| タイトル | The Gravity Field of Mercury After the Messenger Low-Altitude Campaign |
| 本文（外部サイト） | http://hdl.handle.net/2060/20160008407 |
| 著者（英） | Smith, David E.; Solomon, Sean C.; Genova, Antonio; Mazarico, Erwan; Goossens, Sander; Zuber, Maria T.; Lemoine, Frank G.; Neumann, Gary A. |
| 著者所属（英） | NASA Goddard Space Flight Center |
| 発行日 | 2015-03-16 |
| 言語 | eng |
| 内容記述 | The final year of the MESSENGER mission was designed to take advantage of the remaining propellant onboard to provide a series of lowaltitude observation campaigns and acquire novel scientific data about the innermost planet. The lower periapsis altitude greatly enhances the sensitivity to the short-wavelength gravity field, but only when the spacecraft is in view of Earth. After more than 3 years in orbit around Mercury, the MESSENGER spacecraft was tracked for the first time below 200-km altitude on 5 May 2014 by the NASA Deep Space Network (DSN). Between August and October, periapsis passages down to 25-km altitude were routinely tracked. These periods considerably improved the quality of the data coverage. Before the end of its mission, MESSENGER will fly at very low altitudes for extended periods of time. Given the orbital geometry, however the periapses will not be visible from Earth and so no new tracking data will be available for altitudes lower than ~75 km. Nevertheless, the continuous tracking of MESSENGER in the northern hemisphere will help improve the uniformity of the spatial coverage at altitudes lower than ~150 km, which will further improve the overall quality of the Mercury gravity field. |
| NASA分類 | Geophysics |
| レポートNO | GSFC-E-DAA-TN21235 |
| 権利 | Copyright, Distribution as joint owner in the copyright |
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