear to correlate to dust jets Spacecraft viewed sun from this side Feature Altitude Dust * (km) Jet Alexandria IV a 20 Closest approach 19.7 b 21 Cairo V and/or VIII c 27 Baghdad I d 30 Baghdad VII e 38 Damascus III f 46 Damascus II * Altitude of ray to sun from limb Ingress Minimum Altitude Egress Basemap from Spitale & Porco, 2007 2007 - Plume Structure and Jets Summary of 2007 results • • • • • Significant events are likely gas jets UVIS-observed gas jets correlate with dust jets in images Characterize jet widths, opacity, density Density in jets ~2x density in background plume Ratio of vertical velocity to bulk velocity = 1.5, supersonic Supersonic gas jets are consistent with Schmidt et al. model of nozzle-accelerated gas coming from liquid water reservoir Jet Structure Optical Depth • Higher SNR enables better measurements of jets’ dimensions – more clearly distinguished from background plume • Density of gas in jets is twice the density of the background plume • The jets contribute 3.4% of the molecules escaping from Enceladus, based on comparison of the equivalent width of the broad plume compared to the jets’ total equivalent width Solar Occultation Jets Comparison to INMS results from E7 Jet Properties Feature Altitude of ray relative to limb Z0: Altitude of ray relative to jet source FWHM: full width half max(km ) Mach number ~ 2 * Z0 / FWHM Associat ed Dust Jet Excess attenuation at the jet (%) – for density calc* a 21.3 21.6 7 6 Alexandria IV 27 Closest approach 20.7 b 22 24 9 5 Cairo V and/or VIII 17 c 28.4 29 10 6 Baghdad I 19 d 31.2 36 10 7 Baghdad VII 12 e 39 40 10 8 Damascus III 13 f 47.5 49.7 14 7 Damascus II 14 *Average attenuation =17% CJH To Do List 1. Re-do calculation of eps Ori column density 2. Really rigorous determination of error bars for every occultation we have observed 3. Re-do summed FUV vs. time for just spatial pixels 24, calibrated properly 4. Plot HSP with eps Ori – now that timing issues are resolved! 5. Then go back to higher time resolution HSP data UVIS Observations of Enceladus’ Plume • Cassini’s Ultraviolet Imaging Spectrograph (UVIS) observes occultations of stars and the sun to probe Enceladus’ plume – Composition, mass flux, and plume and jet structure • Four stellar and one solar occultation observed to-date • Feb. 2005 - lambda Sco • No detection (equatorial) • July 2005 - gamma Orionis • Composition, mass flux • Oct. 2007 - zeta Orionis • Gas jets • May 2010 - Sun • Composition, jets • Oct. 2011 – epsilon and zeta Orionis dual occultation “Plume” refers to the broad cloud of dust and gas emanating from the south pole of Enceladus “Jets” are the highly collimated streams of ice particles (detected by ISS) and gas Nomenclature Plume Jets UVIS observes the gas component Data Bonnie’s Analysis Visual inspection • Human eye is good at picking out features Data Data Only one time integration Interesting wide hole Binned Data N Y ? ? ? Optical Depth M Values Caveats • How constant is the source rate? • Is the source rate modulated by the position of Enceladus in its orbit? From Larry: • The previous derivations use slightly different approaches to find the column density N: 2005 gOri: Last FUV spectrum measured, closest to surface. Best fit for N. Use scale height H to estimate L. 2007 zOri: Two 5-second FUV spectra that span the entire occultation. Best fit for N. 2010 Solar: 42 seconds of summed EUV spectra, covering the FWHM of the occultation. Best fit for N. 2011 eOri, zOri: Mean of photometric analysis (match total attenuation with H2O alone) of spectra within FWHM. This resembles DES approach for Solar occ. To get the mass flux, multiply by the mass of H2O molecule and FWHM. This gives zOri: 1.3 E16 * 134km (9 spectra) = 236kg/sec eOri: 1.4 E16 * 120km (8 spectra) = 227kg/sec • Given the variety of approaches, the different channels, IP and occultation tracks, it may be fortuitous that all 5 UVIS results give 208 ± 28 kg/sec. That is, a constant flux with standard deviation of 15%. Eps and Zeta Orionis Comparison • Signal of gas from Baghdad fissure (B-f), though no dust jet nearby • Damascus jets (DII and DIII) and BI identified BVII? • Feature at BVII? ? B-f DII&III BI • • • • Weak feature at “?” is not located at a published dust jet, but ISS and CIRS have reported enhanced activity here Average computed for each star Then ratios computed for each Time shifted to align enhanced absorption feature at B-f because geometry clearly correlated with fissure-crossing (4 sec) One more comparison to tidal energy model • Hurford et al 2007 model predicts tidallycontrolled differences in eruption activity as a function of where Enceladus is in its eccentric orbit • Expect fissures to open and close • Substantial changes are not seen in the occultation data, although they would be predicted, based on this model Position of Enceladus in its orbit at times of stellar occultations, and solar occultation Taken from Hurford et al, Nature 447:292 (2007) True Anomaly (deg) Fraction of orbit from Periapsis Position in Orbit Stress 105 Pa 0 0.0 Periapsis 0.3 0.186 May 18, 2010 90 0.25 One quarter -0.8 97.76 0.27 July 14, 2005 -0.77 180 0.5 Apoapsis -0.4 254.13 0.7 2007 and 2011 0.4 270 0.75 Three quarter 0.6 Source rate Kg/sec 180 170 220, 240