author_facet Sizemore, H. G.
Platz, T.
Schorghofer, N.
Prettyman, T. H.
De Sanctis, M. C.
Crown, D. A.
Schmedemann, N.
Neesemann, A.
Kneissl, T.
Marchi, S.
Schenk, P. M.
Bland, M. T.
Schmidt, B. E.
Hughson, K. H. G.
Tosi, F.
Zambon, F.
Mest, S. C.
Yingst, R. A.
Williams, D. A.
Russell, C. T.
Raymond, C. A.
Sizemore, H. G.
Platz, T.
Schorghofer, N.
Prettyman, T. H.
De Sanctis, M. C.
Crown, D. A.
Schmedemann, N.
Neesemann, A.
Kneissl, T.
Marchi, S.
Schenk, P. M.
Bland, M. T.
Schmidt, B. E.
Hughson, K. H. G.
Tosi, F.
Zambon, F.
Mest, S. C.
Yingst, R. A.
Williams, D. A.
Russell, C. T.
Raymond, C. A.
author Sizemore, H. G.
Platz, T.
Schorghofer, N.
Prettyman, T. H.
De Sanctis, M. C.
Crown, D. A.
Schmedemann, N.
Neesemann, A.
Kneissl, T.
Marchi, S.
Schenk, P. M.
Bland, M. T.
Schmidt, B. E.
Hughson, K. H. G.
Tosi, F.
Zambon, F.
Mest, S. C.
Yingst, R. A.
Williams, D. A.
Russell, C. T.
Raymond, C. A.
spellingShingle Sizemore, H. G.
Platz, T.
Schorghofer, N.
Prettyman, T. H.
De Sanctis, M. C.
Crown, D. A.
Schmedemann, N.
Neesemann, A.
Kneissl, T.
Marchi, S.
Schenk, P. M.
Bland, M. T.
Schmidt, B. E.
Hughson, K. H. G.
Tosi, F.
Zambon, F.
Mest, S. C.
Yingst, R. A.
Williams, D. A.
Russell, C. T.
Raymond, C. A.
Geophysical Research Letters
Pitted terrains on (1) Ceres and implications for shallow subsurface volatile distribution
General Earth and Planetary Sciences
Geophysics
author_sort sizemore, h. g.
spelling Sizemore, H. G. Platz, T. Schorghofer, N. Prettyman, T. H. De Sanctis, M. C. Crown, D. A. Schmedemann, N. Neesemann, A. Kneissl, T. Marchi, S. Schenk, P. M. Bland, M. T. Schmidt, B. E. Hughson, K. H. G. Tosi, F. Zambon, F. Mest, S. C. Yingst, R. A. Williams, D. A. Russell, C. T. Raymond, C. A. 0094-8276 1944-8007 American Geophysical Union (AGU) General Earth and Planetary Sciences Geophysics http://dx.doi.org/10.1002/2017gl073970 <jats:title>Abstract</jats:title><jats:p>Prior to the arrival of the Dawn spacecraft at Ceres, the dwarf planet was anticipated to be ice‐rich. Searches for morphological features related to ice have been ongoing during Dawn's mission at Ceres. Here we report the identification of pitted terrains associated with fresh Cerean impact craters. The Cerean pitted terrains exhibit strong morphological similarities to pitted materials previously identified on Mars (where ice is implicated in pit development) and Vesta (where the presence of ice is debated). We employ numerical models to investigate the formation of pitted materials on Ceres and discuss the relative importance of water ice and other volatiles in pit development there. We conclude that water ice likely plays an important role in pit development on Ceres. Similar pitted terrains may be common in the asteroid belt and may be of interest to future missions motivated by both astrobiology and in situ resource utilization.</jats:p> Pitted terrains on (1) Ceres and implications for shallow subsurface volatile distribution Geophysical Research Letters
doi_str_mv 10.1002/2017gl073970
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series Geophysical Research Letters
source_id 49
title Pitted terrains on (1) Ceres and implications for shallow subsurface volatile distribution
title_unstemmed Pitted terrains on (1) Ceres and implications for shallow subsurface volatile distribution
title_full Pitted terrains on (1) Ceres and implications for shallow subsurface volatile distribution
title_fullStr Pitted terrains on (1) Ceres and implications for shallow subsurface volatile distribution
title_full_unstemmed Pitted terrains on (1) Ceres and implications for shallow subsurface volatile distribution
title_short Pitted terrains on (1) Ceres and implications for shallow subsurface volatile distribution
title_sort pitted terrains on (1) ceres and implications for shallow subsurface volatile distribution
topic General Earth and Planetary Sciences
Geophysics
url http://dx.doi.org/10.1002/2017gl073970
publishDate 2017
physical 6570-6578
description <jats:title>Abstract</jats:title><jats:p>Prior to the arrival of the Dawn spacecraft at Ceres, the dwarf planet was anticipated to be ice‐rich. Searches for morphological features related to ice have been ongoing during Dawn's mission at Ceres. Here we report the identification of pitted terrains associated with fresh Cerean impact craters. The Cerean pitted terrains exhibit strong morphological similarities to pitted materials previously identified on Mars (where ice is implicated in pit development) and Vesta (where the presence of ice is debated). We employ numerical models to investigate the formation of pitted materials on Ceres and discuss the relative importance of water ice and other volatiles in pit development there. We conclude that water ice likely plays an important role in pit development on Ceres. Similar pitted terrains may be common in the asteroid belt and may be of interest to future missions motivated by both astrobiology and in situ resource utilization.</jats:p>
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author Sizemore, H. G., Platz, T., Schorghofer, N., Prettyman, T. H., De Sanctis, M. C., Crown, D. A., Schmedemann, N., Neesemann, A., Kneissl, T., Marchi, S., Schenk, P. M., Bland, M. T., Schmidt, B. E., Hughson, K. H. G., Tosi, F., Zambon, F., Mest, S. C., Yingst, R. A., Williams, D. A., Russell, C. T., Raymond, C. A.
