The spectrum of Pluto, 0.40–0.93

Context. During the past 30 years the surface of Pluto has been characterized and its variability monitored through continuous near-infrared spectroscopic observations. But in the visible range only a few data are available. Aims. The aim of this work is to define Pluto’s relative reflectance in th...

Full description

Bibliographic Details
Main Authors: Lorenzi, V., Pinilla-Alonso, N., Licandro, J., Cruikshank, D. P., Grundy, W. M., Emery, J. P., Binzel, Richard P
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format: Article
Language:en_US
Published: EDP Sciences 2017
Online Access:http://hdl.handle.net/1721.1/106193
_version_ 1811087000485232640
author Lorenzi, V.
Pinilla-Alonso, N.
Licandro, J.
Cruikshank, D. P.
Grundy, W. M.
Emery, J. P.
Binzel, Richard P
author2 Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
author_facet Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Lorenzi, V.
Pinilla-Alonso, N.
Licandro, J.
Cruikshank, D. P.
Grundy, W. M.
Emery, J. P.
Binzel, Richard P
author_sort Lorenzi, V.
collection MIT
description Context. During the past 30 years the surface of Pluto has been characterized and its variability monitored through continuous near-infrared spectroscopic observations. But in the visible range only a few data are available. Aims. The aim of this work is to define Pluto’s relative reflectance in the visible range to characterize the different components of its surface, and to provide ground based observations in support of the New Horizons mission. Methods. We observed Pluto on six nights between May and July 2014 with the imager/spectrograph ACAM at the William Herschel Telescope (La Palma, Spain). The six spectra obtained cover a whole rotation of Pluto (Prot = 6.4 days). For all the spectra, we computed the spectral slope and the depth of the absorption bands of methane ice between 0.62 and 0.90 μm. To search for shifts in the center of the methane bands, which are associated with dilution of CH[subscript 4] in N[subscript 2], we compared the bands with reflectances of pure methane ice. Results. All the new spectra show the methane ice absorption bands between 0.62 and 0.90 μm. Computation of the depth of the band at 0.62 μm in the new spectra of Pluto and in the spectra of Makemake and Eris from the literature, allowed us to estimate the Lambert coefficient at this wavelength at temperatures of 30 K and 40 K, which has never been measured before. All the detected bands are blueshifted with respect to the position for pure methane ice, with minimum shifts correlated to the regions where the abundance of methane is higher. This could be indicative of a dilution of CH[subscript 4]:N[subscript 2] that is more saturated in CH[subscript 4]. The longitudinal and secular variations in the parameters measured in the spectra are in accordance with results previously reported in the literature and with the distribution of the dark and bright materials that show the Pluto’s color maps from New Horizons.
first_indexed 2024-09-23T13:38:17Z
format Article
id mit-1721.1/106193
institution Massachusetts Institute of Technology
language en_US
last_indexed 2024-09-23T13:38:17Z
publishDate 2017
publisher EDP Sciences
record_format dspace
spelling mit-1721.1/1061932022-10-01T16:13:13Z The spectrum of Pluto, 0.40–0.93 Lorenzi, V. Pinilla-Alonso, N. Licandro, J. Cruikshank, D. P. Grundy, W. M. Emery, J. P. Binzel, Richard P Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences Binzel, Richard P Context. During the past 30 years the surface of Pluto has been characterized and its variability monitored through continuous near-infrared spectroscopic observations. But in the visible range only a few data are available. Aims. The aim of this work is to define Pluto’s relative reflectance in the visible range to characterize the different components of its surface, and to provide ground based observations in support of the New Horizons mission. Methods. We observed Pluto on six nights between May and July 2014 with the imager/spectrograph ACAM at the William Herschel Telescope (La Palma, Spain). The six spectra obtained cover a whole rotation of Pluto (Prot = 6.4 days). For all the spectra, we computed the spectral slope and the depth of the absorption bands of methane ice between 0.62 and 0.90 μm. To search for shifts in the center of the methane bands, which are associated with dilution of CH[subscript 4] in N[subscript 2], we compared the bands with reflectances of pure methane ice. Results. All the new spectra show the methane ice absorption bands between 0.62 and 0.90 μm. Computation of the depth of the band at 0.62 μm in the new spectra of Pluto and in the spectra of Makemake and Eris from the literature, allowed us to estimate the Lambert coefficient at this wavelength at temperatures of 30 K and 40 K, which has never been measured before. All the detected bands are blueshifted with respect to the position for pure methane ice, with minimum shifts correlated to the regions where the abundance of methane is higher. This could be indicative of a dilution of CH[subscript 4]:N[subscript 2] that is more saturated in CH[subscript 4]. The longitudinal and secular variations in the parameters measured in the spectra are in accordance with results previously reported in the literature and with the distribution of the dark and bright materials that show the Pluto’s color maps from New Horizons. 2017-01-04T20:18:55Z 2017-01-04T20:18:55Z 2016-01 2015-08 Article http://purl.org/eprint/type/JournalArticle 0004-6361 1432-0746 http://hdl.handle.net/1721.1/106193 Lorenzi, V. et al. “The Spectrum of Pluto, 0.40–0.93 μ M: I. Secular and Longitudinal Distribution of Ices and Complex Organics.” Astronomy & Astrophysics 585 (2016): A131. © 2016 ESO en_US http://dx.doi.org/10.1051/0004-6361/201527281 Astronomy & Astrophysics Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. application/pdf EDP Sciences EDP Sciences
spellingShingle Lorenzi, V.
Pinilla-Alonso, N.
Licandro, J.
Cruikshank, D. P.
Grundy, W. M.
Emery, J. P.
Binzel, Richard P
The spectrum of Pluto, 0.40–0.93
title The spectrum of Pluto, 0.40–0.93
title_full The spectrum of Pluto, 0.40–0.93
title_fullStr The spectrum of Pluto, 0.40–0.93
title_full_unstemmed The spectrum of Pluto, 0.40–0.93
title_short The spectrum of Pluto, 0.40–0.93
title_sort spectrum of pluto 0 40 0 93
url http://hdl.handle.net/1721.1/106193
work_keys_str_mv AT lorenziv thespectrumofpluto040093
AT pinillaalonson thespectrumofpluto040093
AT licandroj thespectrumofpluto040093
AT cruikshankdp thespectrumofpluto040093
AT grundywm thespectrumofpluto040093
AT emeryjp thespectrumofpluto040093
AT binzelrichardp thespectrumofpluto040093
AT lorenziv spectrumofpluto040093
AT pinillaalonson spectrumofpluto040093
AT licandroj spectrumofpluto040093
AT cruikshankdp spectrumofpluto040093
AT grundywm spectrumofpluto040093
AT emeryjp spectrumofpluto040093
AT binzelrichardp spectrumofpluto040093