Item talk:Q235221
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "TES mapping of Mars' north seasonal cap", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70022775", "url": "https://pubs.usgs.gov/publication/70022775" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70022775 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1006/icar.2001.6670", "url": "https://doi.org/10.1006/icar.2001.6670" }, { "@type": "PropertyValue", "propertyID": "ISSN", "value": "00191035" } ], "journal": { "@type": "Periodical", "name": "Icarus", "volumeNumber": "154", "issueNumber": "1" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Icarus" } ], "datePublished": "2001", "dateModified": "2019-02-22", "abstract": "The\u00a0Mars Global Surveyor\u00a0thermal emission spectrometer has made observations of Mars' north polar region for nearly a full martian year. Measurements of bolometric emission and reflectance, as well as brightness temperatures in specific bands synthesized from thermal radiance spectra, are used to track the behavior of surface and atmospheric temperatures, the distribution of condensed CO2\u00a0and H2O, and the occurrence of dust storms. CO2\u00a0grain size in the polar night is variable in space and time, and is influenced by atmospheric conditions. Some specific locations display concentration of H2O frost and indicate the presence of long-term water-ice near the surface. 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