Compact Reconnaissance Imaging Spectrometer for Mars

confirm many previous models and shed new light on the nature of polar surface materials, particularly in intermediate-albedo units of the polar layered deposits, many of which are found to be ice-rich. We identify hydrated non ice materials present in many low-albedo troughs, as well as in the circ...

Full description

Bibliographic Details
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Ice
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.655.1406
http://planetary.brown.edu/pdfs/3960.pdf
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.655.1406
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.655.1406 2023-05-15T16:37:11+02:00 Compact Reconnaissance Imaging Spectrometer for Mars The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.655.1406 http://planetary.brown.edu/pdfs/3960.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.655.1406 http://planetary.brown.edu/pdfs/3960.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://planetary.brown.edu/pdfs/3960.pdf text ftciteseerx 2016-01-08T16:34:26Z confirm many previous models and shed new light on the nature of polar surface materials, particularly in intermediate-albedo units of the polar layered deposits, many of which are found to be ice-rich. We identify hydrated non ice materials present in many low-albedo troughs, as well as in the circumpolar erg that was previously associated with gypsum. We identify icy outlier deposits that may be related to subsurface thermophysical properties and permafrost. New observations of the gypsum-rich dune material constrain models for its formation and distribution. Intrinsic properties of ice content and grain size are found to be independent of the albedo of fine layered units and may provide a novel method for stratigraphic identification and correlation. Text Ice permafrost Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description confirm many previous models and shed new light on the nature of polar surface materials, particularly in intermediate-albedo units of the polar layered deposits, many of which are found to be ice-rich. We identify hydrated non ice materials present in many low-albedo troughs, as well as in the circumpolar erg that was previously associated with gypsum. We identify icy outlier deposits that may be related to subsurface thermophysical properties and permafrost. New observations of the gypsum-rich dune material constrain models for its formation and distribution. Intrinsic properties of ice content and grain size are found to be independent of the albedo of fine layered units and may provide a novel method for stratigraphic identification and correlation.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
title Compact Reconnaissance Imaging Spectrometer for Mars
spellingShingle Compact Reconnaissance Imaging Spectrometer for Mars
title_short Compact Reconnaissance Imaging Spectrometer for Mars
title_full Compact Reconnaissance Imaging Spectrometer for Mars
title_fullStr Compact Reconnaissance Imaging Spectrometer for Mars
title_full_unstemmed Compact Reconnaissance Imaging Spectrometer for Mars
title_sort compact reconnaissance imaging spectrometer for mars
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.655.1406
http://planetary.brown.edu/pdfs/3960.pdf
genre Ice
permafrost
genre_facet Ice
permafrost
op_source http://planetary.brown.edu/pdfs/3960.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.655.1406
http://planetary.brown.edu/pdfs/3960.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
_version_ 1766027484884631552