The Importance of Ice Vertical Resolution for Snowball Climate and Deglaciation

Journal of Climate American Meteorological Society 23:22 (2010) 6100-6109

Authors:

Dorian S Abbot, Ian Eisenman, Raymond T Pierrehumbert

HARMONI: A single-field wide-band integral-field spectrograph for the European ELT

Proceedings of SPIE - The International Society for Optical Engineering 7735:PART 1 (2010)

Authors:

N Thatte, M Tecza, F Clarke, RL Davies, A Remillieux, R Bacon, D Lunney, S Arribas, E Mediavilla, F Gago, N Bezawada, P Ferruit, A Fragoso, D Freeman, J Fuentes, T Fusco, A Gallie, A Garcia, T Goodsall, F Gracia, A Jarno, J Kosmalski, J Lynn, S McLay, D Montgomery, A Pecontal, H Schnetler, H Smith, D Sosa, G Battaglia, N Bowles, L Colina, E Emsellem, A Garcia-Perez, S Gladysz, I Hook, P Irwin, M Jarvis, R Kennicutt, A Levan, A Longmore, J Magorrian, M McCaughrean, L Origlia, R Rebolo, D Rigopoulou, S Ryan, M Swinbank, N Tanvir, E Tolstoy, A Verma

Abstract:

We describe the results of a Phase A study for a single field, wide band, near-infrared integral field spectrograph for the European Extremely Large Telescope (E-ELT). HARMONI, the High Angular Resolution Monolithic Optical & Nearinfrared Integral field spectrograph, provides the E-ELT's core spectroscopic requirement. It is a work-horse instrument, with four different spatial scales, ranging from seeing to diffraction-limited, and spectral resolving powers of 4000, 10000 & 20000 covering the 0.47 to 2.45 μm wavelength range. It is optimally suited to carry out a wide range of observing programs, focusing on detailed, spatially resolved studies of extended objects to unravel their morphology, kinematics and chemical composition, whilst also enabling ultra-sensitive observations of point sources. We present a synopsis of the key science cases motivating the instrument, the top level specifications, a description of the opto-mechanical concept, operation and calibration plan, and image quality and throughput budgets. Issues of expected performance, complementarity and synergies, as well as simulated observations are presented elsewhere in these proceedings[1]. © 2010 Copyright SPIE - The International Society for Optical Engineering.

Abundances of Jupiter's trace hydrocarbons from Voyager and Cassini

Planetary and Space Science 58:13 (2010) 1667-1680

Authors:

CA Nixon, RK Achterberg, PN Romani, M Allen, X Zhang, NA Teanby, PGJ Irwin, FM Flasar

Abstract:

The flybys of Jupiter by the Voyager spacecraft in 1979, and over two decades later by Cassini in 2000, have provided us with unique datasets from two different epochs, allowing the investigation of seasonal change in the atmosphere. In this paper we model zonal averages of thermal infrared spectra from the two instruments, Voyager 1 IRIS and Cassini CIRS, to retrieve the vertical and meridional profiles of temperature, and the abundances of the two minor hydrocarbons, acetylene (C2H2) and ethane (C 2H6). The spatial variation of these gases is controlled by both chemistry and dynamics, and therefore their observed distribution gives us an insight into both processes. We find that the two gases paint quite different pictures of seasonal change. Whilst the 2-D cross-section of C 2H6 abundance is slightly increased and more symmetric in 2000 (northern summer solstice) compared to 1979 (northern fall equinox), the major trend of equator to pole increase remains. For C2H2 on the other hand, the Voyager epoch exhibits almost no latitudinal variation, whilst the Cassini era shows a marked decrease polewards in both hemispheres. At the present time, these experimental findings are in advance of interpretation, as there are no published models of 2-D Jovian seasonal chemical variation available for comparison. © 2010 Elsevier Ltd. All rights reserved.

Diviner lunar radiometer observations of cold traps in the moon's south polar region

Science 330:6003 (2010) 479-482

Authors:

DA Paige, MA Siegler, JA Zhang, PO Hayne, EJ Foote, KA Bennett, AR Vasavada, BT Greenhagen, JT Schofield, DJ McCleese, MC Foote, E DeJong, BG Bills, W Hartford, BC Murray, CC Allen, K Snook, LA Soderblom, S Calcutt, FW Taylor, NE Bowles, JL Bandfield, R Elphic, R Ghent, TD Glotch, MB Wyatt, PG Lucey

Abstract:

Diviner Lunar Radiometer Experiment surface-temperature maps reveal the existence of widespread surface and near-surface cryogenic regions that extend beyond the boundaries of persistent shadow. The Lunar Crater Observation and Sensing Satellite (LCROSS) struck one of the coldest of these regions, where subsurface temperatures are estimated to be 38 kelvin. Large areas of the lunar polar regions are currently cold enough to cold-trap water ice as well as a range of both more volatile and less volatile species. The diverse mixture of water and high-volatility compounds detected in the LCROSS ejecta plume is strong evidence for the impact delivery and cold-trapping of volatiles derived from primitive outer solar system bodies.

Infrared limb sounding of Titan with the cassini composite infrared spectrometer: Effects of the mid-IR detector spatial responses: Errata

Applied Optics 49:29 (2010) 5575-5576

Authors:

CA Nixon, NA Teanby, SB Calcutt, S Aslam, DE Jennings, VG Kunde, FM Flasar, PGJ Irwin, FW Taylor, DA Glenar, MD Smith

Abstract:

We provide a revised Table 5 for the paper by Nixon et al. [Appl. Opt. 48, 1912 (2009)], in which the abundances of 13CO2 and C 18O were incorrect . © 2010 Optical Society of America.