Show simple item record

dc.contributor.authorMazarico, Erwan Matias
dc.contributor.authorGenova, Antonio
dc.contributor.authorGoossens, Sander
dc.contributor.authorLemoine, Frank G.
dc.contributor.authorNeumann, Gregory A.
dc.contributor.authorSolomon, Sean C.
dc.contributor.authorZuber, Maria
dc.contributor.authorSmith, David Edmund
dc.date.accessioned2015-07-31T12:10:29Z
dc.date.available2015-07-31T12:10:29Z
dc.date.issued2014-12
dc.date.submitted2014-06
dc.identifier.issn21699097
dc.identifier.issn2169-9100
dc.identifier.urihttp://hdl.handle.net/1721.1/97927
dc.description.abstractWe have analyzed 3 years of radio tracking data from the MESSENGER spacecraft in orbit around Mercury and determined the gravity field, planetary orientation, and ephemeris of the innermost planet. With improvements in spatial coverage, force modeling, and data weighting, we refined an earlier global gravity field both in quality and resolution, and we present here a spherical harmonic solution to degree and order 50. In this field, termed HgM005, uncertainties in low-degree coefficients are reduced by an order of magnitude relative to earlier global fields, and we obtained a preliminary value of the tidal Love number k[subscript 2] of 0.451 ± 0.014. We also estimated Mercury's pole position, and we obtained an obliquity value of 2.06 ± 0.16 arcmin, in good agreement with analysis of Earth-based radar observations. From our updated rotation period (58.646146 ± 0.000011 days) and Mercury ephemeris, we verified experimentally the planet's 3:2 spin-orbit resonance to greater accuracy than previously possible. We present a detailed analysis of the HgM005 covariance matrix, and we describe some near-circular frozen orbits around Mercury that could be advantageous for future exploration.en_US
dc.language.isoen_US
dc.publisherAmerican Geophysical Union (AGU)en_US
dc.relation.isversionofhttp://dx.doi.org/10.1002/2014JE004675en_US
dc.rightsCreative Commons Attribution-NonCommercial-NoDerivs Licenseen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/en_US
dc.sourceAmerican Geophysical Unionen_US
dc.titleThe gravity field, orientation, and ephemeris of Mercury from MESSENGER observations after three years in orbiten_US
dc.typeArticleen_US
dc.identifier.citationMazarico, Erwan, Antonio Genova, Sander Goossens, Frank G. Lemoine, Gregory A. Neumann, Maria T. Zuber, David E. Smith, and Sean C. Solomon. “The Gravity Field, Orientation, and Ephemeris of Mercury from MESSENGER Observations after Three Years in Orbit.” Journal of Geophysical Research: Planets 119, no. 12 (December 2014): 2417–2436.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciencesen_US
dc.contributor.mitauthorMazarico, Erwan Matiasen_US
dc.contributor.mitauthorGenova, Antonioen_US
dc.contributor.mitauthorZuber, Mariaen_US
dc.contributor.mitauthorSmith, David Edmunden_US
dc.relation.journalJournal of Geophysical Research: Planetsen_US
dc.eprint.versionFinal published versionen_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dspace.orderedauthorsMazarico, Erwan; Genova, Antonio; Goossens, Sander; Lemoine, Frank G.; Neumann, Gregory A.; Zuber, Maria T.; Smith, David E.; Solomon, Sean C.en_US
dc.identifier.orcidhttps://orcid.org/0000-0001-5584-492X
dc.identifier.orcidhttps://orcid.org/0000-0003-2652-8017
dspace.mitauthor.errortrue
mit.licensePUBLISHER_CCen_US
mit.metadata.statusComplete


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record