{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1361699994018172032.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2015gl063219"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2015GL063219"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2015GL063219"}}],"dc:title":[{"@value":"Volume of Martian midlatitude glaciers from radar observations and ice flow modeling"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Numerous glacier‐like forms have been identified in the midlatitudes of Mars, and within recent years the acquisition of radar sounding data has revealed that the features are chiefly composed of water ice. Here we use radar observations in combination with ice flow models and inverse methods to calculate the volume of ice present at the midlatitudes of Mars. In order to obtain ice thicknesses, we infer the yield stress of the ice deposits, and we find that they are consistently lower than those of most terrestrial glaciers. We estimate the present ice volume of lobate debris aprons (identified by Levy et al. (2014)) on Mars to correspond to 1.55 · 10<jats:sup>5</jats:sup> km<jats:sup>3</jats:sup> with an uncertainty of 25%. This corresponds to a global ice cover of 1.1m. Thus, the water ice found at midlatitudes is an important water reservoir, and an important part of the global surface ice budget.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699994018171904","@type":"Researcher","foaf:name":[{"@value":"N. B. Karlsson"}],"jpcoar:affiliationName":[{"@value":"Centre for Ice and Climate, Niels Bohr Institute University of Copenhagen  Copenhagen Denmark"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994018172033","@type":"Researcher","foaf:name":[{"@value":"L. S. Schmidt"}],"jpcoar:affiliationName":[{"@value":"Centre for Ice and Climate, Niels Bohr Institute University of Copenhagen  Copenhagen Denmark"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994018172032","@type":"Researcher","foaf:name":[{"@value":"C. S. Hvidberg"}],"jpcoar:affiliationName":[{"@value":"Centre for Ice and Climate, Niels Bohr Institute University of Copenhagen  Copenhagen Denmark"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2015-04-27","prism:volume":"42","prism:number":"8","prism:startingPage":"2627","prism:endingPage":"2633"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2015GL063219"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2015GL063219"}],"createdAt":"2015-03-18","modifiedAt":"2023-09-16","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360302865718988032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Estimation of the mass fraction and distribution of ice in a lunar regolith simulant from seismic velocity"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317028462208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Estimation of bulk permittivity of the Moon’s surface using Lunar Radar Sounder on-board Selenological and Engineering Explorer"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/2015gl063219"},{"@type":"CROSSREF","@value":"10.1016/j.icarus.2023.115725_references_DOI_YjQmE4cnb42Ah7HFJRhsgz0ze2S"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01259-2_references_DOI_YjQmE4cnb42Ah7HFJRhsgz0ze2S"}]}