author_facet Sizemore, H. G., Platz, T., Schorghofer, N., Prettyman, T. H., De Sanctis, M. C., Crown, D. A., Schmedemann, N., Neesemann, A., Kneissl, T., Marchi, S., Schenk, P. M., Bland, M. T., Schmidt, B. E., Hughson, K. H. G., Tosi, F., Zambon, F., Mest, S. C., Yingst, R. A., Williams, D. A., Russell, C. T., Raymond, C. A., Sizemore, H. G., Platz, T., Schorghofer, N., Prettyman, T. H., De Sanctis, M. C., Crown, D. A., Schmedemann, N., Neesemann, A., Kneissl, T., Marchi, S., Schenk, P. M., Bland, M. T., Schmidt, B. E., Hughson, K. H. G., Tosi, F., Zambon, F., Mest, S. C., Yingst, R. A., Williams, D. A., Russell, C. T., Raymond, C. A.
author_sort sizemore, h. g.
container_issue 13
container_start_page 6570
container_title Geophysical Research Letters
container_volume 44
description <jats:title>Abstract</jats:title><jats:p>Prior to the arrival of the Dawn spacecraft at Ceres, the dwarf planet was anticipated to be ice‐rich. Searches for morphological features related to ice have been ongoing during Dawn's mission at Ceres. Here we report the identification of pitted terrains associated with fresh Cerean impact craters. The Cerean pitted terrains exhibit strong morphological similarities to pitted materials previously identified on Mars (where ice is implicated in pit development) and Vesta (where the presence of ice is debated). We employ numerical models to investigate the formation of pitted materials on Ceres and discuss the relative importance of water ice and other volatiles in pit development there. We conclude that water ice likely plays an important role in pit development on Ceres. Similar pitted terrains may be common in the asteroid belt and may be of interest to future missions motivated by both astrobiology and in situ resource utilization.</jats:p>
doi_str_mv 10.1002/2017gl073970
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spelling Sizemore, H. G. Platz, T. Schorghofer, N. Prettyman, T. H. De Sanctis, M. C. Crown, D. A. Schmedemann, N. Neesemann, A. Kneissl, T. Marchi, S. Schenk, P. M. Bland, M. T. Schmidt, B. E. Hughson, K. H. G. Tosi, F. Zambon, F. Mest, S. C. Yingst, R. A. Williams, D. A. Russell, C. T. Raymond, C. A. 0094-8276 1944-8007 American Geophysical Union (AGU) General Earth and Planetary Sciences Geophysics http://dx.doi.org/10.1002/2017gl073970 <jats:title>Abstract</jats:title><jats:p>Prior to the arrival of the Dawn spacecraft at Ceres, the dwarf planet was anticipated to be ice‐rich. Searches for morphological features related to ice have been ongoing during Dawn's mission at Ceres. Here we report the identification of pitted terrains associated with fresh Cerean impact craters. The Cerean pitted terrains exhibit strong morphological similarities to pitted materials previously identified on Mars (where ice is implicated in pit development) and Vesta (where the presence of ice is debated). We employ numerical models to investigate the formation of pitted materials on Ceres and discuss the relative importance of water ice and other volatiles in pit development there. We conclude that water ice likely plays an important role in pit development on Ceres. Similar pitted terrains may be common in the asteroid belt and may be of interest to future missions motivated by both astrobiology and in situ resource utilization.</jats:p> Pitted terrains on (1) Ceres and implications for shallow subsurface volatile distribution Geophysical Research Letters
spellingShingle Sizemore, H. G., Platz, T., Schorghofer, N., Prettyman, T. H., De Sanctis, M. C., Crown, D. A., Schmedemann, N., Neesemann, A., Kneissl, T., Marchi, S., Schenk, P. M., Bland, M. T., Schmidt, B. E., Hughson, K. H. G., Tosi, F., Zambon, F., Mest, S. C., Yingst, R. A., Williams, D. A., Russell, C. T., Raymond, C. A., Geophysical Research Letters, Pitted terrains on (1) Ceres and implications for shallow subsurface volatile distribution, General Earth and Planetary Sciences, Geophysics
title Pitted terrains on (1) Ceres and implications for shallow subsurface volatile distribution
title_full Pitted terrains on (1) Ceres and implications for shallow subsurface volatile distribution
title_fullStr Pitted terrains on (1) Ceres and implications for shallow subsurface volatile distribution
title_full_unstemmed Pitted terrains on (1) Ceres and implications for shallow subsurface volatile distribution
title_short Pitted terrains on (1) Ceres and implications for shallow subsurface volatile distribution
title_sort pitted terrains on (1) ceres and implications for shallow subsurface volatile distribution
title_unstemmed Pitted terrains on (1) Ceres and implications for shallow subsurface volatile distribution
topic General Earth and Planetary Sciences, Geophysics
url http://dx.doi.org/10.1002/2017gl073970